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青海某地第三系红色碎屑岩层中金异常特征及成因探讨
引用本文:马生明,周国华,王俊祥,刘志勇.青海某地第三系红色碎屑岩层中金异常特征及成因探讨[J].物探与化探,1999,23(2):112-114.
作者姓名:马生明  周国华  王俊祥  刘志勇
作者单位:1. 国土资源部地球物理地球化学勘查研究所,廊坊,0650002
2. 青海省地球物理勘查院,西宁,810000
摘    要:对青海某地第三系红色碎屑岩层中的金异常特征进行了综述,指出金异常主要存在于第三系中段岩层中,异常在水系沉积物中强度最大,并认为金异常由次生富集作用形成。

关 键 词:青海  第三系碎屑岩  金异常  成因
收稿时间:1998-01-19

A PRELIMINARY DISCUSSION ON THE CHARACTERISTICS AND GENESIS OF GOLD ANOMALIES WITHIN THE TERTIARY RED CLASTIC BEDS IN A CERTAIN AREA OF QINGHAI PROVINCE
Ma Shengming,Zhou Guohua,Wang Junxiang,Liu Zhiyong.A PRELIMINARY DISCUSSION ON THE CHARACTERISTICS AND GENESIS OF GOLD ANOMALIES WITHIN THE TERTIARY RED CLASTIC BEDS IN A CERTAIN AREA OF QINGHAI PROVINCE[J].Geophysical and Geochemical Exploration,1999,23(2):112-114.
Authors:Ma Shengming  Zhou Guohua  Wang Junxiang  Liu Zhiyong
Institution:1. Institute of Geophysical and Geochemical Exploration, Langfang 065000;
2. Qinghai Institute of Geophysical Exploration, Xining 810000
Abstract:This paper sums up characteristics of Au anomalies within Tertiary red clastic beds in a certain area of Qinghai Province,and points out that Au anomalies mainly exist in the middle part of the Tertiary strata, that anomalies are most strong in stream sediments, and that Au anomalies result from secondary enrichment of Au.
Keywords:gold anomaly  genesis  Tertiary  clastic rock  Qinghai
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