THE COMPOSITION AND ORIGIN OF BRINES DURING THE MESSINIAN DESICCATION EVENT IN THE MEDITERRANEAN BASIN AS DEDUCED FROM CONCENTRATIONS OF IONS COPRECIPITATED WITH GYPSUM AND ANHYDRITE

被引：32

作者：

KUSHNIR, J ^{[1
]}

机构：

[1] WEIZMANN INST SCI,DEPT ISOTOPE,GEOSCI GRP,IL-76100 REHOVOT,ISRAEL

来源：

CHEMICAL GEOLOGY | 1982年 / 35卷 / 3-4期

关键词：

D O I：

10.1016/0009-2541(82)90010-9

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：

引用

页码：333 / 350

页数：18

共 26 条

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[8]

Garrison R., 1978, INITIAL REPORTS DEEP, P571, DOI DOI 10.2973/DSDP.PROC.42-1.123.1978

[9] ISOTOPE HYDROLOGY OF INLAND SABKHAS IN BARDAWIL AREA, SINAI [J].

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