Clumped isotope thermometry reveals diagenetic origin of the dolomite layer within late Ordovician black shale of the Guanyinqiao Bed (SW China)
Xiaolong Hu, Inigo A. Müller, Ankun Zhao, Martin Ziegler, Qing Chen, Lu Han, Zhiqiang Shi
Topics & Concepts
DolomiteGeologyOrdovicianGeochemistryIsotopes of oxygenPaleozoicDiagenesisCarbonateδ18OIsotopes of carbonStable isotope ratioPaleontologyMineralogyTotal organic carbonChemistryEnvironmental chemistryPhysicsQuantum mechanicsOrganic chemistryPaleontology and Stratigraphy of FossilsGeology and Paleoclimatology ResearchGeological and Geochemical Analysis