BEHAVIOR OF C-13 AND O-18 IN CARBONATES DURING CONTACT-METAMORPHISM AT MARYSVILLE, MONTANA - IMPLICATIONS FOR ISOTOPE SYSTEMATICS IN IMPURE DOLOMITIC LIMESTONES

被引：57

作者：

LATTANZI, P ^{[1
]}

RYE, DM ^{[1
]}

RICE, JM ^{[1
]}

机构：

[1] YALE UNIV,DEPT GEOL & GEOPHYS,NEW HAVEN,CT 06511

来源：

AMERICAN JOURNAL OF SCIENCE | 1980年 / 280卷 / 09期

关键词：

D O I：

10.2475/ajs.280.9.890

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

引用

页码：890 / 906

页数：17

共 31 条

[1]

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[5]

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[6] CHANGE IN CARBON AND OXYGEN ISOTOPIC COMPOSITION DURING CONTACT METAMORPHISM OF TRENTON LIMESTONE BY MOUNT ROYAL PLUTON [J].

DEINES, P ;

GOLD, DP .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1969, 33 (03) :421-&

[7]

Epstein S., 1964, ISOTOPIC COSMIC CHEM, P169

[8]

Faure G, 1977, PRINCIPLES ISOTOPE G

[9]

FRIEDMAN I, 1977, 440KK US GEOL SURV P

[10] OXYGEN ISOTOPE RATIOS IN COEXISTING MINERALS OF REGIONALLY METAMORPHOSED ROCKS [J].

GARLICK, GD ;

EPSTEIN, S .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1967, 31 (02) :181-&

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