New evidence for compaction-driven vertical fluid migration into the Upper Ordovician (Hirnantian) Guanyinqiao bed of south China
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DOI: 10.1016/j.palaeo.2020.109746
Abstract: Abstract The Late Ordovician was a time of major climatic and sea-level changes linked to the Hirnantian Glaciation, marked by large positive excursions of δ13Ccarb and δ13Corg globally known as the Hirnantian carbon isotopic excursion… read more here.
Keywords: south china; fluid migration; upper ordovician; guanyinqiao ... See more keywords