SOME CHEMICAL ALTERATIONS OF SUBSURFACE WATERS DURING DIAGENESIS

被引：7

作者：

CHILINGARIAN, GV

RIEKE, HH

机构：

[1] Petroleum Engineering Department, University of Southern California, Los Angeles, CA

来源：

CHEMICAL GEOLOGY | 1969年 / 4卷 / 1-2期

关键词：

D O I：

10.1016/0009-2541(69)90048-5

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：

A brief review of some of the processes which affect the chemical composition of interstitial waters is presented. The experimental results obtained by the writers indicate that the mineralization of squeezed-out solutions progressively decreases with increasing overburden pressure. Possibly, as the underground waters move through a thick shale sequence, the mineralization could increase to levels found in oil-field brines; the Ca/Cl and Ca/Na ratios could, but not necessarily, also increase. © 1969.

引用

页码：235 / +

页数：1

共 44 条

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[7] 2
[8] CHILINGAR GV, 1963, J SEDIMENT PETROL, V33, P801
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[J]. SEDIMENTOLOGY, 1964, 3 (03) : 199 - 225
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