Potential causes of depleted δ13Ccarb excursions in Ordovician marine carbonates, Ordos Basin, China
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DOI: 10.1016/j.marpetgeo.2021.105331
Abstract: Abstract Variations in the stable carbon isotope signature of marine carbonate rocks (δ13Ccarb) are utilized as an indicator for changes in depositional environment and tracers of diagenetic alteration. Various petrologic (textural changes) and geochemical indicators… read more here.
Keywords: ordos basin; marine carbonates; carbon; depleted 13ccarb ... See more keywords