Mesozoic litho- and magneto-stratigraphic evidence from the central Tibetan Plateau for megamonsoon evolution and potential evaporites

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Mesozoic litho- and magneto-stratigraphic evidence from the central Tibetan Plateau for megamonsoon evolution and potential evaporites

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作者：Xiaomin Fang^a ; ^{fangxm@itpcas.ac.cn" class="auth_mail" title="E-mail the corresponding author} ; Chunhui Song^b ; Maodu Yan^a ; Jinbo Zan^a ; Chenglin Liu^c ; Jingeng Sha^d ; Weilin Zhang^a ; Yongyao Zeng^b ; Song Wu^b ; Dawen Zhang^a
关键词：Mesozoic magnetostratigraphy ; Central Tibetan Plateau ; Land&ndash ; sea interaction climate model ; Megamonsoon ; Evaporite mineral sources
刊名：Gondwana Research
出版年：2016
出版时间：September 2016
年：2016
卷：37
期：Complete
页码：110-129
全文大小：6207 K

文摘

•: Paleomagnetism and paleontology constrain well the Qiangtang Mesozoic stratigraphy.
•: Sequence lithology records a complete cycle of megamonsoon from birth to end in Asia.
•: Time-spatial evolution of the Mesozoic Qiangtang and Pangea climates.
•: Coupling of late Jurassic hot-dry climate and Mesotethys closure ensured a salt window.

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