铁白云石矿物学特征及原生次生成因机制

由雪莲; 贾文强; 徐帆; 刘仪

doi:10.3799/dqkx.2018.152

Volume 43 Issue 11

Nov. 2018

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Article Navigation > Earth Science > 2018 > 43(11): 4046-4055

You Xuelian, Jia Wenqiang, Xu Fan, Liu Yi, 2018. Mineralogical Characteristics of Ankerite and Mechanisms of Primary and Secondary Origins. Earth Science, 43(11): 4046-4055. doi: 10.3799/dqkx.2018.152

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You Xuelian, Jia Wenqiang, Xu Fan, Liu Yi, 2018. Mineralogical Characteristics of Ankerite and Mechanisms of Primary and Secondary Origins. Earth Science, 43(11): 4046-4055. doi: 10.3799/dqkx.2018.152

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Mineralogical Characteristics of Ankerite and Mechanisms of Primary and Secondary Origins

doi: 10.3799/dqkx.2018.152

1.
School of Ocean Sciences, China University of Geosciences, Beijing 100083, China
2.
School of Energy Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2018-04-10
Publish Date: 2018-11-15

Abstract

Abstract

The compositional break between ferroan dolomite and ankerite has not been well-defined for a long time. Ankerite has always been regarded as a secondary mineral generated at high temperatures. In this paper, progress in mineralogy and origins of ankerite and a link between microbial activity and ankerite are evaluated. Based on documented data:(1) The compositional break based on the "50% rule" principle from International Association of Mineralogy is applied for Ca-Mg-Fe carbonate. Any minerals with more than 50 mol% Fe in the Mg site would be called ankerite; (2) Progresses in mineralogical and lattice characteristics of ankerite are presented; (3) The origins of ankerite are primary and secondary. In the process of microbial mediated primary dolomite, microbe facilitates iron into the dolomite lattice and increases the iron content in the Mg site in its structure. Microbes could be added into the primary sedimentary experiments to promote mediation of the primary ankerite.
- ankerite,
- primary ankerite,
- microbial origin,
- mineralogy

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References(72)

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