SEA-WATER SULFATE REDUCTION AND SULFUR ISOTOPE FRACTIONATION IN BASALTIC SYSTEMS - INTERACTION OF SEA-WATER WITH FAYALITE AND MAGNETITE AT 200-350-DEGREES-C

被引：188

作者：

SHANKS, WC ^{[1
]}

BISCHOFF, JL ^{[1
]}

ROSENBAUER, RJ ^{[1
]}

机构：

[1] US GEOL SURVEY,MENLO PK,CA 94025

来源：

GEOCHIMICA ET COSMOCHIMICA ACTA | 1981年 / 45卷 / 11期

关键词：

D O I：

10.1016/0016-7037(81)90054-5

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：

引用

页码：1977 / 1995

页数：19

共 58 条

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[6] SEAWATER-BASALT INTERACTION AT 200 DEGREESC AND 500 BARS - IMPLICATIONS FOR ORIGIN OF SEA-FLOOR HEAVY-METAL DEPOSITS AND REGULATION OF SEAWATER CHEMISTRY
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[8] THE AGE CURVES OF SULFUR AND OXYGEN ISOTOPES IN MARINE SULFATE AND THEIR MUTUAL INTERPRETATION
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[9] OCEAN-FLOOR METAMORPHISM IN BETTS COVE OPHIOLITE, NEWFOUNDLAND
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[J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1977, 60 (03) : 255 - 270
[10] COLEMAN RG, 1977, ROCKS MINERALS, V12

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