CARBON ISOTOPE COMPOSITION OF GRAPHITE AND CARBONATE MINERALS FROM 3.8-AE METAMORPHOSED SEDIMENTS, ISUKASIA, GREENLAND

被引：57

作者：

PERRY, EC ^{[1
]}

AHMAD, SN ^{[1
]}

机构：

[1] NO ILLINOIS UNIV,DEPT GEOL,DEKALB,IL 60115

来源：

EARTH AND PLANETARY SCIENCE LETTERS | 1977年 / 36卷 / 02期

关键词：

D O I：

10.1016/0012-821X(77)90210-2

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：280 / 284

页数：5

共 22 条

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[3] CALCULATED FRACTIONATION FACTORS FOR CARBON AND HYDROGEN ISOTOPE EXCHANGE IN SYSTEM CALCITE-CARBON DIOXIDE-GRAPHITE-METHANE-HYDROGEN-WATER VAPOR [J].

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CRAIG, H .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1957, 12 (1-2) :133-149

[7] ISOTOPIC FRACTIONATION BETWEEN COEXISTING ORGANIC CARBON-CARBONATE PAIRS IN PRECAMBRIAN SEDIMENTS [J].

EICHMANN, R ;

SCHIDLOWSKI, M .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1975, 39 (05) :585-595

[8] STABILITY RELATIONS OF SIDERITE (FECO3) IN SYSTEM FE-C-O [J].

FRENCH, BM .

AMERICAN JOURNAL OF SCIENCE, 1971, 271 (01) :37-&

[9] POSSIBLE BIOLOGICAL ORIGIN OF PRECAMBRIAN IRON-FORMATIONS [J].

LABERGE, GL .

ECONOMIC GEOLOGY, 1973, 68 (07) :1098-1109

[10]

MCGREGOR VR, 1977, COMMUNICATION

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