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Volume 21 Issue S1
Nov 2021
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Article Contents
Yan Huang, Li Lin, Yongjun Yang, Liyan Ma, Deliang Li. Dominant Input of Marine Microbial Organics to Ni-Mo Polymetallic Sulfide Shale in Early Cambrian Niutitang Formation in Zhangjiajie, Hunan, South China. Journal of Earth Science, 2010, 21(S1): 33-35. doi: 10.1007/s12583-010-0163-4
Citation: Yan Huang, Li Lin, Yongjun Yang, Liyan Ma, Deliang Li. Dominant Input of Marine Microbial Organics to Ni-Mo Polymetallic Sulfide Shale in Early Cambrian Niutitang Formation in Zhangjiajie, Hunan, South China. Journal of Earth Science, 2010, 21(S1): 33-35. doi: 10.1007/s12583-010-0163-4

Dominant Input of Marine Microbial Organics to Ni-Mo Polymetallic Sulfide Shale in Early Cambrian Niutitang Formation in Zhangjiajie, Hunan, South China

doi: 10.1007/s12583-010-0163-4
Funds:

the National Natural Science Foundation of China 40743016

the Fund for the Doctoral Program of Higher Education of China 20070616014

the SINOPEC Project G0800-06-ZS-319

the Wengfu Phosphate Industry 

More Information
  • Corresponding author: Li Lin, linli@cdut.edu.cn
  • Received Date: 22 Dec 2009
  • Accepted Date: 10 Feb 2010
  • Publish Date: 01 Jun 2010
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    Feng, Z., Peng, Y., Jin, Z., et al., 2001. The Cambrian and Ordovician Lithofacies and Paleogeography in South China. Geological Publishing House, Beijing. 75–86 (in Chinese)
    Fu, J., Sheng, G., Xu, J., et al., 1990. Application of Biological Markers in the Assessment of Paleoenvironments of Chinese Nonmarine Sediments. Organic Geochemistry, 16(4–6): 769–799
    Kříbek, B., Sýkorová, I., Pašava, J., et al., 2007. Organic Geochemistry and Petrology of Barren and Mo-Ni-PGE Mineralized Marine Black Shales of the Lower Cambrian Niutitang Formation (South China). International Journal of Coal Geology, 72(3–4): 240–256
    Lehmann, B., Nagler, T., Holland, H., et al., 2007. Highly Metalliferous Carbonaceous Shale and Early Cambrian Seawater. Geology, 35(5): 403–406 doi: 10.1130/G23543A.1
    Orberger, B., Vymazalova, A., Wagner, C., et al., 2007. Biogenic Origin of Intergrown Mo-Sulphide- and Carbonaceous Matter Lower Cambrian Black Shales (Zunyi Formation, Southern China). Chemical Geology, 238(3–4): 213–231
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