Article ID Journal Published Year Pages File Type
4723475 Precambrian Research 2012 16 Pages PDF
Abstract
► The Fanchang volcanic rocks in the northeastern Yangtze Craton formed at 134-126 Ma. ► The deep crust of the northeastern Yangtze Craton probably contained unexposed Archean components. ► The northeastern Yangtze crust underwent complex accretion and reworking. ► The Precambrian crustal accretion and reworking of the Yangtze Craton are spatially and temporally heterogeneous.
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Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Complex Precambrian crustal evolution beneath the northeastern Yangtze Craton reflected by zircons from Mesozoic volcanic rocks of the Fanchang basin, Anhui Province
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