Interaction between the Central Asian Orogenic Belt (CAOB) and the Siberian craton as recorded by detrital zircon suites from Transbaikalia

Precambrian Research(2015)

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摘要
•1.7Ga craton-derived grains dominate the pre-Ediacaran part of the section.•Few grains of 1.7–1.4Ga are of unknown provenance.•Neoproterozoic CAOB-derived grains dominate post-610Ma strata.•Provenance shift marks the accretion of CAOB terranes to Siberian craton.
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关键词
Siberia,Neoproterozoic,Central Asian Orogenic Belt,Paleogeography,Baikal-Patom basin,Detrital zircons
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