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WARD

NEDERLAND

GRAYS PEAK

ELDORADO SPRINGS

MOUNT RICHTHOFEN

BUCKHORN MOUNTAIN HORSETOOTH RESERVOIR

MASONVILLE

PANORAMA PEAK

DW-105

DW-107 DW-111

DW-094

DW-114DW-113

DW-106

DW-093DW-110

DW-112 DW-098

DW-109DW-099

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DW-092

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DW-115

EP-066

EP-067EP-015

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DW-172DW-067

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DW-118 EP-004DW-090DW-096

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DW-095EP-005

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EP-009 EP-080

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DW-137-141,148-171, 226-228

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DW-047DW-058

DW-027DW-024 DW-215

DW-025

DW-222DW-221DW-038

DW-041DW-037

DW-080

FC-019

FC-027

FC-020FC-021

FC-018FC-001

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FC-022

FC-025FC-002

FC-028

EP-065EP-064

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EP-020

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EP-087

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EP-031

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BA-067

BA-072

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EP-097

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CRAZY MOUNTAIN

GLENDEVEY

RAWAH LAKES

CLARK PEAK

BOWEN MOUNTAIN

TRAIL MOUNTAIN

GRANBY

BOTTLE PASS

BYERS PEAK

LOVELAND PASS

KEYSTONE

BOREAS PASS

COMO

FAIRPLAY EAST

GARO

SAND CREEK PASS

DEADMAN

BOSTON PEAK

CHAMBERS LAKE

FALL RIVER PASS

GRAND LAKE

SHADOW MOUNTAIN

STRAWBERRY LAKE

FRASER

BERTHOUD PASS

MONTEZUMA

JEFFERSON

MILLIGAN LAKES

ELKHORN

HARTSEL

EATON RESERVOIR

SOUTH BALD MOUNTAIN

KINIKINIK

COMANCHE PEAK

TRAIL RIDGE

MCHENRYS PEAK

ISOLATION PEAK

MONARCH LAKE

EAST PORTAL

EMPIRE

GEORGETOWN

MOUNT EVANS

MOUNT LOGAN

OBSERVATORY ROCK

EAGLE ROCK

SULPHUR MOUNTAIN

DIAMOND PEAK

RED FEATHER LAKES

RUSTIC

PINGREE PARK

ESTES PARK

LONGS PEAK

ALLENS PARK

CENTRAL CITY

IDAHO SPRINGS

HARRIS PARK

SHAWNEE

TOPAZ MOUNTAIN

FARNUM PEAK

GLENTIVAR

CHEROKEE PARK

HAYSTACK GULCH

BIG NARROWS

CRYSTAL MOUNTAIN

GLEN HAVEN

RAYMOND

GOLD HILL

TUNGSTEN

BLACK HAWK

SQUAW PASS

MERIDIAN HILL

BAILEY

WINDY PEAK

MCCURDY MOUNTAIN

TARRYALL

VIRGINIA DALE

LIVERMORE MOUNTAIN

POUDRE PARK

DRAKE

PINEWOOD LAKE

LYONS

BOULDER

RALSTON BUTTES

EVERGREEN

CONIFER

PINE

GREEN MOUNTAIN

CHEESMAN LAKE

HACKETT MOUNTAIN

TABLE MOUNTAIN

LIVERMORE

LAPORTE

CARTER LAKE RESERVOIR

HYGIENE

NIWOT

LOUISVILLE

GOLDEN

MORRISON

INDIAN HILLS

PLATTE CANYON

DECKERS

WESTCREEK

SIGNAL BUTTE

ROUND BUTTE

BUCKEYE

WELLINGTON

FORT COLLINS

LOVELAND

BERTHOUD

LONGMONT

ERIE

LAFAYETTE

ARVADA

FORT LOGAN

LITTLETON

KASSLER

DEVILS HEAD

DAKAN MOUNTAIN

MOUNT DECEPTION

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OPEN-FILE REPORT 2006-1051SHEET 2 of 2

Version 1.0

105°00'

SAMPLE LOCATIONS

These maps, and the tables that accompany them, are a compilation of isotopic age determinations of rocks and minerals in four 1:100,000-scale quadrangles in the northern and central Front Range, Colorado. Phanerozoic (primarily Tertiary and Cretaceous) agedata are shown on one map; Proterozoic data are on the other (sheet 1). A sample locationmap (sheet 2) is included for ease of matching specific localities and data in the tables to the maps. Several records in the tables were not included in the maps because either there were ambiguous dates or lack of location precluded accurate plotting.

Introduction

To illustrate the geological setting for the samples, the plutonic rocks are shown on the maps. The boundaries of the plutons are from the Geologic Map of Colorado (Tweto, 1979; digital version by Green, 1992) with a few modifications (Gable, 1984; A.B. Wilson, 2004, unpub. data). For ease of reference, we labeled each of the larger (and some of the smaller) plutons with a generally accepted name from the literature. As a convenience in using the data, we have informally named some plutons based on geographic features on or near those plutons. Those names are shown in parentheses.

The maps show the type of age determination by symbol and age subdivisions by color. Seven different methods, each shown with a different symbol, were used to determine Phanerozoic ages: Ar/ Ar (circles), Rb/Sr (crosses), K-Ar (stars), U/Pb (squares), zircon fission track (diamonds), sphene fission track (inverted triangles), and apatite fission track (triangles). Four different methods were used to determine Proterozoic ages: Ar/ Ar (circles), Rb/Sr (crosses), K-Ar (stars), and U/Pb (squares).

Many age determinations have been made on samples which were not located precisely on published maps, although some were located on small-scale geologic sketch maps. We located those samples as best we could on published 1:24,000-scale geologic maps and determined a latitude and longitude for that location. These uncertain or imprecise locations are indicated in the tables by a footnote and on the maps they are shown with open, or unfilled, symbols in the same shapes as explained previously.

Many ages in these tables were determined before the use of the currently accepted values for the decay and abundance constants recommended by the IUGS Subcommission on Geochronology (Steiger and Jäger, 1977). We have corrected the K-Ar ages that used the older decay constant (40K/K=1.19x10-4 mol/mol) and abundance constants generally used in the Western World to ones based on the currently accepted decay constant (40K/K=1.167x10-4 mol/mol) by using the tables of Dalrymple (1979). We have corrected the Rb/Sr ages that used the older decay constant (87Rbλ=1.39x10-11/yr) to ones based on the currently accepted constant ( 87Rbλ=1.42x10-11/yr) by multiplying the age by 0.9788.

On the two maps intrusions of similar ages are highlighted in color, and the dated samples of each age group are shown in the same color. On the map showing Proterozoic ages, samples are divided into mostly Early Proterozoic (1,900–1,500 Ma; green) and Middle and Late Proterozoic (1,500–540 Ma, but mostly Middle Proterozoic; purple). On the map showing Phanerozoic ages samples are divided into six groups: Paleozoic and Mesozoic (540–80 Ma; yellow); Late Cretaceous to early Eocene ("Laramide"; 80–50 Ma; blue), early and middle Eocene (50–40 Ma; pale blue); middle Eocene to early Oligocene (40–30 Ma; pink), early Oligocene to early Miocene (30–20 Ma; magenta); and early Miocene and younger (20–0 Ma, but mostly Miocene; red).

Additional isotopic age data were intentionally not included in this compilation because the data are unreliable. This includes early attempts to date rocks based on chemical determinations of total uranium and lead in pitchblende in some samples from the Central City district. For the older isotopic age determinations on these uranium-bearing minerals see Marvin and others (1974). Phair (1979) discussed and corrected some of these data and concluded that there were two groups of ages at 58 Ma and 72.5 Ma.

References Cited

Dalrymple, G.B., 1979, Critical tables for conversion of K-Ar ages from old to new constants: Geology, v. 7, p. 558–560.

Gable, D.J., 1984, Geologic setting and petrochemistry of the Late Cretaceous-Early Tertiary intrusives in the northern Front Range Mineral Belt: U.S. Geological Survey Professional Paper 1280, 33 p., scale 1:48,000.

Green, G.N., 1992, The Digital Geologic Map of Colorado in ARC/INFO Format: U.S. Geological Survey Open-File Report OF-92-0507, scale 1:500,000.

Marvin, R.F., Young, E.J., Mehnert, H.H., and Naeser, C.W., 1974, Summary of radiometric age determinations on Mesozoic and Cenozoic igneous rocks and uranium and base metal deposits in Colorado: Isochron/West, n. 11, 41 p.

Phair, George, 1979, Interpretation of lead-uranium ages of pitchblende deposits in the Front Range, Colorado: Geological Society of America Bulletin, Part 1, v. 90, p. 858–870.

Steiger, R.H., and Jäger, E., 1977, Subcommission on geochronology: Convention on use of decay constants in geo- and cosmochronology: Earth and Planetary Science Letters, v. 126, p. 359–362.

Tweto, Ogden, 1979, Geologic map of Colorado: U.S. Geological Survey, scale 1:500,000.

40 39

40 39

106°00'41°00'

40°30'

40°00'

39°30'

39°00'

U.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY

5 0 10 15 20 25 30 KILOMETERS

SCALE 1: 250 000105 0 5 15 20 MILES

e Bryant

ISOTOPIC AGES OF ROCKS IN THE NORTHERN FRONT RANGE,

Anna B. Wilson and Bruc

2006

COLORADO

5

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