Ore-forming Geological Background of K-Mg Salt in Qarhan Salt Lake

WANG Chun-nan; GUO Xin-hua; MA Ming-zhu; LI Jun-de; LI Jian

Northwestern Geology > 2008 > 41(1): 97-106.

WANG Chun-nan, GUO Xin-hua, MA Ming-zhu, et al. Ore-forming Geological Background of K-Mg Salt in Qarhan Salt Lake[J]. Northwestern Geology, 2008, 41(1): 97-106.

Citation:

WANG Chun-nan, GUO Xin-hua, MA Ming-zhu, et al. Ore-forming Geological Background of K-Mg Salt in Qarhan Salt Lake[J]. Northwestern Geology, 2008, 41(1): 97-106.

Citation:

WANG Chun-nan, GUO Xin-hua, MA Ming-zhu, et al. Ore-forming Geological Background of K-Mg Salt in Qarhan Salt Lake[J]. Northwestern Geology, 2008, 41(1): 97-106.

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Ore-forming Geological Background of K-Mg Salt in Qarhan Salt Lake

Qinghai Geological Survey Institute, Xining 810012, China

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Received Date: August 22, 2007
Revised Date: August 23, 2007
Published Date: March 04, 2008

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Abstract

Abstract

Qarhan Salt Lake is the largest K-Mg salt deposit with proven reserves in China.The formation of K-Mg salt deposit is controlled by several factors: strata and magmatite material components of surrounding mountain area,the mountain-building and basin-formation movement caused by Qinghai-Tibet Plateau movement,paleoclimate and paleoenvironment,and other factors.Promising K-Mg salt deposit is mainly distributed in Quaternary stratum.
- matter source,
- neotectonic movement,
- paleoclimate

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Ore-forming Geological Background of K-Mg Salt in Qarhan Salt Lake

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