ELEMENTAL COMPOSITION AND NUCLEAR PARAMETERS OF SOME COMMON SEDIMENTARY MINERALS

被引:0
|
作者
HERRON, MM
MATTESON, A
机构
来源
NUCLEAR GEOPHYSICS | 1993年 / 7卷 / 03期
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中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Major and trace element chemistry has been used to investigate critical characteristics of 89 specimens of 15 minerals that are commonly found in sedimentary rocks. For kaolinites, Na+, Mg2+ and Ca2+ are exchangeable cations while other elements are essentially non-exchangeable. The compositional variability of most minerals is seen to be quite low (even for clay minerals) which bodes well for resolving the mineralogy of formations from down-hole elemental data. Nuclear parameters such as the photoelectric absorption cross section, natural gamma-ray activity, thermal neutron absorption cross section and neutron porosities calculated from chemical analyses of minerals often exceed values calculated using simple chemical formulae.
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页码:383 / 406
页数:24
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