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Zircon U-Pb ages in the Nuratau ophiolitic mélange in the southern Tianshan,Uzbekistan:Implication for the closure of Paleo-Asian Ocean
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作者 Kai Weng Ji-fei Cao +3 位作者 divayev-farid karibovich Jahongir-Jurabekovich Movlanov Bo Chen Zhong-ping Ma 《China Geology》 CAS CSCD 2024年第2期365-368,I0004-I0007,共8页
1.Objective The Central Asian Orogenic Belt(CAOB),which is located between the European craton,Siberian craton,and Tarim-North China craton(Fig.1a),is the largest phanerozoic accretionary orogen in the world.It result... 1.Objective The Central Asian Orogenic Belt(CAOB),which is located between the European craton,Siberian craton,and Tarim-North China craton(Fig.1a),is the largest phanerozoic accretionary orogen in the world.It resulted from the longterm subduction and accretion of the Paleo-Asian Ocean(PAO).The PAO has been in existence since at least the late Mesoproterozoic(about 1020 Ma).However,there has been debate about the closing time of the PAO. 展开更多
关键词 ASIAN Paleo TIANSHAN
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