united states department of the interior …pubs.usgs.gov/of/1978/0558q/report.pdfnumerous copper...
TRANSCRIPT
UNITED STATES DEPARTMENT OF THE INTERIOR
GEOLOGICAL SURVEY
MAP AND DISCUSSION OF THE METALLIFEROUS AND SELECTED NONMETALLIFEROUS
MINERAL RESOURCES OF THE TALKEETNA MOUNTAINS QUADRANGLE, ALASKA
By
D. A. Singer, Bela Csejtey, Jr., and R. 0. Miller
TO ACCOMPANY OPEN-FILE REPORT 78-558Q
This report is preliminary and has not been reviewed for con formity with Geological Survey standards and nomenclature
Menlo Park, California
1978
Introduction
This report consists of a text, three tables, references cited and
an accompanying map, and it is the culmination of a mineral resource
assessment of the Talkeetna Mountains quadrangle of Alaska. The report
was prepared as part of a multidisciplinary assessment of the quadrangle
by the U.S. Geological Survey's Alaska Mineral Resource Assessment
Program (AMRAP). It represents an integration of the geologic, geochemi-
cal, and geophysical investigations of the program; the other components
are listed in the references at the end of this report.
The general form of this assessment is consistent with that used in
the AMRAP program (Singer, 1975). An attempt is made to estimate the
resources in the ground in such a way that different assumptions about
intensity and quality of exploration, future prices, and mining costs
can be tested to estimate potential supply. Three basic steps are
attempted. First, tracts of land are delineated according to the kinds
of mineral deposits their character will permit. Second, the number of
deposits within each tract is estimated. And third, characteristics of
the ore in deposits are estimated by means of models of average grades
and tonnages based on similar well-explored deposits.
Tracts of land that are geologically permissive for the occurrence
of mineral deposit types are delineated on the accompanying map. These
tracts were outlined on the basis of their known deposits (listed in
Table 3 and shown on the map) and their potential for undiscovered de
posits as inferred on the basis of occurrences in similar geologic set
tings elsewhere. Table 3 was previously published by Csejtey and
Miller (1978). The outer Vimit of delineated tracts was not allowed to
extend beyond geologic units that are permissive for the occurrence of
a deposit type, and tracts were further restricted in area! extent if
closer examination demonstrated absence of mineralization. Criteria that
were used to identify and delimit each tract are presented in Table 1.
The undelineated tracts, including areas of thick unconsolidated sediments,
were also investigated for mineral deposits. Although these tracts may
contain deposits of placer gold, zeolites, and barium (see page 7), the
available geological, geochemical, and geophysical data did not permit
delineation.
Probabilistic estimates of the number of deposits of each type were
made for the few tracts where such estimates were warranted by available
information. The estimates were made subjectively, and are presented in
a probabilistic form in order to show the degree of certainty concerning
the number of deposits that might occur. In order to provide estimates
which agree in general with the established format of AMRAP assessments
(Singer, 1975; Singer and Ovenshine, 1979, p. 588), in this report we
have estimated the number of mineral deposits possibly present in each
tract from a cumulative distribution diagram at the arbitrarily chosen 10,
50, and 90 percent confidence levels. Thus, at the 90 percent level there
is a 90 percent chance that the actual number of deposits in the tract is
equal to or exceeds the estimate. A variety of pertinent considerations
were integrated, including degrees of geologic, geochemical, and geophys
ical favorability; extent and adequacy of exploration and geologic know
ledge; and extent of exploration of deposits already recognized.
Grade-tonnage models are provided for four deposit types: porphyry
copper, porphyry molybdenum, fel sic to intermediate volcanogenic, and
mafic volcanogenic (Table 2). Models were based on well-explored de
posits for which tonnages of mineralized rock would be calculated by
adding past production to estimated reserves or resources. Deposits
known to be incompletely explored were excluded in constructing models.
A more extensive discussion of the models can be found in Menzie and
Singer (in press).
The mineral resources in the quadrangle are discussed below by tract
and by deposit type. Grade-tonnage models are mentioned where applicable,
Estimates of the number of deposits are also presented by tract for the
few situations where it was possible to make such estimates. Several
commodities and/or deposit types are not specifically delineated because
of their widespread occurrence or apparent lack of geologic control;
these are described in the section following the discussion of resources
by tract.
Tract TI
This tract is delineated for disseminated tin deposits. Tin values
range from 20 to 15,000 ppm in the nine rock samples of alaskite and mus-
covite granite reported by Reed (1978). Values of 100 and 150 ppm silver
were reported from two of Reed's samples and disseminated cassiterite was
observed in three samples. The distribution of high values of tin in
stream sediment and pan concentrate samples (Miller and others, 1978a)
suggests that tin mineralization is widespread in the tract. Additional
work is required to determine the extent and grade of tin mineralization.
It was not possible to construct a grade-tonnage model for this deposit
type.
Tract T£
No tin-bearing occurrences are known in this tract, however the
presence of geochemical anomalies of tin and related elements (Miller and
others, 1978a) like those in Tract T^, and the presence of the same age and
general types of granite as those in Tract TJI suggest that this tract also
deserves further work.
Tract P}
Two porphyry molybdenum prospects are known in this tract, but neither
has been drilled intensively enough to determine whether their sizes and
grades are comparable to the deposits used to construct the porphyry molytx-
denum grade-tonnage model (Table 2). Although permissive granitic rocks
are widespread, the number of geochemical anomalies is not large. On the
basis of this evidence, the number of porphyry molybdenum deposits com
parable to the grade-tonnage model is subjectively estimated to be:
(1) a 90 percent chance that there are 1 or more deposits;
(2) a 50 percent chance that there are 2 or more deposits;
(3) a 10 percent chance that there are 2 or more deposits; that is,
the chance that there are more than two deposits is estimated
to be much less than 10 percent.
Tract ?2
A few anomalous values of copper and gold from pan concentrate and
stream sediment samples, a low-grade disseminated molybdenum and gold
occurrence (map no. 19), and an aeromagnetic pattern indicative of either
a zoned or altered pluton that is incompletely exposed, suggest the possi
bility of either porphyry copper or molybdenum deposits in this tract.
The number of porphyry copper or molybdenum deposits comparable to the
grade*-tonnage models of these deposit types (Table 2) is subjectively
estimated to be:
(1) a 90 percent chance that there are 0 or more deposits;
(2) a 50 percent chance that there are 1 or more deposits;
(3) a 10 percent chance that there are 1 or more deposits; that is,
the chance that there is more than one deposit is estimated to
be much less than 10 percent.
Tract P3
This tract is delineated for porphyry copper and/or porphyry molyb
denum deposits. There is one known porphyry copper prospect (map no. 88)_
that has had some drilling by industry. Scattered geochemical anomalies
and a float sample of altered granodiorite containing molybdenum are
suggestive of other mineralization in the tract. The number of porphyry
copper or molybdenum deposits comparable to the grade-tonnage models of
these deposit types (Table 2) is subjectively estimated to be:
(1) a 90 percent chance that there are 1 or more deposits;
(2) a 50 percent chance that there are 1 or more deposits;
(3) a 10 percent chance that there are 2 or more deposits.
Tract ?4
The presence of porphyry copper and/or molybdenum type deposits
in this tract is suggested by numerous float samples of altered granitic
rocks containing copper and/or molybdenum, several prospects in altered
granitic rocks, and numerous anomalous samples containing copper,
molybdenum, and lead. The number of porphyry copper and/or porphyry
molybdenum deposits comparable to the grade-tonnage models (Table 2) is
subjectively estimated to be:
(1) a 90 percent chance that there are 1 or more deposits;
(2) a 50 percent chance that there are 2 or more deposits;
(3) a 10 percent chance that there are 3 or more deposits.
Tract Y! (P)
Widespread pan concentrate samples having high concentrations of
lead, arsenic, gold, tungsten, molybdenum, copper, tin, and bismuth
suggest that Tract Vj (P) contains base and precious metal vein deposits.
Such deposits would be localized in granitic rocks and the associated
older sediments. Although a grade-tonnage model is not available, de
posits of this type typically have low tonnage. Porphyry molybdenum
deposits are also indicated as possible because of the extension of the
favorable rocks of Tract PI into Tract V} (P) and the numerous geochemi-
cal anomalies, some of which may be related to porphyry molybdenum
mineralization.
Tract V2
The Tertiary fel sic volcanic rocks in this tract are associated with
numerous pan concentrate samples with high values of copper, lead, arse
nic, silver, zinc, and molybdenum; locally there are high values of tung
sten, bismuth, and tin. The only known occurrences are claims for copper
and gold, apparently veins, and altered andesite dikes containing low
values of tin and zinc. Based on this evidence, the tract is delineated
for base and precious metal vein deposits that typically have low tonnage
but locally may have high grades.
Tract Msvj
This tract is delineated for mafic to intermediate volcanogenic
massive sulfide deposits and for copper in amygdaloidal basalts.
Numerous copper and related sulfide-bearing prospects and occurrences of
veins and local disseminations in altered intermediate to mafic meta-
volcanics of upper Paleozoic age are known. There are also some indi
cations of copper in the upper Triassic amygdaloidal metabasalts, but
little is known about the extent of these occurrences. A large pro
portion of the geochemical samples from this extensive tract contain
anomalous amounts of the metals that are commonly associated with
veins and volcanogenic massive sulfide deposits. Although this tract
contains numerous base and precious metal veins, tonnages of the vol
canogenic massive sulfide deposits that are believed to exist in the
tract dwarf those of the veins. A grade-tonnage model for intermediate
to mafic volcanogenic deposits does not exist, however, grade-tonnage
models for felsic to intermediate volcanogenic and for mafic volcano
genic deposits are provided in Table 2 in order to demonstrate the grades
and tonnages that may exist in this tract. Tonnages are similar for the
two models; the main difference is the presence of lead in some of the
felsic to intermediate deposits. Lead is known to occur in some of the
prospects and occurrences in this tract.
Undelineated Tracts
Some of the commodities or deposit types that are not specifically
delineated are discussed below.
In the Horn Mountains and Albert Creek region, extensive deposits
of mordenite and other zeolites of possible economic interest are known
(see Table 3, map number 112). The known deposits are in the tuffaceous
part of the Lower Jurassic Talkeetna Formation. Similar deposits prob
ably occur elsewhere in the Talkeetna Formation.
Claims for placer gold are widely distributed in the quadrangle.
For the placer gold deposits of the Nelchina area, Grantz (1956) suggests
that continental gravels of Eocene age, inferred to have overlain most
of the area, contained concentrations of placer gold which were reworked
during late Pleistocene .and Recent time to form the present placers.
The source of the other placer gold in the quadrangle is not known. About
150 oz. of gold was produced from Albert Creek (map number 111), the only
placer deposit in the quadrangle with proven production. Because of the
scanty production, it is believed that there is little chance of signifi
cant future production of gold from the quadrangle's placer deposits.
Throughout the quadrangle, a large number of the heavy mineral con
centrate samples showed apparently anomalous concentrations of barium
(Miller and others, 1978k), however, the source of this barium is not
known.
In spite of two creeks having the name Coal Creek in the quadrangle,
no significent deposits of coal are known or suspected.
Table 1. Deposit type and criteria for selection of mineral resource
tracts in the Talkeetna Mountains quadrangle, Alaska.
[Numbers in parentheses are the map numbers of mineral deposits, prospects and occurrences listed on the accompanying resource map and in Table 3.Sources of information for the various criteria are: Csejtey and others (1978), geology; Miller and others (1978a-l), Miller and others (JL978), geochemistry; Csejtey and Griscom (1978), aeromagnetics; Csejtey and Miller (1978), mineral deposits.]
Tract Types of deposit(s) possible and criteria usedoutlined to delineate tractson map _________________________________________
TI Disseminated tin deposits(a) Known disseminated tin prospect containing cassiterite (4).(b) Pervasive alteration (addition of boron and flourine).(c) Small outcrop of greisenized muscovite granite containing
tourmaline, topaz, sericite, and minor flourite.(d) High concentrations of tin and locally silver, arsenic,
copper and zinc in rock samples.(e) Anomalous concentrations of tin, gold, and zinc in stream
sediment samples.(f) High concentrations of tin, silver, tungsten, barium,
arsenic and gold in pan concentrate samples.
T« Disseminated tin deposits(a) Same age and general type of granite as in Ti.(b) Consistently high tin and tungsten and locally high gold
and silver values in pan concentrate samples.(c) One anomalous tin value in a stream sediment sample.
P! Porphyry molybdenum deposits(a) Two porphyry molybdenum prospects are known (8,9).(b) Forcibly emplaced epizonal plutons of biotite, grano-
diorite and adamellite.(c) Anomalous concentrations of lead, zinc, and one sample each
of molybdenum and copper in stream sediment samples.(d) High concentrations of lead, tungsten and tin in pan con
centrate samples.
?2 Porphyry copper or porphyry molybdenum(a) Very low-grade disseminated occurrence (19) containing
molybdenum and gold located in granodiorite.(b) Aeromagnitic pattern that suggests either compositionally
zoned or an altered pluton that is incompletely exposed.(c) Two stream sediment samples have anomalous gold values.(d) Two pan concentrate samples have high copper values.
Table 1. (continued)
Porphyry copper and/or porphyry molybdenum(a) A prospect (88) containing copper minerals and molyb
denite disseminated in altered granitic rock is known.(b) A float sample (86) of altered granodiorite with dis
seminated pyrite is probably from P3. jc) Forcibly emplaced epizonal plutons of biotite granodiorite.[d) Several stream sediment samples contain anomalous concen
trations of zinc, molybdenum, lead, and copper.(e) Several pan concentrate samples contain high values of
tungsten, bismuth, and molybdenum; one sample contains high values of gold, copper, and silver.
?4 Porphyry copper and/or porphyry molybdenum(a) Float samples containing pyrite, copper-bearing minerals,
or molybdenum in altered granitic rocks or quartz veins (64, 65, 67, 89, 90, 96, 98).
(b) Two prospects reported as gold (95), and copper, gold and silver claims (94) in tonalite; molybdenum-bearing altered granodiorite (66); disseminated sulfides in quartz diorite (50).
(c) Biotite-hornblende tonalite locally grading into quartzdiorite of Late Cretaceous and Jurassic ages; intermixed mosaic of amphybolite, quartz diorite, and granodiorite.
(d) Anomalous stream sediment samples contain lead and copper; one sample each anomalous in molybdenum and tin.
(e) Numerous pan concentrate samples containing high values of molybdenum and copper; several samples contain high tungsten values.
VI(P) Base and precious metal veins and/or porphyry molybdenum deposits(a) Argentiferous galena in quartz veinlets (31) and several
placer gold deposits (32, 33, 34, 35, 36) known.(b) Forcibly emplaced epizonal plutons of biotite granodiorite
exposed in southeastern V,(P) and partially exposed in northwestern V^(P).
(c) Majority of stream sediment samples have anomalous concen trations of lead; several samples have anomalous values of gold, copper, silver, and zinc.
(d) High concentrations of lead, arsenic, gold, tungsten,molybdenum copper, tin, and bismuth in pan concentrate samples.
10
Table 1. (continued)
V2 Base and precious metal vein deposits(a) Lode claims for copper and gold, apparently veins (63);
pyritiferous altered andesite dikes contain low values of tin and zinc (62).
(b) Tertiary felsic subaerial volcanic rocks and related shallow intrusives.
(c) Based on aeromagnetics, ^2 is restricted to felsic por tions of TV.
(d) Numerous high copper, lead, arsenic, silver, zinc, and molybdenum values in pan concentrate samples; locally high tungsten, bismuth, and tin values.
(e) Local anomalous values of lead, gold, and tin in stream sediment samples.
Mafic to intermediate volcanogenic and copper-in-amygdaloidal- basalt deposits
(a) Numerous copper and related sulfide-bearing prospects and occurrences,of veins and local disseminations in altered intermediate to mafic metavolcanics of upper Paleozoic age (e.g. 17, 27, 48, 76, 81, 82, 92).
(b) Altered sulfide-bearing dikes of felsic volcanics prob ably Tertiary in age (15, 16, 70).
(c) Paleozoic marine sequence of dominantly metamorphosed flows and tuffs having basaltic to andesitic composi tion; subordinate upper Triassic shallow marine amygdaloidal metabasalts, partially unmapped; locally unmapped Tertiary felsic dikes.
(d) Anomalous concentrations of molybdenum, copper, lead, zinc, gold, and silver in stream sediment samples.
(e) Pan concentrate samples with high values of tungsten,silver, and molybdenum; locally high values of bismuth, arsenic, copper, zinc, lead, and gold.
11
Tabl
e 2.--Grade
and
tonnage
mode
ls for
mineral
depo
sits
of
the
Talk
eetn
a Mountains
quadrangle,
Alas
ka
[Related d
ata
occur
In li
ne f
rom
colu
mn t
o column;
all
tonnages In m
etri
c units; **
, significant
at 1
per
cent
lev
el]
Deposit
Type
Porp
hyry
co
pper
Porp
hyry
molybdenum
Mafic
volcanogenic
massive
sulfide
Felsic a
nd
inte
rmed
iate
volcanogenic
massive
sulfide
Tonnage
and
grade
vari
able
s (units
In p
aren
thes
is)
Tonnage
of "
ore"
(millions
of t
ons)
Average
copp
er g
rade
(p
erce
nt)
Tonnage
of "
ore"
(millions
of t
ons)
Average molybdenum
grad
e (percent)
Tonnage
of "
ore"
(millions
of t
ons)
Average
copp
er g
rade
(percent)
Average
zinc gr
ade
excl
udin
g de
posi
ts w
ithout
re
port
ed g
rades
(percent)
Average
gold a
nd s
ilve
r grades locally
sign
ific
ant
but
not
determined
Tonnage
of "ore"
(millions
of t
ons)
Average
copp
er g
rade (percent)
Average
zinc g
rade
Numb
er o
f Correlation
coef
fici
ent
of
Depo
sits
used
list
ed v
ariable
with
to d
evel
op
variable o
n li
ne w
ith
it
model
in c
olum
n 2
38 38
With tonnage
of "
ore"
=
-0.0
8
34 34
With t
onnage o
f "o
re"
= -.11
37
37
With t
onnage o
f "o
re"
= -.13
19
With t
onnage o
f "ore"
= .03
89
89
With tonnage
of "
ore" =
-.41
**
41
With t
onnage o
f "ore"
= .25
90 p
ercent
of d
epos
its
have a
t le
ast 18.0
0
.10
.27
.07
.24
1.10 .30
.19
.54
1.40
50 p
ercent
of d
eposits
have
at
leas
t 89.0
0
.25
28.0
0
.12
2.30
2.20
1.30
1.90
1.70
3.80
10 p
erce
nt
of d
epos
its
have
at
leas
t
450.
00 .55
430.
00 .24
22.00
.
4.10
5.50
16.0
0
5.40
10.00
excl
udin
g de
posi
ts w
itho
ut
repo
rted
grades
(per
cent
)
Average
lead
gra
de
14
excl
udin
g de
posi
ts w
ithout
re
port
ed l
ead
grad
es (p
erce
nt)
Tonnage
cont
aine
d gold
38
excl
udin
g de
posi
ts w
ithout
repo
rted
gol
d (t
ons
Au)
Tonnage
contained
silv
er
46
excluding
depo
sits
wit
hout
repo
rted
silver
(ton
s Ag)
With t
onnage o
f "ore"
= -.
02
.20
With t
onnage o
f "ore"
= .73**
.27
With t
onnage o
f "ore"
= .82**
5.00
.95
2.90
80.00
4.80
32.0
0
1300.00
Table 3. Mines, prospects, and mineral occurrences in the Talkeetna Mountains quadrangle, Alaska.
Explanatory note
In this report the term "mineral deposits" is used in the broad sense to include deposits, both lode and placer, at mines and prospects as well as unclaimed occurrences, regardless of economic significance. Localities of geochemical rock samples with anomalous metal concentrations have also been included. Geochemical rock samples are considered to be anomalous when out of the selected ten metallic elements, one element greatly exceeds or two or more elements at least reach the following empirically chosen concentration levels (in parts per million): silver--0.7, arsenic 200, gold--0.25, chromium--1,500, copper 1,000, molybdenum--?, lead 70, anti mony 300, tin 10, and zinc 500. The sample numbers of these anomalous geochemical rock samples from prospects as well as from unclaimed occur rences, including float samples, are given in parentheses in the Principal references column of this table. Complete analytical data for all geochemical rock samples collected by the U.S. Geological Survey in the study area have been reported by Miller and others (1978).
Explanation of table headings
Map no. and name(s) (if known)
Map no. refers to a specific deposit on the accompanying map. Name(s) of prospects or mines are derived from published sources or from gen eral usage. In several cases, more than one prospect or occurrence is grouped under the same map number.
Location
Location refers to the'standard township and range land designations relevant to specific parallels and meridians on the U.S. Geological Survey quadrangle map used as a base for this report.
Category
M -- mine P -- prospect 0 -- occurrence
The terms mines, prospect, and occurrences are used as follows:
Mine -- a mineral deposit with recorded production. Ore was mined but not necessarily shipped.
Prospect -- a deposit which has been- staked and, in many cases, has been scantily explored; lacks evidence of production. Claims may or may not be active. Some of tiie.placer gold deposits that
13
Table 3. (continued)
are listed as prospects probably have had at least meager pro duction but, because of lack of definitive evidence, they are classified as prospects.
Occurrence generally a minor deposit that, as far as known, is unclaimed and is mainly known from recent U.S. Geological Sur vey field investigations or from the analyses of geochemical rock samples. Also includes the locations of float samples with anomalous concentrations of metals. The criteria for anomalous geochemical rock samples are discussed in the Explan atory note of this table.
Resource(s) (minor constituents or potential byproducts in Parentheses)
Indicates commodity or commodities that are known or reported at each locality. Question marks are used where presence of commodity is inferred from indirect evidence or based on unverified reports. Commodities are listed in decreasing order of probable commercial value or of abundance in the deposits. Metallic commodities are denoted by standard chemical symbols.
Form
Type
Denotes the physical aspect of a deposit. Queried where uncertain. Left blank for occurrences based on mineralized rock samples found only in float.
Rather speculative designation concerning the genesis of the deposit. Queried where based on insufficient information. Left blank for mineralized rock samples found only in float.
Brief description
Provides brief descriptions of the geology and mineralogy of the deposits and, where applicable, production data. Several prospects are known only from a U.S. Bureau of Mines claim map (1973); infor mation of these is generally limited to reported commodities and category of deposit.
Principal references
Cites sources for information used in the table and map. For pros pects and occurrences known primarily from analyzed geochemical rock samples reported by Miller and others (1978), the sample field numbers are given in parentheses.
Abbreviations used
Standard chemical symbols are used;'for example, Cu - copper, Au - gold, Sn - tin.
14
MINES, PR
OSPE
CTS, A
ND M
INER
AL O
CCUR
RENC
ES IN
THE TALKEETNA
MOUNTAINS
QUAD
RANG
LE,
ALAS
KA
RESOURCE (S)
Mi
nor
cons
tl tu-
HAP
NO.
AND
NAME(S)
LOCATION
CATE
GORY
ents o
r po
tent
ial
FORM
(If
known)
byproducts 1n
pa
rent
hese
s
1 T.33N..R.4U.
P Ag,As,Mo(Pb,Au)
Diss
emin
ated
2 T.22S..R.12U.
P Au(Ag)
Vein
3 T.22S..R.12H.
P Au
Vein
4 T.22S..R.12W.
P Sn(Ag.As,Cu,Mo,
Diss
emin
ated
Zn.Pb)
S T.32N..R.2W.
0 Cr(Pb)
Diss
emin
ated
6 T.32N..R.2W.
P Cu(Au)
Vein?
7 Mi
nt
T.32
N..R
.1E.
M
Sb,A
g,Cu
,As(
Pb,
Velnlets
Au)
8 T.J2N..R.1E.
P Mo
(Cu.
Zn)
Diss
emin
ated
TYPE
Hydr
o thermal
Hydro t
hermal
Hydr
o thermal
"Porphyry
tin"
Meta
morp
hlc?
Hydrothermal?
Hydrothermal
Hydro thermal
,po
rphy
ry?
PRINCIPAL
BRIE
F DESCRIPTION
REFE
RENC
ES
Smal
l py
rlte
-bea
rlng
min
eral
- Mi
ller
and
lied
zon
e In b
reed
a ted
chert
others,
1978
and ar
gllH
te o
f unit J
ta.
(sample
no.
Seve
ral
claims In a
djac
ent
area
75Nw
095)
; U.S.
Bur.
Mines. 1973
Lode c
laims
1n c
hert a
nd a
rgil
- U.S. Bur
Mines.
llte o
f un
it J
ta
1973;
MacKevett
and
Holl
oway
,1977
_. ....-do...-... ..
...
....
. Do.--
Primarily
tin mineralization
Reed
. 1978
(cas
sUer
lte)
In sm
all
outcrop
of g
relsenlzed T
ertiary
granitic
Intrusive
Into u
nit
DSga
Scat
tere
d pyrlte In
altered
Miller a
ndco
ntac
t metamorphosed ar
gllH
te
others,
1978
and
gray
wacke
of u
nit
Kag;
adja-
(sample
no.
cent to Te
rtia
ry g
rani
tic
Intru- 75
Nw00
3A)
slon
Lode c
laims
In small
Tert
iary
MacKevett
and
gran
itic
In
trus
ion
Holl
oway
. 19
77;
U.S. Bur. Mines.
1973
Pyrargyrlte
and
mlargyrlte.
Capp
s and
Short,
alon
g wi
th m
inor
amounts o
f 19
26;
Rlch
ter,
othe
r su
l fi
des,
1n q
uartz
vein-
1963
; Berg a
ndlets cutting ar
gllH
te o
f unit
Cobb,
1967
, p.
Kag.
Some
production.
Sev-
27;
Cobb.
1972;
eral lo
de c
laim
s In a
djacent
MacKevett
and
area
s Ho
llow
ay,
1977
Molybden
ite, pyrlte,
mino
r Rlchter, 1963
chalcopy
rlte.
and
spha
leri
te In
I
Q> cr (D CO o o 3 ri- 13 c n> o.
9 Tr
easu
re C
reek
T.32N..R.1E.
slllclfl
ed shear
zone w
ithi
n Tertiary granitic Intrusion
Mo(Cu.Au.Zn)
Vein a
nd
Hydrothermal
Molybdenite
and
associated s
ul-
velnlet
fides
In c
ontact m
etamorphosed
argllHte a
nd g
raywacke o
f unit
Kag; ad
jace
nt to T
ertiary
gran
itic Intr
usion
Do.
MINE
S, PR
OSPE
CTS,
AND
MINERAL
OCCU
RREN
CES
IN T
HE TALKEETNA
MOUN
TAIN
S QU
ADRA
NGLE
, AL
ASKA
(c
onti
nued
)
HAP
NO. AN
D NA
ME(S
) LOCATION
(If
known)
RESO
URCE
(S)
Minor
cons
tltu
- CATEGORY
ents o
r potential
FORM
TYPE
byproducts In
parentheses
PRIN
CIPA
L BR
IEF DESCRIPTION
REFE
RENC
ES
10T.
33N.
.R.7
W.(Au.Ag)
Vein
Hydrothermal
Smal
l quartz v
eins
In a
rgllHtt
HUler
and
of u
nit
Kag.
No visible
ore
others.
1978
mine
rals
(s
ampl
e no.
75NW132)
11 12 13 14 IS
T.32N..R.4E.
0
T.22S..R.5H.
P
T.22S..R.3U.
0
Mo(Pb)
Au
Au(Ag)
Diss
emin
ated
Hydrothermal?
Diss
emin
ated
Placer
Disseminated
Hydrothermal
T.22S..R.2U.
0(Mo)
Disseminated?
Hydrothermal?
T.22
S..R
.2U
. 0
Ag(
Mo.
Au)
D
isse
min
ated
P
orph
yry?
Sca
ttere
d pyrlte
In
mic
a sc
his
t ad
jace
nt
to T
ert
iary
g
ran
itic
In
trusi
on
Sev
eral
cl
aim
s In
cre
ek b
ed.
Surf
ldal
depo
sits
are
too
sm
all
to
show
at
the
scal
e of
geol
ogic
nap
Pyr
lte a
nd q
uart
z In
altera
tion
zone
with
in T
ert
iary
gra
nitic
In
trusi
on
Low
-gra
de.s
ulfi
de-b
earin
g
alte
ratio
n
zone
In
maf
ic r
oeta
- vo
lcan
lc
rock
s of
un
it Tk
v
Smal
l su
lfid
e-b
ea
rin
g a
ltera
tio
n z
one
In fe
lslc
vo
lcan
ic
dike
In
trudin
g m
afic
met
avol
ca
nic
rock
s of
unit t
iv
Mill
er
and
othe
rs,
1978
(s
ampl
e no
. 77
Cy0
16B)
U.S
. Bu
r. H
ints
, 19
73DI
cr n>
Mill
er
and
oth
ers
, 19
78
(sam
ple
no.
73S
t007
0);
T.
E.
Sm
ith,
written c
ooro
un.,
1973
Mill
er
and
oth
ers
, 19
78
(sam
ple
no.
73S
tl035
);
T.C
. S
mith
, w
ritt
en
co
iranu
n.,
1973
Mill
er
and
oth
ers
, 19
78
(sam
ple
nos.
73
Stl0
30,
73S1
0040
); T.
E.
S
mith
, w
rit
te
n co
mm
on.,
1973
o
o 3 c
n>
o.
)6T.22S..R.2W.
P(Cu)
Diss
emin
ated
Porphyry?
Low-
grad
e, cha
lcop
yrlt
e-be
arin
g mineralized
felslc volcanic
dike cutting
mafic
meta
volc
anlc
ro
cks
of u
nit
T<v
HacKevett
and
Holl
oway
. 1977}
U.S. Bu
r. Hlnes,
1973
NINE
S, PR
OSPE
CTS.
AND M
INER
AL O
CCUR
RENC
ES I
N THE
TALK
EETN
A MO
UNTA
INS
QUADRANGLE,
ALASKA
(co
ntin
ued)
MAP
NO.
AND
NAME(S)
LOCA
TION
CA
TEGO
RY
(If
known)
17
T.33N..R.9E.
0
18
Lichtn
T.32
N..R
.11E
. P
19
T.32
N..R
.9E.
0
20
T.32
N..R
.9E.
0
21
T.32N..R.9E.
0
RESO
URCE
(S)
Minor
constitu
ents o
r po
tent
ial
FORM
TYPE
bypr
oduc
ts In
parentheses
Cu
Diss
emin
ated
? Vo
lcan
ogen
lc?
Cu(A
u.Ag
) Disseminated
Subm
arin
eand
veln
let
volc
anog
enlc
(Mo.
Au)
Disseminated
Porphyry?
Hydr
othe
rmal
?
As(A
g.Pb
)
Ag(A
$.Mo
,Sn,
Au)
BRIEF
DESC
RIPT
ION
Low-gr
ade
copper m
iner
aliz
ation In
maf
ic m
etavolcanlc
rock
s of
uni
t "fo
v
Chal
copyrlte.
born
He. a
ndother
copp
er m
iner
als
scat
tere
dIn
a m
afic m
etavolcanlc
flow
of
unit P
zv.
Mine
rali
zed
zone
extend
s fo
r about
900 n. a
nd I
tIs less
than
2
wide
Very l
ow-grade, sul fide-bearing
mine
rali
zed
zone
in
quartz
dlorlt
e of u
nit
TKg
Dissemin
ated
sul fid
e mi
nera
lsIn f
loat
of
mafic
meta
volc
anlc
rock
Dissemin
ated
fine-grained
sul-
fide min
eral
s In
float o
f mafic
metavolcanlc r
ock
PRIN
CIPA
L REFERENCES
Mill
er a
ndothers,
1978
(sample
no.
73SU
050)
; T. E.
Smith, w
ritt
enco
mnun
., 19
73
Smit
h an
d others,
1975
Mill
er a
ndothers.
1978
(sam
ple
no.
73St
0164
); T
. E.
Smith, w
ritt
encomroun.,
1973
Miller a
ndothers.
1978
(sam
ple
no.
73S1
1107
); T
. E.
Smit
h, written
comm
un.,
19
73
Miller a
ndot
hers
. 1978
(sample
no.
73SU
099)
; T. E.
Smith, w
ritt
encommun.
, 19
73
-H O* cr n> CJ o o 3 =3 C n>
o.
22T
.32N
..R.8
E.
0A
g(M
o.P
b.S
n.Zn
)D
isse
min
ated
, H
ydro
ther
mal
? ve
in?
Ver
y lo
w g
rade
, su
lfid
e-b
eari
ng
m
iner
aliz
ed
zone
In
maf
ic
to
Inte
rmed
iate
met
avol
canl
c ro
cks
of
un
it P
zv
Mille
r an
d o
ther
s.
1978
(s
ampl
e no
s.
73S
t110
0,
73S
U10
1);
T.
E.
Sm
ith,
wri
t
ten
com
mun
., 19
73
MINES, PR
OSPE
CTS,
AN
D MI
NERA
L OCCURRENCES
IN T
HE T
ALKEETNA M
OUNT
AINS
QUADRANGLE, AL
ASKA
(continued)
HAP
NO.
AND
NAME(S)
(If
known)
RESO
URCE
(S)
Mi
nor
constltu-
LO CA
T I ON
CATEGORY
ents o
r potential
FORM
TYPE
byproducts In
parentheses
PRINCIPAL
BRIEF
DESC
RIPT
ION
REFERENCES
23 24
oo
25 26 27 28 29
T.32N..R.9E.
T.32N..R.8E.
0
T.32N..R.8E.
T.31N..R.9E.
T.30
N..R
.7E.
T.31N..R.3E.
T.30
N..R
.3E.
(Ag.Mo.Zn)
(Ag.Mo)
Cu
(Cu.Au)
(Ag) Au Au
Diss
emin
ated
Hydrothermal?
Disseminated,
Hydrothermal?
mass
ive,
and
vein?
Veln
let
Vein
Hydrothermal
Hydrothermal
Diss
emin
ated
Pl
acer
Diss
emin
ated
Placer
Float
of a
ltered m
afic
to
Inter- M
iller
and
mediate
meta
volc
anlc
rock
othe
rs,
1978
(sample
no.
73St
)104
h T.
£.
Smit
h, w
ritten
coro
mun.
, 19
73
Very l
ow g
rade
, su
lfid
e-be
arin
g mi
nera
lize
d sh
ear
zone I
n mafic
to I
ntermediate
metavolcanlc
rocks
of u
nit
Pzv
Copper minerals, m
ainl
y chal-
copyrlte,
within a
n extensive
shea
r zone a
long
contact
betw
een
unit
s Iw an
d Pz
v
Minor
chalcopyrlte a
nd p
yrlte
In s
mall qu
artz
vei
n cutting
mafic
metavolcanlc r
ocks o
f unit P
zv.
Exposures
too
small
to s
how
on g
eolo
gic
map
Minor
pyrl
te I
n sm
all
quartz
vein c
utting m
afic
metavol-
ca
nlc
rocks of
uni
t Pzv
Plac
er cla
im at
the mo
uth
of
smal
l tributary
of S
uslt
na
River
Placer c
laim alo
ng s
mall
creek
Incised
Into
extensive Q
uater
nary
surflclal deposits
Miller a
nd
othe
rs,
1978
(sample
nos.
73Stll03,
73StllOSH
T. E.
Smith, writ
ten
comm
un..
1973
MacKevett
and
Holl
oway
. 1977;
U.S. Bur. Mines.
1973
Miller a
nd
othe
rs.
1978
(sam
ple
no.
7TM276)
Miller a
nd
others,
1978
(sam
ple
no.
72Cy03B)
U.S. Bur. Mines.
1973
(u
cr n>
co o 3 C n>
ex
MINES. PR
OSPE
CTS.
AND
MIN
ERAL
OCC
URRE
NCES
IN
THE
TALKEETNA
MOUN
TAIN
S QUADRANGLE,
ALASKA (
continued)
MAP
NO.
AND
NAME(S
) LO
CATI
ON
CATE
GORY
(I
f known)
30
T.3DN..R.2E.
P
31
Inly
T.30N..R.1W.
P
32
T.31N..R.2W.
P
33
Susl
tna
River-
T.31N..R.2H.
PGold C
reek
34
T.29-30N..R.2H.
P
35
T.28-29N..R.3H.
P
1H
T 9RM
D AU
0JO
1 CON. .K.4W.
r
17
T 90 M
D 1U
DJ/
I.CON..K.JN.
r
38
T.27-28N..R.3-4W.
P
RESOURCE(S)
Mino
r constitu
ents o
r potential
bypr
oduc
ts In
pa
rent
hese
s
Au
Ag.P
b
Au Au Au Au Au Au Au
FORM
TYPE
Disseminated
Plac
er
Vein
Hydr
o the
rmal
Disseminated
Placer
Disseminated
Placer
Disseminated
Placer
Disseminated
Placer
Disseminated
Placer
Disseminated
Placer
Disseminated
Placer
BRIEF
DESC
RIPT
ION
Placer claim alo
ng s
mall
creek
Incised
Into
ext
ensi
ve Qua
ter
nary
sur
flcl
al de
posi
ts
Argentiferous
galena 1n
quartz
velnlets t
hat cu
t an a
lter
edfels
lc v
olcanic
dike
1n r
ocks
of u
nit
Kag
Several
placer cla
ims
alon
gcr
eek
1n a
lluv
ium
too
smal
lto
sho
w on
geo
logi
c ma
p
Gold
pla
cers
sporadically
ex
plor
ed f
or man
y ye
ars;
pos
sibl
ytoken
prod
ucti
on.
Location
show
n on m
ap I
s on
ly a
ppro
xi
mate
Plac
er c
laims
along
uppe
r Ch
u-nl
lna
River
In a
lluvial
de
posits too
smal
l to
show
ongeologic map
Plac
er c
laim
s 1n a
lluv
ium
too
small
to s
how
on g
eolo
gic
map
. do
. -
do
.
Plac
er claims
In a
lluv
ium
along
PRIN
CIPA
L REFERENCES
U.S. Bu
r. M
ines.
1973
Berg and
Cobb,
1967
. p. 27
MacK
evet
t an
dHo
llow
ay,
1977;
U.S. Bu
r. Mi
nes.
1973
Capps. 1919d, p.
231;
Cob
b. 1
972
MacK
evet
t an
dHo
llow
ay.
1977;
U.S. Bur. M
ines
.1973
Do
.
. DO
.
f\_
Do
. -
-i o> cr _j
n> co o o 3 rf 3 C n> Q. ^ '
39 40 41
T.27N..R.3-4H.
T.28N..R.2E.
T.2BN..R.2E.
Au
Disseminated
Plac
er
(Ag.
Au.P
b)
Diss
emin
ated
Hydrothermal
Zn
Diss
emin
ated
Hy
drot
herm
al
Chunllna R
iver
Plac
er c
laim
s In a
lluvium
too
smal
l to
sho
w on
geo
logi
c ma
p D
o.
Very
fin
e g
rain
ed d
isse
min
ated
. M
ille
r an
dp
yrlt
e-b
earl
ng
gos
san
alon
g ot
hers
. 19
78sh
ear
zone
1n
maf
ic m
etav
ol-
(sam
ple
no.
canl
c ro
cks
of
un
it P
zv
7SCy
lOSB
)
Pyr
lte-
bea
rln
g g
ossa
n In
sh
eare
d m
etaa
ndes
lte o
f u
nit
Pz
v
Mil
ler
and
othe
rs.
1978
(s
ampl
e no
. 75
Dr0
07)
MINE
S, PROSPECTS, A
ND M
INERAL O
CCUR
RENC
ES IN T
HE TA
LKEE
TNA MO
UNTA
INS
QUAD
RANG
LE,
ALAS
KA (c
onti
nued
)
MAP
NO
. AN
D N
AME(
S)
LOCA
TIO
N CA
TEGO
RY(I
f kn
own)
42
T.2
8N..R
.2E
. 0
RESO
URCE
(S)
Min
or c
on
stitu
en
ts o
r p
ote
ntia
l FO
RM
TYPE
bypr
oduc
ts
Inpa
rent
hese
s
Mo,
Ag(
Pb.
Sn,
As)
D
isse
min
ated
H
ydro
the ra
il
BRIE
F DE
SCRI
PTIO
N
Dee
p-re
d to
lig
ht-
bro
wn
, pyrltt-
bear
lng,
ext
ensi
ve g
ossa
n In
ap
ha
nltl
c In
term
edia
te m
eti-
volc
anlc
ro
cks
of
un
it P
zv
PRIN
CIP
ALRE
FERE
NCES
Mill
er
and
oth
ers
, 19
78(s
ampl
e no
s.TM
0287
RD
.75
Dr0
14,
75M
S011
)
43T
.29N
..R.3
E.
0C
u(A
u.M
o)
Vei
n,
dls
- H
ydro
ther
mal
se
min
ated
ro
o
44 4S
T.28N..R.3E.
T.28N..R.4E.
Cu(Zn)
Disseminated
Volcanogenlc?
Ag.Cu
Disseminated
Hydr
othe
rmal
?
Quartz v
elnl
ets
with
pyrlte
cuttin
g py
rlte
-bea
rlng
alt
er
atio
n zone,
cont
aini
ng s
ome
malach
ite
stai
ns.
In m
afic
metavolcanlc r
ocks
of
unit P
zv.
Extent o
f mi
nera
lize
d altera
tion z
one
appe
ars
to b
e sm
all
Altere
d mafic
meta
volc
anlc
rocks of
unit
Pzv.
No
visi
ble
ore
minerals
Small breed a t
ed s
hear z
one,
with l
lmon
lte
and
mala
chit
e.
1n m
afic m
etav
olca
nlc
rock
s of
unit
Pzv
Miller a
nd
othe
rs,
1978
(sample
nos.
72Cy
073,
72
Cy06
1)
Miller a
nd
others,
1978
(sam
ple
no.
74Cy
062)
Mill
er a
nd
othe
rs,
1978
(sam
ple
no.
7SNw
l41)
cr
n>
co.
o o 3
rt C n>
o.
MINES, PROSPECTS, AN
D MI
NERA
L OC
CURR
ENCE
S IN
THE
TALKEETNA
MOUNTAINS
QUAD
RANG
LE,
ALAS
KA (continued)
MAP
NO.
AND
NAME
(S)
LOCA
TION
CATEGORY
(If
known)
46
T.28
N..R
.4E.
0
47
T.2B
N..R
.5E.
0
48
T.2B
N..R
.5E.
P
49
T.2BN..R.5E.
0
50
T.28
N..R
.5E.
0
51
T.2B
N..R
.5E.
0
52
T.28N..R.5E.
0
53
T.28
N..R
.9E.
P
54
T. ION. ,R. 10
H.
0
55
T.26N.R.1DE.
P
56 Go
ld Creek
T.25
-26N
..R.
9E.
P
RESOURCE (S)
Minor
cons
titu
ents o
r potential
bypr
oduc
ts in
parentheses
Cu
(Au.Ag)
Cu Cu
(Cu, Au.Ag)
(Ag.Cu)
(Cu)
Au(Pt)
(Zn) Au Au
FORM
Diss
emin
ated
Diss
emin
ated
Diss
emin
ated
Vein,
repl
acem
ent
Disseminated
...
Velnlets.
diss
emin
ated
Diss
emin
ated
Diss
emin
ated
Disseminated
Diss
emin
ated
TYPE
Hydr
othe
rmal
Hydr
othe
rmal
Volc
anog
enlc
?Hydrothermal?
Hydr
othe
rmal
?Su
bmar
ine
vol-
cano
genl
c?
Hydrothermal?
Porp
hyry
?
...
Hydrothermal?
Plac
er
Porp
hyry
?
Placer
Placer
BRIEF
DESC
RIPT
ION
Mino
r chalcopyrite and p
yrite
in s
mall a
lter
atio
n zone wit
hin
argi
lllt
e of u
nit
Pzv
Scattered
pyri
te I
n altered
phylllte o
f unit P
zv
Copp
er minerals
and
pyrite I
nma
fic
metavolcanic r
ocks o
funit P
zv
Pyrr
hotite a
nd c
halcopyrite
within g
reenstone of u
nit
Pzv.
Exte
nt o
f mi
nera
lize
d zone I
ssm
all
Minor
pyri
te,
pyrr
hoti
te,
and
chalcopyrite;
disseminated i
naltered
gneissose
quartz d
lo-
rlte
of
unit 4
pm
Floa
t of
vei
n quartz wit
hpy
rite
and c
halcopyrite
Minor
pyrrhotite a
nd c
halco
pyrite.
disseminated a
nd I
nve
inle
ts c
utti
ng a
ltered
metagabbro o
f un
it P
zv
Placer c
laims
alon
g upper
Busc
h Creek
Inci
sed
into
extensive
Quaternary s
ur-
fldal
depo
sits
Smal
l felslc v
olcanic
dike
with t
races
of p
yrite. cut
ting
greenstone of
unit
Jpm
Seve
ral
plac
er c
laim
s along
Oshetna
Rive
r
Several
placer c
laim
s along
Gold
Cre
ek I
n Quaternary a
llu
vium t
oo s
mall
to
show on
geol
ogic
map
PRIN
CIPA
L REFERENCES
Rose
. 19
67.
p. 5
Rose,
1967
. p. 4
MacKevett
and
Holl
oway
, 19
77
Rose,
1967
. p. 5
Rose.
1967
. p.
4
Anderson,
1969.
p. 10
-12
Rose
, 1967.
p. 4
U.S. Bu
r. Mi
nes.
1973
Mill
er a
ndothers.
1978
(sam
ple
no.
77Cy
070B
)
U.S. Bu
r. Mines,
1973
Chapln,
1918
. p.
64;
U.S. Bur.
Mines. 1973;
Cobb,
1972
-H cr CD CO O O =1 sj c CD 0.
*"-**
MINES, PR
OSPE
CTS,
AND
MINERAL O
CCURRENCES IN
THE T
ALKEETNA MOU
NTAI
NS Q
UADR
ANGL
E. A
LASKA
(continued)
ro
ro
HAP
NO.
AND
NAME
(S)
LOCATION
CATE
GORY
(1
f kn
own)
57
Granite
Cr««
k T.26N..R.9E.
P
58
T.26N..R.8E.
0
59
T.26
N..R
.8E.
P
60
Roaring
Creek
T.25
N..R
.8E.
P
61
T.25N..R.5E.
P
62
T.26
N..R
.6E.
0
63
T.26
N..R
.4E.
P
RESO
URCE
(S)
Mino
r constitu
ents o
r potential
FORM
bypr
oduc
ts In
parentheses
Au
Disseminated
Zn
Veln
lets
Cu(Au)
Vein?
Au
Disseminated
Au
Disseminated
(Sn.Zn)
Disseminated
Cu?,Au?
Veins?
TYPE
Placer
Hydrothermal
Hydrothermal?
Placer
Placer
Porphyry?
Hydrothermal?
BRIEF
DESCRIPTION
Plac
er c
laim
alo
ng l
ower
Granit
e Creek
Llmo
nlte
and
pyr
ite
along
frac
tures
1n s
mall
go
ssan
wit
hin
metaan
desl
te of
unit J
tk
Lode c
laim
s In g
rani
tic
rocks
of u
nit Jp
m
Plac
er c
laims
alon
g lower
Roaring
Cree
k
Seve
ral
placer claims
Tertia
ry,
pyrltlferous,
alter
ed a
ndeslte
dike
s cu
ttin
gdlorlt
e of u
nit Jp
m
Lode c
laims
In T
ertiary
vol
canic
rock
s
PRIN
CIPA
L REFERENCES
Chap
ln,
1918.
p. 6
4
Miller a
ndothers,
1978
(sample
no.
77Cy
080)
U.S.
Bu
r. M
ines.
1973;
MacK
evet
tan
d Ho Ho wa
y.1977
Chap
ln.
1918.
p. 64
U.S. B
ur.
Mines.
1973
Mill
er a
ndothers,
1978
(sample
no.
74Cy
078A
)
U.S.
Bur. Mines.
1973
; Ma
cKev
ett
and
Ho How
dy,
1977
I
o» cr n> CO o o =3 r* :a £= tt> a.
MINES. PROSPECTS, AN
D MINERAL
OCCURRENCES
IN T
HE T
ALKEETNA M
OUNTAINS Q
UADR
ANGL
E, A
LASK
A (continued)
ro CO
MAP
NO.
AND
NAME
(S)
LOCATION
CATE
GORY
(If
known)
64
T.26N..R.3E.
0
6$
T.26
N..R
.3E.
0
66
T.25N..R.3E.
0
6?
T.25N..R.3E.
0
66
T.25N..R.3E.
P
69
T.25
N..R
.2E.
0
70
T.26N..R.2E.
0
71
East
view
T.26N..R.2E.
P
72 Phoenix
T.26N..R.2E.
P
RESOURCE(S)
Minor
constitu
ents o
r po
tent
ial
FORM
bypr
oduc
ts In
pa
rent
hese
s
Ag.Cu(Au)
Cu(Sn)
(Mo)
Velnlets
Cu(Pb.Au)
Cu
Vein
?
Co.C
r,N1
(Zn.
Disseminated
Au)
Ag.M
ofPb
.Zn,
Disseminated
Au) Cu
Vein
Cu
Vein
TYPE r
Hydr
o the
rmal
Hydr
o the
rmal
?
Magroatlc? a
nd
(or)
hydro-
thermal?
Hydr
othe
rmal
?
Hydr
o the
rmal
Hydr
o thermal
BRIEF
DESC
RIPT
ION
Float
of v
ein
quartz w
ith
py-
rlte
, ch
alco
pyrl
te,
and
pos
sibly
pyrrnotlte
Floa
t of
vei
n quartz w
ith
pyrlte a
nd malachite s
tain
s
Pyrl
te-b
eaHn
g qu
artz
vel
nlet
s 1n
altered g
ranodlorlte
of
unit
Jpr
a
Float
of p
yrlte
and
malachite-
bear
ing
alte
red
granitic r
ock
Copper m
inerals, m
ainl
y mala
chit
e. In
bre
ccia
ted
gran
itic
rocks
of u
nit
Jpm.
Si
te o
f diamond
drilling I
n early
1970
* s.
Seve
ral
claims I
n ar
ea
Alte
red
mafi
c metavolcanlc r
ock,
po
ssib
ly s
erpentlnlte, o
f un
it
Pzv.
No v
isib
le o
re m
iner
als
Altered,
pyr
lte-
bear
Ing
f el s
ic
dike
of
unit
TV
cutting
mafi
c metavolcanlc r
ocks
of
unit P
zv
Quartz v
eins
, wi
th p
yrlte
and
chalcopyrlte,
cutt
ing meta-
andeslte o
f un
it P
zv
Chalcopyrlte,
hematite,
minor
bornlte. a
nd q
uart
z In v
ein-
PR IN
C I PA
L RE
FERE
NCES
Miller a
nd
othe
rs.
1978
(sam
ple
no.
TM00
66RA
)
Miller a
nd
others,
1978
(sam
ple
no.
73Cy
l26)
Miller a
nd
othe
rs,
1978
(sample
no.
TM0103RB)
Miller a
nd
othe
rs.
1978
(sample
no.
TM0104R)
MacKevett
and
Ho How
ay.
1977;
U.S. Bur. M
ines
. 1973
Miller a
nd
othe
rs.
1978
(s
ampl
e nos.
TM0050RA.
TM00
50KB
, TM
OOSO
RC)
Milter and
othe
rs.
1978
(sample
nos.
TM0107RB,
TM01
07RE
)
Capp
s. 19
l9b.
p.
20
3
Capp
s. 19
19b,
p.
20
2
CU cr
n> 3.
(continued)
lets c
utti
ng s
heared m
eta-
ande
slte
of
unit
Pzv
MINE
S. PR
OSPE
CTS.
AND
MIN
ERAL
OCC
URRE
NCES
IN
THE T
ALKE
ETNA
MOUNTAINS Q
UADR
ANGL
E. A
LASKA
(con
tinu
ed)
ro
RESO
URCE
(S)
Mino
r co
nstk
u-
MAP
NO.
AND
NAME(S)
LOCATION
CATE
GORY
ents o
r potential
(If
know
n)
bypr
oduc
ts In
parentheses
73 Bl
ue L
ode
T.26
N..R
.2E,
P
Cu
74
Ice Creaa
T.26
N..R
.2E.
P
CuMo
unta
in,
Rainbow Lake
75 Ta
lkee
tna
T.26N..R.2E.
P Cu.Ag(Au.Mo)
76
T.26N..R.2E.
P Cu
"
T.26
N..R
.3E.
0
Cu(Pb)
FORM
TYPE
Vein,
Hydrothermal
repl
acem
ent
Vein
? Hydrothermal 1
Vein,
Hydrothermal
disseminated
Vein
? Hydrothermal
Disseminated?
Diss
emin
ated
. Hydrothermal
vein
BRIE
F DE
SCRI
PTIO
N
Chal
copy
rlte
and
bornlte 1
ngo
uge
within met
aand
eslt
e of
unit
Pzv
Seve
ral
lode cla
ims
1n m
afic
meta
volc
anlc
rocks o
f unit
Pzv.
Probably s
tme
geol
ogic
cond
itions a
s In t
he E
astv
lew.
Phoe
nix,
and
Blue
Lode
claims
Repl
acem
ent
lodes
alon
g shear
zone
s an
d In a
djacent
wall
rock
of ma
fic
metavolcanlc
rock
s of
unit
Pzv.
Th
e lodes
cont
ain
Chal
copy
rlte
, he
mati
te.
pyri
te,
and
quar
tz.
Several
lode
claims
1n a
rea
Several
lode
claims
1n m
afic
meta
volcanlc r
ocks
of
unit P
zv
Smal
l re
plac
emen
t lo
des
and
veln
lets w
ith
Chalcopyrlte 1
nalte
red mafic
metavolcanlc
rock
s of u
nit
Pzv
PRIN
CIPA
L REFERENCES
Capp
s. I9
19b.
p. 202-203
U.S.
Bu
r. M
ines
,19
73
Capp
s. 1919b. p
.20
3-20
4; M
iller
and
othe
rs,
1978
(sam
ple
nos.
73Cyl23, 7S
Cy12
7)
U.S. Bur. Mi
nes.
1973
Mill
er a
ndot
hers
. 19
78(s
ampl
e no.
73Cy
l22)
-H
cu cr n> CO
* o o 3 <-*
=3 C a.
MINES, PROSPECTS, A
ND MIN
ERAL
OCC
URRE
NCES
IN
THE T
ALKEETNA H
OUNT
AINS
QUA
DRAN
GLE.
ALASKA
(continued)
f\3
cn
MAP
NO.
AND
NAME(S)
LOCA
TION
CA
TEGO
RY
(If
know
n)
78
T.27
N..R
.3E.
0
79 Copper W
onde
r T.
26N.
.R.2
E.
P
60
T.26
N..R
.2E.
0
81
Copper K
ing
T.26
N..R
.1E.
P
82
Iron C
reek,
T.26
N..R
.1E.
P
Morning
Star
83 Co
pper
Que
en
T.26
N..R
.1E.
P
84
T.27N..R.2E.
0
85
T.27N..R.1E.
P
86
T.27N..R.1E.
0
RE SO
URCE (S
) Minor
constitu
ents o
r potential
bypr
oduc
ts In
parentheses
(Cr)
Cu(Fe)
Zn(Pb.Au)
Cu.A
u.Ag
Cu
Cu.Au
Cu,A
g(Au
,Zn,
Pb)
Au (Mo)
FORM
TYPE
Disseminated
Volc
anog
enlc
?
Vein
, Hy
dro t
herm
alre
plac
emen
t
Vein,
Hydrothermal
disseminated
Diss
emin
ated
, Hydrothermal
vein
s
Veins?
Hydrothermal?
Diss
emin
ated
. Hydrothermal
replacement
Vein
Hydrothermal
Disseminated
Placer
...
...
BRIEF
DESC
RIPT
ION
Alte
red
mafi
c me
t* vo
lcan
icrock
of
unit
Pzv
. No
vis
ible
ore
Minerals
Chal
copy r
ite,
hem
atit
e, pyrlte,
and
quar
tz I
n a
zone
of
shea
red
meta
andeslte of
unit
Pzv
Diss
eminated p
yrlt
e an
d Qu
artz
veln
lets In
alt
ered
mafic m
eta-
volc
anlc
roc
k of
uni
t Pz
v
Chal copy r
ite, h
emat
ite,
pyrlte,
and
quar
tz I
n zo
ne o
f sh
eare
dmetaan
desl
te o
f un
it P
zv
Severa
l lo
de c
laim
s In
maf
icme ta
volc
anic
roc
ks o
f un
it P
zv.
Geolog
ic c
onditions
probably
simi
lar
to t
hat
of t
he
Copp
erKing
claim
Pyrlte,
chal
copy
rlte
. ar
seno
-pyrl
te,
and
quar
tz I
n a
zone of
sheared
and al
tere
d mafic
meta
-volcan
lc r
ocks o
f un
it P
zv.
Expo
sure
1s along
the
bank
of
Iron C
reek I
n a
rock
bluff t
oosmall
to s
how on g
eolo
gic ma
p
Quartz
vein, a
bout 6
0 cm t
hick
.wi
th c
halcopyrlte, p
yrlte, a
ndmalach
ite
stai
ns.
Coun
try
rock
Is m
afic m
eta v
olcanic
rock o
funit P
zv
Placer
claims
along
smal
l creek
In a
lluv
ium
too
smal
l to
show
on g
eologic ma
p
Float of
alt
ered
granodlorlte
with
disseminated
pyrl
te
PRIN
CIPA
L RE
FERE
NCES
Miller a
ndothers,
1978
(sample
no.
TM00
57R)
Capps, 19
19b.
p. 201-202
Mill
er and
others.
1978
(sample
no.
7SCy044)
Capps, 19
19b.
p. 201
U.S. Bu
r. M
ines
.1973
Capps, 1919b, p
.199-201
Mill
er a
ndot
hers
. 1978
(sam
ple
nos.
73Cy
l24,
7SCy009A)
U.S. Bu
r. M
ines.
1973
Mill
er and
othe
rs,
1978
(sam
ple
no.
TM184RB)
-H o>
cr n> CO 'rT o 3
r* _ i.
=3
C n>
0. **-"
NINES, PROSPECTS. A
ND M
INER
AL O
CCUR
RENC
ES I
N THE TA
UEET
NA M
OUNTAINS Q
UADR
ANGL
E, A
LASK
A (continued)
ro
en
HAP
NO.
AND
NANE(S)
LOCA
TION
CA
TEGO
RY
(If
know
n)
87
T.26N..R.1W.
0
88
T.2S
N..R
.1U.
P
89
T.25N..R.1W.
0
90
T.25N..R.1H.
0
RESO
URCE
(S)
Minor
constitu
ents o
r potential
FORM
TYPE
byproducts In
pa
rent
hese
s
Ag,A
s,Cu
,Zn(
Pb)
Disseminated
Hydrothermal
Cu.M
o(Pb
.Au.
Zn)
Disseminated
Porp
hyry
(Cu.2n.Au)
(Pb.
Sn.A
u)
BRIE
F DESCRIPTION
Dark-red t
o ye
l low, p
y rit
e-
bearin
g go
ssan
In
mafi
c ro
eta-
volcanlc r
ocks
of
unit
Pzv.
No v
isib
le o
re m
inerals
Copper minerals
and molyb
deni
te d
isse
mina
ted
1n a
lter
edTe
rtia
ry g
ranitic
rock o
f un
itun
it T
bgd
Float
of p
yrlte-bearlng an
d sl
llclfled g
rani
tic
rock
Float
of p
yrlt
e-be
arln
g vein
quar
tz
PRIN
CIPA
L REFERENCES
Miller and
ot
hers
. 19
78(s
ampl
e no.
7SDr
002)
MacK
evet
t an
d Ho
llow
ay.
1977
;Mi
ller
and
othe
rs,
1978
(sample
nos.
75Cy
l57B
, 77Cy01Q,
TM02
4RB.
TM
024R
O,TM
024R
A)
Mill
er a
nd
others,
1978
(sam
ple
no.
TM00
15RB
)
Mill
er a
ndothers,
1978
(sam
ple
nos.
THOOI7RB.
TM0017RC.
TM0017RE)
-H
O> cr o> CO ^x0 o 3 c* 3* C n> 0.
NINES, PROSPECTS. A
ND M
INER
AL O
CCUR
RENC
ES IN T
HE T
ALKEETNA M
OUNTAINS QUA
DRAN
GLE.
ALASKA
(continued)
ro
NAP
NO.
AND
NAHE
(S)
LOCA
TION
CA
TEGO
RY
(if
know
n)
91
T.24
N..R
.2H.
0
92
T.24
N..R
.2W.
0
93
T.23
N..R
.3U.
P
94
T.23N..R.1E.
P
95
T.23
N..R
.1E.
P
96
T.24N..R.1E.
0
97
T.24N..R.2E.
0
96
T.24N..R.2E.
0
99 Mazum
Creek.
T.22
-23N
..R.
9E.
PCa
ribo
u Creek
100
T.23
-24N
..R.
10E.
P
RESO
URCE
(S)
Minor constitu
ents
or
pote
ntia
l FO
RM
bypr
oduc
ts I
n parentheses
(Cr.
Sb.S
n)
Diss
emin
ated
(Ag.
Sn.Z
n.Au
) Di
ssem
inat
ed
Au
Diss
emin
ated
Cu.Au.Ag
Vein
?*
Au?
Vein
?
Afl.
Cu(A
u)
Cr(N
I.Sb
)
Ag,Cu(Pb,Au)
Au
Diss
emin
ated
Au
Disseminated
TYPE
Porphyry?
Hydr
o the
rmal
?
Hydrothermal?
Volc
anog
enlc
?
Placer
Hydr
othe
rmal
?
Kydrothermal?
...
...
...
Placer
Placer
BRIEF
DESC
RIPT
ION
Altered
granitic r
ock
of u
nit
TKg wi
th mafic m
etavolcanic
xeno
llth
s.
No v
isib
le o
reminerals
Altered metaandeslte o
f unit
Pzv.
No v
isible o
re m
inerals
Placer c
laims, lo
cati
on u
ncer
tain
Lode
claims
In t
onal
He o
funit T
Kt
.--...
..-.
..Hn
............
Floa
t of
vei
n quartz w
ith
py-
rlte
, chalcopyrUe, a
nd mala
chite
stai
ns
Several
float
samp
les
of a
lter
ed m
afic m
etavolcanic
rock
s,po
ssib
ly s
erpe
ntln
lte.
No
visi
ble
ore
mine
rals
Floa
t of mal
achi
te-s
tain
edgr
anit
ic r
ock
Several
placer c
laims
along
Mazuma C
reek
and C
aribou C
reek
In a
lluvium
too
smal
l to s
how
on g
eolo
gic
map
Seve
ral
plac
er c
laim
s along
upper
Little Nel
cMna
Riv
er 1
n
PRINCIPAL
REFE
RENC
ES
Miller a
ndothers.
1978
(sam
ple
no.
74Cy
029A
)
Miller a
ndothers,
1978
(sam
ple
no.
74Cy
030)
U.S. Bu
r. N
ines.
1973
Do
.
. Do
.
Miller a
ndot
hers
. 19
78(s
ampl
e no.
72CyllO)
Miller a
ndot
hers
. 19
78(s
ampl
e no
s.74Cy097A,
74Cy
097C
.74Cy097D)
Mill
er and
othe
rs.
1978
(sample
no.
74Cy096)
Martin a
ndHe
rtle
, 1914.
p.27
9-28
0; U
.S.
Bur.
Mine
s. 1973;
Cobb.
1973.
p. 19
U.S. Bur. M
ines
.19
73
tu cr n> CO o' o =J rt-
i.
3 C n> ex
alluvium t
oo s
mall
to s
how
on
geol
ogic
map
MINLi. PKUSPECIS, ANU
MINE
RAL
OCCU
KKEN
CES
IN T
HE TA
LKEE
TNA
MOUNTAINS
QUADRANGLE,
ALASKA (
continued)
oo
MAP
NO.
AND
NAME
(S)
(If
know
n)
101
Yacko
Cree
k
102
Four
th o
f Ju
ly Cre
ek
103
T.6N
..R.
10U.
104
Dais
y Cr
eek
105
106
107
LOCA
TION
CATEGORY
T.25N..R.11E.
P
T.25-26N..R.12E.
P
T.6N
..R.
10U.
P
T.6N
..R.
10U.
. P
T.25N..R.12E.
T.25N..R.12E.
P
T.4N.,«,)OW.
P
T.3N..R.10W.
P
RESOURCE(S)
Mino
r constitu
ents or p
oten
tial
FORM
TYPE
bypr
oduc
ts In
parentheses
Au
Disseminated
Placer
Au
Disseminated
Placer
Au
Disseminated
Placer
Au
Disseminated
Placer
Au
Disseminated
Placer
Au
Disseminated
Placer
Au
Disseminated
Placer
BRIE
F DE
SCRI
PTIO
N
Severa
l pl
acer
claims
alon
g Yacko
Creek
1n a
lluv
ium
too
small
to s
how on
geo
logi
c map.
Poss
ibly s
ome
minor
production
Seve
ral
placer c
laim
s along
Four o
f Ju
ly C
reek I
n al
luvi
um
too
smal
l to s
how on
geologic
map
Seve
ral
plac
er claims
In a
llu
vium
too
sma
ll to
show on
geolog
ic m
ap
Several
placer c
laim
s along
Dais
y Creek
tn a
lluvium
Seve
ral
placer cla
ims
along
uppe
r Daisy
Creek
In a
lluv
ium
too
smal
l to s
how
on g
eologic
map
Seve
ral
placer claims
Placer cla
im alo
ng Old
Man
r ..
*>»!
.
PRIN
CIPA
L RE
FERE
NCES
Chapln,
1918.
p.
64;
U.S.
Bur.
Mine
s. 1
973
Chap
ln.
1918
. p.
64;
Cobb.
1972
U.S.
Bu
r. M
ines
. 1973
Chap
ln.
1918
. p.
64;
Cobb
. 1972;
U.S.
Bur. Mi
nes.
1973
U.S. Bur. M
ines.
1973
Do
.--
Do.
\ o> cr n> CO
0 o 3 c+
_i.3 C n> 0.
MINES. PR
OSPE
CTS,
AND
MINERAL
OCCURRENCES
IN T
HE TALKEETNA
MOUNTAINS
QUADRANGLE.
ALAS
KA (continued)
MAP
NO.
AND
NAME(S)
LOCA
TION
CATEGORY
(If
known)
108
Croo
ked
Creek
T.23N..R.12E.
P
109
Willow C
reek
T.23N..R.12E.
P
110
North
Creek
T.22
-23N
..R.
12E.
P
111
Albert C
reek
T.22
N..R
.11-
12E.
M
112
T.22
N..R
.11E
. 0
RESOURCE(S)
Mino
r co
nsti
tu
ents o
r potential
FORM
TYPE
byproducts In
parentheses
Au
Diss
emin
ated
Pl
acer
Au
Diss
emin
ated
Placer
Au
Disseminated
Placer
Au(P
t)
Diss
emin
ated
Placer
Zeol
ites
Di
ssem
inat
ed
Dlagenlc a
ndme
tamo
rphl
c
BRIE
F DE
SCRI
PTIO
N
Placer c
laim
s along
lower
Croo
ked
Cree
k
Old
placer cla
im along
Will
ow C
reek
Seve
ral
placer c
laims
along
North
Creek
In a
lluvium
too
smal
l to s
how on
geo
logi
c ma
p
Also
Inc
luded
several
other
claims a
long
Albert
Cree
k In
allu
vium
too
sma
ll to
show
ongeologic m
ap.
Old
Albe
rtCr
eek
plac
er p
rodu
ced
abou
t15
0 02
gold
during 1
914
(Chapln.
191B).
This
Is
the
only p
lacer
deposit
In q
uadr
angl
e with
prov
en,
thou
gh minor,
production
In H
orn
Moun
tain
s an
d Albert
Cree
k region,
extensive
de
posi
ts o
f mordenlte
and
othe
rVA
/\I 4+AC «i
f nneeiKl* Af
rtnr
tmft
f*
PRINCIPAL
REFERENCES
Chap
ln.
1918.
p. 60
-61
U.S. B
ur.
Mines.
1973;
Chap
ln.
1918.
p. 62
Martin a
ndMe
rtle
. 19
14.
p.278; U
.S.
Bur.
Mine
s, 19
73
Chap
ln.
1918
. p.
S9-6
2; M
arti
n.19
20.
p. 2
3; C
obb*
1972;
U.S. Bur.
Mine
s. 1
973;
Cob
b.1973.
p. 29
Hawklns. 1
976;
MacKevett
and
Holl
oway
. 19
77
H tu cr o> CO ^-^o o 3 <-f
j. rj c n>
o.
1U McOougil C
reek
T.
22N.
.R.1
1E.
AuDi
ssem
inat
ed
Placer
Interest
; lo
cali
zed
In t
uffa
- ce
ous
part o
f Lower Ju
rass
ic
Talkeetn
a Formation.
Similar
deposits
probably oc
cur
else
wher
e In
Tal
keet
na M
ount
ains
quadrang
le
Seve
ral
placer cla
ims
alon
g McOougal
Creek
In a
lluv
ium
too
smal
l to
sho
w on
geologic
map
U.S.
Bur. M
ines
, 19
73
References Cited
Anderson, R.E., 1969, Preliminary geochemistry and geology, Little Falls Creek area, Talkeetria Mountains quadrangle, Alaska: Alaska Division of Mines and Geology Geochemical Report 19, 16 p.
Berg, H.C., and Cobb, E.H., 1967, Metalliferous lode deposits of Alaska: U.S. Geological Survey Bulletin 1246, 254 p.
Capps, S.R., 1919a, Mineral resources of the upper Chulitna region: U.S. Geological Survey Bulletin 692, p. 207-232.
___1919b, Mineral resources of the Western Talkeetna Mountains: U.S. Geological Survey Bulletin 692, p. 187-205.
Capps, S.R., and Short, M.N., 1926, A ruby silver prospect in Alaska: U.S. Geological Survey Bulletin 783, p.89-95
Chapin, Theodore, 1918, The Nelchina-Susitna region, Alaska: U.S. Geological Survey Bulletin 668, 67 p.
Cobb, E.H., 1972, Metallic mineral resources map of the Talkeetna Mountains quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-370.
1973, Placer .deposits of Alaska: U.S. Geological Survey Bulletin 1374,213 p.
Csejtey, Bela, Jr., Nelson, W.H., Jones, D.L., Silberling, N.J., Dean, R.M., Morris, M.S., Lanphere, M.A., Smith, J.G., and Silberman, M.L., 1978, Reconnaissance geologic map and geochronology, Talkeetna Mountains quadrangle, northerm part of Anchorage quadrangle, and southwest corner of Healy quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-558A, 60 p., 1 sheet, scale 1:250,000.
Csejtey, Bela, Jr., and Miller, R.J., 1978, Map and table describingmetalliferous and selected nonmetalliferous mineral deposits in the Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-558-B. 1 sheet, 20 p.
Csejtey, Bela, Jr., and Griscom, Andrew, 1978, Preliminary aeromagnetic interpretive map of the Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-558-C, scale 1:250,000, 14 p.
Grantz, Arthur, 1956, Possible orgin of the placer gold deposits of the Nelchina area, Alaska, (Abs.): Geol. Soc. America Bull., v. 67, p.1807.
30
Hawkins, D.B., 1976, Mordenlte deposits and zeolite zonation in the HornMountains area, south-central Alaska: Alaska Division of Geologicaland Geophysical Surveys Special Report 9, 9 p.
MacKevett, E.M., Jr., and Holloway, C.D., 1977, Map showing metalliferous and selected nonmetalliferous mineral deposits in the eastern part of southern Alaska: U.S. Geological Survey Open-File Map 77-169A.
Martin, G.C., 1920, The Alaskan mining industry in 1918: U.S. Geological Survey Bulletin 712, p. 11-52.
Martin, G.C., and Mertie, J.B., Or., 1914, Mineral resources of tKe upper Matanuska and Nelchina valleys: U.S. Geological Survey Bulletin 592, p. 273-299.
Menzie, W.D., and Singer, D.A., in press, Some quantitative properties of mineral deposits, in Meyer, R.F., ed., Small Scale Mining of the World New York, McGraw-HTTl.
Miller, R.J., Curtin, G.C., and Csejtey, Bela, Jr., 1978a, Map showinggeochemical distribution and abundance of tin in stream sediments and heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-558-E, 1 sheet, scale 1:250,000.
Miller, R.J., Curtin, G.C., and Csejtey, Bela, Jr., 1978b, Map showing geochemical distribution and abundance of zinc in stream sediments and heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska U.S. Geol. Survey Open-File Report 78-588-F, 1 sheet, scale 1:250,000.
Miller, R.J., Curtin, G.C., and Csejtey, Bela, Jr., 1978c, Map showing ' geochemical distribution and abundance of silver, in stream sediments and heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-558-G, 1 sheet, scale 1:250,000.
Miller, R.J., Curtin, G.C. and Csejtey, Bela, Jr., 1978d, Map showing geochemical distribution and abundance of gold in stream sediments and heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska U.S. Geol. Survey Open-File Report 78-558-H, 1 sheet, scale 1:250,000.
Miller, R.J., Curtin, G.C., and Csejtey, Bela, Jr., 1978e, Map showinggeochemical distribution and abundance of copper, in stream sediments and heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska U.S. Geol. Survey Open-File Report 78-558-1, 1 sheet, scale 1:250,000.
Miller, R.J., Curtin, G.C., and Csejtey, Bela, Jr., 1978f, Map showing geochemical distribution and abundance of lead in stream sediments and heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-558-J, 1 sheet, scale 1:250,000.
31
Miller, R.J., Curtin, G.C., and Csejtey, Bela, Jr., 1978g, Map showing geochernical distribution and abundance of molybdenum in stream sediments and heavy mineral concentrates, Talkeetna Mountains quad rangle, Alaska: U.S. Geol. Survey Open-File Report 78-558-K, 1 sheet, scale 1:250,000.
Miller, R.J., Curtin, G. C. and Csejtey, Bela, Jr., 1978h, Map showinggeochemical distribution and abundance of bismuth in stream sediments and heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-558-L, 1 sheet, scale 1:250,000.
Miller, R.J, Curtin, G.C. and Csejtey, Bela, Jr., 1978i, Map showinggeochemical distribution and abundance of chromium in stream sediments and heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-558-M, 1 sheet, scale 1:250,000.
Miller, R.J., Curtin, G.C., and Csejtey, Bela, Jr., 1978J, Map showing geochemical distribution and abundance of tungsten in heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-588-N, 1 sheet, scale 1:250,000.
Miller, R.J., Curtin, G.C., and Csejtey, Bela,'Jr., 1978k, Map showing geochemical distribution and abundance of barium in heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-588-0, 1 sheet, scale 1:250,000.
Miller, R.J., Curtin, G.C., and Csejtey, Bela, Jr., 19781, Map showing geochemical distribution and abundance of arsenic in heavy mineral concentrates, Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-588-P, 1 sheet, scale 1:250,000.
Miller, R.J., Cooley, E.F., O'Leary, R.M., Garmezy, Larry, Csejtey, Bela, Jr., Smith, T.E., and Cleveland, M.N., 1978, Analyses of geochemical samples from the Talkeetna Mountains quadrangle, Alaska: U.S. Geol. Survey Open-File Report 78-1052, 279 p.
Reed, B.L., 1978, Disseminated tin occurrence near Coal Creek, Talkeetna Mountains D-6 quadrangle, Alaska: U.S. Geol.Survey Open-File Report 78-77, 8 p.
Richter, D.H., 1963, Geology of the Portage Creek-Susitna River area, Alaska: Alaska Division of Mines and Minerals Geologic Report 3, 2 sheets.
Rose, A.W., 1967, Geology of an area on the upper Talkeetna River, Talkeetna Mountains quadrangle, Alaska: Alaska Division of Mines and Minerals Geologic Report 32, 7 p.
32
Singer, D.A., 1975, Mineral resource models and the Alaskan Mineral Resource Assessment Program: in Vogely, W.A., ed., "Mineral Materials Modeling," Resources for the Future, p. 370-382.
Singer, D.A., and Ovenshine, A.T., 1979, Assessing metallic resources in Alaska: American Scientist, v. 67, no. 5, p. 582-589.
Smith, I.E., Bundtzen, T.K., and Trible, T.C., 1975, Stratabound copper- gold occurrence, northern Talkeetna Mountains, Alaska: Alaska Division of Geological and Geophysical Surveys Miscellaneous Paper 3, 7 p.
U.S. Bureau of Mines, 1973, Alaska 1:250,000 scale quadrangle map overlays showing mineral deposit locations, principal minerals, and number and type of claims: U.S. Bureau of Mines Open-File Report 20-73.
33