Using detrital zircons from late Permian to Triassic sedimentary rocks in the south-eastern Central Asian Orogenic Belt (NE China) to constrain the timing of the final closure of the Paleo-Asian Ocean

Volume: 144, Pages: 82 - 109
Published: Aug 1, 2017
Abstract
We present new detrital zircon U–Pb–Hf isotope data for seven samples from late Permian to Triassic sedimentary units in Jilin Province, Northeast (NE) China, and use these data to constrain the timing of final closure of the Paleo-Asian Ocean and the late Permian to Triassic tectonic evolution of the Changchun–Yanji suture belt. The late Permian to Early Triassic sedimentary rocks contain material derived from both the northern margin of the...
Paper Details
Title
Using detrital zircons from late Permian to Triassic sedimentary rocks in the south-eastern Central Asian Orogenic Belt (NE China) to constrain the timing of the final closure of the Paleo-Asian Ocean
Published Date
Aug 1, 2017
Volume
144
Pages
82 - 109
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