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