CONCENTRATION CHANGES OF THORIUM, URANIUM AND OTHER METALS IN HYDROTHERMALLY ALTERED CONWAY GRANITE, NEW HAMPSHIRE

被引：16

作者：

BRIMHALL, WH

ADAMS, JAS

机构：

[1] Department of Geology, Rice University, Houston

来源：

GEOCHIMICA ET COSMOCHIMICA ACTA | 1969年 / 33卷 / 10期

关键词：

D O I：

10.1016/0016-7037(69)90050-7

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：

Concentrations of Th, U, K, Mg, Ca, Mn, Fe, Zn, Co and Cu are significantly different in two sections of a 1000 foot core sample of Conway granite. The differences, attributable to the action of weak hydrothermal fluids, indicate that the fluids, though weak, caused effective redistribution of these elements. © 1969.

引用

页码：1308 / &

共 10 条

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PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 1962, 48 (11) :1898-&

[2]

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[5]

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[10]

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