Petrogenesis of early Paleozoic I-type granitoids in the Longshoushan and implications for the tectonic affinity and evolution of the southwestern Alxa Block
Renyu Zeng,Hui Su,Mark B. Allen,Haiyan Shi,Houfa Du,Chenguang Zhang,and Jie Yan
School of Earth Sciences, East China University of Technology, Nanchang, 330013, China
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
Department of Earth Sciences, Durham University, Durham DH1 3LE, UK
Hui Su
School of Earth Sciences, East China University of Technology, Nanchang, 330013, China
Mark B. Allen
Department of Earth Sciences, Durham University, Durham DH1 3LE, UK
Haiyan Shi
Qinghai Geological Survey, Technology Innovation Center for Exploration and Exploitation of Strategic Mineral Resources in Plateau Desert Region, Ministry of Natural Resources, Xining 810000, China
Houfa Du
School of Earth Sciences, East China University of Technology, Nanchang, 330013, China
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
Chenguang Zhang
School of Geographic Sciences, Xinyang Normal University, Xinyang, 464000, China
Jie Yan
School of Earth Sciences, East China University of Technology, Nanchang, 330013, China
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
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Total article views: 1,382 (including HTML, PDF, and XML)
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Debate has long surrounded the tectonic affinity and evolution of Longshoushan during the Paleozoic. This study presents new zircon U–Pb ages, whole-rock major and trace element data, and Hf isotopic analyses for granitoids. (1) Longshoushan was influenced by the North Qilian Orogenic Belt in the early Paleozoic, (2) it transitioned from a post-collisional compressional to an extensional setting ~435 Ma, and (3) a three-stage early Paleozoic tectonic model is proposed.
Debate has long surrounded the tectonic affinity and evolution of Longshoushan during the...