H
Heng-Ci Tian
Researcher at Chinese Academy of Sciences
Publications - 33
Citations - 567
Heng-Ci Tian is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Geology & Basalt. The author has an hindex of 7, co-authored 14 publications receiving 274 citations. Previous affiliations of Heng-Ci Tian include University of Washington.
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Journal ArticleDOI
Deep carbon cycles constrained by a large-scale mantle Mg isotope anomaly in eastern China
Shuguang Li,Shuguang Li,Wei Yang,Shan Ke,Xunan Meng,Heng-Ci Tian,Lijuan Xu,Yongsheng He,Jian Huang,Xuan-Ce Wang,Qunke Xia,Weidong Sun,Xiaoyong Yang,Zhong-Yuan Ren,Haiquan Wei,Yongsheng Liu,Fancong Meng,Jun Yan +17 more
TL;DR: In this article, a large-scale mantle low δ26Mg anomaly in eastern China has been delineated, suggesting the contribution of sedimentary carbonates recycled into the upper mantle, but limited into the lower mantle.
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Non-KREEP origin for Chang'E-5 basalts in the Procellarum KREEP Terrane
Heng-Ci Tian,Hao Wang,Yi Chen,Wei Yang,Qin Zhou,Chi Zhang,Honglei Lin,Chao Huang,Shitou Wu,Li-Hui Jia,Lei Xu,Di Zhang,Xiaoguang Li,Rui Chang,Yue-Heng Yang,Lie-Wen Xie,Dan-Ping Zhang,Guang-liang Zhang,Sai-Hong Yang,Fu-Yuan Wu +19 more
TL;DR: A petrological and geochemical study of the basalt clasts from the Procellarum KREEP Terrane (PKT) returned by the Chang'e-5 mission is presented in this paper.
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Origin of low δ26Mg basalts with EM-I component: Evidence for interaction between enriched lithosphere and carbonated asthenosphere
TL;DR: This article presented stable Mg isotopic data for Cenozoic potassic basalts from Wudalianchi and Erkeshan in northeastern China to determine the interactions between upwelling carbonated asthenosphere and enriched lithospheric mantle.
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Low δ26Mg volcanic rocks of Tengchong in Southwestern China: A deep carbon cycle induced by supercritical liquids
TL;DR: In this paper, high-precision stable Mg isotopes of arc-like volcanic rocks from Tengchong, Southwestern China, have been investigated, revealing a new carbon cycle in which Mg-rich carbonate -dolomite -can be dissolved by supercritical liquids and subducted into a deep mantle wedge to depths of 120 to 300 km in the oceanic subduction zone.
Journal ArticleDOI
Iron, magnesium, and titanium isotopic fractionations between garnet, ilmenite, fayalite, biotite, and tourmaline: Results from NRIXS, ab initio, and study of mineral separates from the Moosilauke metapelite
N. X. Nie,N. X. Nie,Nicolas Dauphas,Esen E. Alp,Hao Zeng,Corliss Kin I Sio,J. Y. Hu,Xi Chen,S. M. Aarons,S. M. Aarons,Zhe Zhang,Heng-Ci Tian,Heng-Ci Tian,Da Wang,Kelsey B. Prissel,Kelsey B. Prissel,Jennika Greer,Jennika Greer,Wenli Bi,Michael Y. Hu,Jiyong Zhao,Anat Shahar,M. Roskosz,Fang-Zhen Teng,Michael J. Krawczynski,Philipp R. Heck,Philipp R. Heck,Frank S. Spear +27 more
TL;DR: In this article, the authors determine equilibrium Fe isotope fractionation factors between several common rock-forming minerals using a comparative approach involving three independent methods: (i) isotopic analyses of natural minerals from a metapelite from Mt. Moosilauke, New Hampshire, for which equilibration temperature and pressure are well constrained to be near the aluminosilicate triple point (T