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Published in 2018 at "Earth and Planetary Science Letters"
DOI: 10.1016/j.epsl.2018.04.004
Abstract: Abstract The last glaciation during the late Paleozoic ice age commenced at around the Guadalupian–Lopingian (G–L) boundary and is synchronous with the emplacement of the Emeishan large igneous province. Using CA-TIMS zircon U–Pb dating, we…
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Keywords:
age;
basaltic weathering;
early wuchiapingian;
wuchiapingian cooling ... See more keywords