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Clumped isotope thermometry reveals diagenetic origin of the dolomite layer within late Ordovician black shale of the Guanyinqiao Bed (SW China) 期刊论文
CHEMICAL GEOLOGY, 2022, 卷号: 588, 页码: 14
Authors:  Hu, Xiaolong;  Muller, Inigo A.;  Zhao, Ankun;  Ziegler, Martin;  Chen, Qing （陈清）;  Han, Lu;  Shi, Zhiqiang
Adobe PDF(4821Kb)  |  Favorite  |  View/Download：142/0  |  Submit date：2022/02/16
Late Ordovician  Guanyinqiao Bed  Organic-rich dolomite  Geochemistry  Clumped isotope thermometry