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

Title
Clumped isotope thermometry reveals diagenetic origin of the dolomite layer within late Ordovician black shale of the Guanyinqiao Bed (SW China)
Authors
Keywords
Late Ordovician, Guanyinqiao Bed, Organic-rich dolomite, Geochemistry, Clumped isotope thermometry
Journal
CHEMICAL GEOLOGY
Volume 588, Issue -, Pages 120641
Publisher
Elsevier BV
Online
2021-11-25
DOI
10.1016/j.chemgeo.2021.120641

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