note : the geochemical analyses were performed at the

12
16?. NOTE : The Geochemical analyses were performed at the Anglo American Research Laboratories between August 1979 and April 1980. Major element detection was carried out using X-ray fluorescence techniques. The low totals may be due to the presence of other elements which were not detected. Repeatedly low results could reflect inaccurate calibration of the detection crystal, however it is unclear as to the precise reasons for the low totals. Trace element analyses were carried out using atomic absorption and semiquantitative spectrographic techniques. Moisture content is not included in the totals.

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Page 1: NOTE : The Geochemical analyses were performed at the

16?.

NOTE :

The Geochemical analyses were performed at the Anglo

American Research Laboratories between August 1979 and

April 1980. Major element detection was carried out using

X-ray fluorescence techniques. The low totals may be due

to the presence of other elements which were not detected.

Repeatedly low results could reflect inaccurate calibration

of the detection crystal, however it is unclear as to the

precise reasons for the low totals.

Trace element analyses were carried out using atomic

absorption and semiquantitative spectrographic techniques.

Moisture content is not included in the totals.

Page 2: NOTE : The Geochemical analyses were performed at the

CHAPTER IX

References

Page 3: NOTE : The Geochemical analyses were performed at the

163.

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ANDERSON, G.

ANDERSON, G.

ANDERSON, W.

ANHAEUSSER,

ASSEREIO, R.

ASSERETO, R.

BARNES, H. I

BARTON, P. (

BATHURST, R

BEALES, F. I

BEUKES, N. .

BISCHOFF, J

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Page 12: NOTE : The Geochemical analyses were performed at the

Author Clay A N Name of thesis The geology of the Malmani Dolomite Subgroup in the Carletonville area, Transvaal 1981

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