Fangyang Hu
@igg.cas.cn
Key Laboratory of Mineral Resources
Insitute of Geology and Geophysics, CAS
RESEARCH, TEACHING, or OTHER INTERESTS
Geology, Geochemistry and Petrology, Earth and Planetary Sciences
Scopus Publications
Scholar Citations
Scholar h-index
Scholar i10-index
Scopus Publications
Feng Cong, Fu-Yuan Wu, Wen-Chang Li, Zai-Bo Sun, Xiao-Chi Liu, De-Feng He, Wei-Qiang Ji, Fang-Yang Hu, Shao-Hua Zhang, and Xiao-Ming Huang
Elsevier BV
Shao-Xiong He, Christopher J. Spencer, Xiao-Chi Liu, Fangyang Hu, Jia-Min Wang, Wei-Qiang Ji, and Fu-Yuan Wu
Elsevier BV
Lei Yang, Jia-Min Wang, Xiao-Chi Liu, Fang-Yang Hu, Kang-Shi Hou, Jian-Gang Fu, Guang-Ming Li, Yu-Lu Tian, and Fu-Yuan Wu
Elsevier BV
Wei Wang, Shuwen Liu, Peter A. Cawood, Jiachen Yao, Lei Gao, Rongrong Guo, Fangyang Hu, Denggang Lu, and Xin He
Elsevier BV
KangShi HOU, , JiaMin WANG, FangYang HU, Lei YANG, , , and
Chinese Society for Mineralogy, Petrology, and Geochemistry
FangYang HU, , HaoLan PU, Zhao GUO, TanJie LIU, XiaoChi LIU, ShaoXiong HE, FuYuan WU, , ,et al.
Chinese Society for Mineralogy, Petrology, and Geochemistry
XiaoChi LIU, , Lei YANG, ShaoXiong HE, FangYang HU, JiaMin WANG, , and
Chinese Society for Mineralogy, Petrology, and Geochemistry
Yang CHU, , YiLin GUO, TanJie LIU, XiaoChi LIU, FangYang HU, YiYang LEI, Wei LIN, , and
Chinese Society for Mineralogy, Petrology, and Geochemistry
Guohui Chen, Fangyang Hu, Alastair H.F. Robertson, Eduardo Garzanti, Shaohua Zhang, and Fu-Yuan Wu
Elsevier BV
Fangyang Hu, Xiaochi Liu, Shaoxiong He, Jiamin Wang, and Fuyuan Wu
Springer Science and Business Media LLC
Chao Huang, Hao Wang, Wenbei Shi, Jinfeng Sun, Fangyang Hu, Lei Xu, Yueheng Yang, Shitou Wu, Liewen Xie, and Jinhui Yang
Springer Science and Business Media LLC
Jia-Min Wang, Kang-Shi Hou, Lei Yang, Xiao-Chi Liu, Ru-Cheng Wang, Guang-Ming Li, Jian-Gang Fu, Fang-Yang Hu, Yu-Lu Tian, and Fu-Yuan Wu
Elsevier BV
Zi-Yi Ding, Shan-Ke Liu, Ben-Xun Su, Wen-Jun Li, Yang Bai, Qi-Qi Pan, Fang-Yang Hu, and Kwan-Nang Pang
Elsevier BV
FuYuan WU, , ChunLi GUO, FangYang HU, XiaoChi LIU, JunXing ZHAO, XiaoFeng LI, KeZhang QIN, , ,et al.
Chinese Society for Mineralogy, Petrology, and Geochemistry
Lei Gao, Shuwen Liu, Peter A. Cawood, Fangyang Hu, Jintuan Wang, Guozheng Sun, and Yalu Hu
Springer Science and Business Media LLC
AbstractThe redox evolution of Archean upper mantle impacted mantle melting and the nature of chemical equilibrium between mantle, ocean and atmosphere of the early Earth. Yet, the origin of these variations in redox remain controversial. Here we show that a global compilation of ∼3.8-2.5 Ga basalts can be subdivided into group B-1, showing modern mid-ocean ridge basalt-like features ((Nb/La)PM ≥ 0.75), and B-2, which are similar to contemporary island arc-related basalts ((Nb/La)PM < 0.75). Our V-Ti redox proxy indicates a more reducing upper mantle, and the results of both ambient and modified mantle obtained from B-1 and B-2 samples, respectively, exhibit a ∼1.0 log unit increase in their temporal evolution for most cratons. Increases in mantle oxygen fugacity are coincident with the changes in basalt Th/Nb ratios and Nd isotope ratios, indicating that crustal recycling played a crucial role, and this likely occurred either via plate subduction or lithospheric drips.
Yujian Wang, Dicheng Zhu, Chengfa Lin, Fangyang Hu, and Jingao Liu
Geological Society of America
Abstract Accretionary orogens function as major sites for the generation of continental crust, but the growth model of continental crust remains poorly constrained. The Central Asian Orogenic Belt, as one of the most important Phanerozoic accretionary orogens on Earth, has been the focus of debates regarding the proportion of juvenile crust present. Using published geochemical and zircon Hf-O isotopic data sets for three belts in the Eastern Tianshan terrane of the southern Central Asian Orogenic Belt, we first explore the variations in crustal thickness and isotopic composition in response to tectono-magmatic activity over time. Steady progression to radiogenic zircon Hf isotopic signatures associated with syn-collisional crustal thickening indicates enhanced input of mantle-derived material, which greatly contributes to the growth of the continental crust. Using the surface areas and relative increases in crustal thickness as the proxies for magma volumes, in conjunction with the calculated mantle fraction of the mixing flux, we then are able to determine that a volume of ~14–22% of juvenile crust formed in the southern Central Asian Orogenic Belt during the Phanerozoic. This study highlights the validity of using crustal thickness and zircon isotopic signatures of magmatic rocks to quantify the volume of juvenile crust in complex accretionary orogens. With reference to the crustal growth pattern in other accretionary orogens and the Nd-Hf isotopic record at the global scale, our work reconciles the rapid crustal growth in the accretionary orogens with its episodic generation pattern in the formation of global continental crust.
Fangyang Hu, Fu‐Yuan Wu, Mihai N. Ducea, James B. Chapman, and Lei Yang
American Geophysical Union (AGU)
AbstractThe mechanisms driving crustal deformation and uplift of orogenic plateaus are fundamental to continental tectonics. Large‐scale crustal flow has been hypothesized to occur in eastern Tibet, but it remains controversial due to a lack of geologic evidence. Geochemical and isotopic data from Cenozoic igneous rocks in the eastern Tibet‐Gongga‐Zheduo intrusive massif, provide a way to test this model. Modeling results suggest that Cenozoic magmas originated at depths of ∼30–40 km, the depth that crustal flow has been postulated to occur at. Detailed isotopic analyses indicate that the igneous rocks are derived from partial melting of the local Songpan‐Ganzi crust, arguing against a long‐distance crustal flow. Episodic magmatism during the Cenozoic showing a repeated shifting of magmatic sources can be correlated with crustal uplift. The continued indentation of the Indian Block and upwelling of the asthenosphere contribute to the crustal deformation, magmatism, and uplift.
Fangyang Hu, Fu-Yuan Wu, Jian-Gang Wang, Mihai N. Ducea, James B. Chapman, Khin Zaw, Wei Lin, Kyaing Sein, and Sebastien Meffre
Elsevier BV
HU FangYang, , WU FuYuan, CHEN GuoHui, YANG Lei, , , , and
Chinese Society for Mineralogy, Petrology, and Geochemistry
Guozheng Sun, Shuwen Liu, Peter A. Cawood, Ming Tang, Jeroen van Hunen, Lei Gao, Yalu Hu, and Fangyang Hu
Springer Science and Business Media LLC
AbstractConstraining thickness and geothermal gradient of Archean continental crust are crucial to understanding geodynamic regimes of the early Earth. Archean crust-sourced tonalitic–trondhjemitic–granodioritic gneisses are ideal lithologies for reconstructing the thermal state of early continental crust. Integrating experimental results with petrochemical data from the Eastern Block of the North China Craton allows us to establish temporal–spatial variations in thickness, geothermal gradient and basal heat flow across the block, which we relate to cooling mantle potential temperature and resultant changing geodynamic regimes from vertical tectonics in the late Mesoarchean (~2.9 Ga) to plate tectonics with hot subduction in the early to late Neoarchean (~2.7–2.5 Ga). Here, we show the transition to a plate tectonic regime plays an important role in the rapid cooling of the mantle, and thickening and strengthening of the lithosphere, which in turn prompted stabilization of the cratonic lithosphere at the end of the Archean.
Shao-Xiong He, Xiao-Chi Liu, Lei Yang, Jia-Min Wang, Fang-Yang Hu, and Fu-Yuan Wu
Elsevier BV
Feng Cong, Fu-Yuan Wu, Wen-Chang Li, Jian-Gang Wang, Fang-Yang Hu, De-Feng He, Wei-Qiang Ji, Wei Lin, and Kyaing Sein
Elsevier BV
LIU XiaoChi, , WU FuYuan, WANG RuCheng, LIU ZhiChao, WANG JiaMin, LIU Chen, HU FangYang, YANG Lei, HE ShaoXiong,et al.
Chinese Society for Mineralogy, Petrology, and Geochemistry
ZHAO JunXing, , HE ChangTong, QIN KeZhang, SHI RuiZhe, LIU XiaoChi, HU FangYang, YU KeLong, SUN ZhengHao, ,et al.
Chinese Society for Mineralogy, Petrology, and Geochemistry
LIU ShuWen, , BAO Han, GAO Lei, SUN GuoZheng, WANG Wei, GUO RongRong, GUO BoRan, FU JingHao, HU YaLu,et al.
Chinese Society for Mineralogy, Petrology, and Geochemistry