Search Results - "Qi, Ningyuan"

Magnesium Isotopes Archive the Initial Carbonate Abundances of Metasedimentary Rocks Prior to Thermal Decarbonation by Shi, Qingshang, He, Yongsheng, Zhao, Zhidan, Rolfo, Franco, Groppo, Chiara, Harris, Nigel, Wu, Hongjie, Qi, Ningyuan, Ke, Shan

“…Investigating the carbonate preservation efficiency (CPE) of continental crust is crucial to understand the global carbon cycle, which requires constraints on…”
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Miocene Alkaline Basaltic Magmatism in Northeastern Tibetan Plateau: Implications for Mantle Evolution and Plateau Outward Growth by Che, Yue, Liu, Dong, Zhao, Zhidan, Niu, Yaoling, Teng, Fang‐Zhen, DePaolo, Donald J., Yu, Xuehui, Zhu, Di‐Cheng, Qi, Ningyuan, Mo, Xuanxue

“…The widespread Cenozoic alkaline magmatism within and around the Tibetan Plateau offers a prime opportunity to probe the nature of the mantle at the depths…”
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Middle-Late Jurassic magmatism in the west central Lhasa subterrane, Tibet: Petrology, zircon chronology, elemental and Sr-Nd-Pb-Hf-Mg isotopic geochemistry by Tong, Xin, Yan, Jingjing, Zhao, Zhidan, Niu, Yaoling, Qi, Ningyuan, Shi, Qingshang, Liu, Dong, Wang, Qing, Zhang, Liang-Liang, Dong, Guochen, Zhu, Di-Cheng

“…Mesozoic magmatic rocks are widespread in the Lhasa terrane, but most of them are of cretaceous age. Because Jurassic rocks are relatively rare and our…”
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Early Paleocene diorite and bimodal dykes from the Dagze region, southern Lhasa Terrane: Tectonic implications for the late-stage of Neo-Tethyan subduction by Tang, Yan, Zhao, Zhidan, Li, Xiaowei, Wang, Zhenzhen, Qi, Ningyuan, Liu, Dong, Wang, Qing, Mo, Xuanxue

“…The tectonic transition from oceanic subduction to continental collision is a fundamental process during orogenesis. Yet, the nature of this transition and its…”
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Late Cretaceous adakitic and A-type granitoids in Chanang, southern Tibet: Implications for Neo-Tethyan slab rollback by Wang, Zhenzhen, Zhao, Zhidan, Li, Xuping, Asimow, Paul D., Liu, Dong, Mo, Xuanxue, Qi, Ningyuan, Tang, Yan, Wang, Qing, Zhu, Di-Cheng, Zhang, Liangliang, Sheikh, Lawangin

“…[Display omitted] •Adakitic signature originated from residual or fractionated amphibole.•Coeval A-type quartz syenites were produced from fractional…”
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