遵义下寒武统富硒黑色岩系地球化学: 成因和硒富集机理

冯彩霞; 刘燊; 胡瑞忠; 刘家军; 罗泰义; 池国祥; 齐有强

doi:10.3799/dqkx.2010.109

Volume 35 Issue 6

Jun. 2010

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Article Navigation > Earth Science > 2010 > 35(6): 947-958

FENG Cai-xia, LIU Shen, HU Rui-zhong, LIU Jia-jun, LUO Tai-yi, CHI Guo-xiang, QI You-qiang, 2010. Geochemistry of Lower Cambrian Se-Rich Black Rock Series in Zunyi, Guizhou Province, Southwest China: The Petrogenesis and Enrichment Mechanism of Selenium. Earth Science, 35(6): 947-958. doi: 10.3799/dqkx.2010.109

Citation:

FENG Cai-xia, LIU Shen, HU Rui-zhong, LIU Jia-jun, LUO Tai-yi, CHI Guo-xiang, QI You-qiang, 2010. Geochemistry of Lower Cambrian Se-Rich Black Rock Series in Zunyi, Guizhou Province, Southwest China: The Petrogenesis and Enrichment Mechanism of Selenium. Earth Science, 35(6): 947-958. doi: 10.3799/dqkx.2010.109

Citation:

FENG Cai-xia, LIU Shen, HU Rui-zhong, LIU Jia-jun, LUO Tai-yi, CHI Guo-xiang, QI You-qiang, 2010. Geochemistry of Lower Cambrian Se-Rich Black Rock Series in Zunyi, Guizhou Province, Southwest China: The Petrogenesis and Enrichment Mechanism of Selenium. Earth Science, 35(6): 947-958. doi: 10.3799/dqkx.2010.109

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Geochemistry of Lower Cambrian Se-Rich Black Rock Series in Zunyi, Guizhou Province, Southwest China: The Petrogenesis and Enrichment Mechanism of Selenium

doi: 10.3799/dqkx.2010.109

1.
State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
2.
State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences, Beijing100083, China
3.
Department of Geology, University of Regina, Saskatchewan S4S0A2, Canada

Received Date: 2009-12-22
Publish Date: 2010-11-01

Abstract

Abstract

Herein, XRF, ICP-MS and hydride generation atomic fluorescence spectrometry (HGAFS) techniques were used to analyze the major, trace elements and Se contents of the Se-rich black rock series in Zunyi, Guizhou Province, respectively. Based on the elemental geochemistry, we suggest that the Se-rich black rock series, including K-bentonite, phosphrite, black shales, cherts and Ni-Mo ore samples, mainly formed by hydrothermal deposition. Meanwhile, the petrogenesis of the black rock series was related with volcanism. Furthermore, K-bentonite, phosphrite, black shales, chert and Ni-Mo ore samples are characterized by high Se contents, and high enrichment coefficients correspond to those of the crust (801, 531.2, 449, 123 and 11 133). Combining with previous studies, we propose that the enrichment of Se in study area is related to many factors, such as existence of abundant sulfide, hydrothermal deposition and volcanism.
- geochemistry,
- black rock series,
- Lower Cambrian,
- Zunyi

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References(97)

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