Clumped isotope thermometry reveals diagenetic origin of the dolomite layer within late Ordovician black shale of the Guanyinqiao Bed (SW China)

标题
Clumped isotope thermometry reveals diagenetic origin of the dolomite layer within late Ordovician black shale of the Guanyinqiao Bed (SW China)
作者
关键词
Late Ordovician, Guanyinqiao Bed, Organic-rich dolomite, Geochemistry, Clumped isotope thermometry
出版物
CHEMICAL GEOLOGY
Volume 588, Issue -, Pages 120641
出版商
Elsevier BV
发表日期
2021-11-25
DOI
10.1016/j.chemgeo.2021.120641

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