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Reply to comment by L.Z. Shi et al. on “Birth and demise of the Bangong–Nujiang Tethyan Ocean: A review from the Gerze area of central Tibet”
Earth-Science Reviews ( IF 12.1 ) Pub Date : 2020-09-01 , DOI: 10.1016/j.earscirev.2020.103213 Shun Li , Changqing Yin , Carl Guilmette , Lin Ding
Earth-Science Reviews ( IF 12.1 ) Pub Date : 2020-09-01 , DOI: 10.1016/j.earscirev.2020.103213 Shun Li , Changqing Yin , Carl Guilmette , Lin Ding
Abstract Shi et al. (2020) commented on our recent work (Li et al. 2019), which reconstructed the Wilson cycle of the Bangong-Nujiang Tethyan Ocean. They questioned our preferred latest Jurassic-Early Cretaceous Lhasa-Qiangtang initial collision model, and argued that the Bangong-Nujiang Tethyan Ocean did not close until the Late Cretaceous, based on the existence of Mid-Cretaceous OIB-type mafic rocks, arc-type magmatism and marine sedimentation as well as paleomagnetic data. Here we respond to all these pieces of evidence separately and eventually conclude that the observations and data they provided are not proof supporting the persistence of the Bangong-Nujiang Tethyan Ocean into the Late Cretaceous. Our preferred latest Jurassic-Early Cretaceous Lhasa-Qiangtang initial collision model thereby still holds.
更新日期：2020-09-01
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