Fangyang Hu

Scopus Publications

Rapid and concentrated magmatism and mineralization of rare-metal granites: Evidence from the Limu deposit, South China
Shao-Hua Zhang, Hehe Jiang, Wei-Qiang Ji, Fangyang Hu, Yue-Heng Yang, Zuohai Feng, Fu-Yuan Wu
Ore Geology Reviews, 2026
Rare metals, including W, Sn, Nb, Ta, and Li, are strategic resources essential for advanced manufacturing, clean energy, and defense technologies. In-situ isotopic dating of ore minerals directly constrains rare-metal mineralization timing, which could provide essential information for ore-forming process. The Limu rare-metal granite is a representative granite-type Nb–Ta deposit in South China and occurs as several small stocks (∼1 km 2 ), including muscovite granite, Li–phengite granite, and zinnwaldite/lepidolite–albite granite. Previous studies proposed a prolonged magmatic evolution from ∼ 240 to ∼ 200 Ma, longer than that of most batholiths, with controversial ages derived from different methods, leaving its precise chronological framework unresolved. Here we conducted in situ U–Pb/U–Th–Pb dating on zircon, monazite, cassiterite, columbite-group minerals (CGM), and wolframite from 19 granite samples collected from seven localities in the Limu ore field: Paoshuiling, Jinzhuyuan, Xiangtanling, Niulanling, Daqiling, Laohutou, and Shuiximiao. The results constrain the formation of the Limu rare-metal granite to 212.6 ± 4.4 Ma–207.8 ± 2.3 Ma, with a peak at approximately 210 Ma. Integration of new whole–rock geochemical data (n = 17), previously published datasets (n = 51), and zircon trace element analyses shows that granites from Jinzhuyuan, Laohutou, and Shuiximiao are the most evolved, whereas those from Daqiling and Niulanling represent more primitive end-members. These results define a precise temporal framework, indicating that the separate stocks formed within a short interval (∼5 Myr) through fractional crystallization and prompting a reevaluation of the magmatic and metallogenic evolution of the Limu rare-metal granite, with broader implications for dating comparable highly fractionated granites and granite-type rare-metal deposits worldwide.
Experimental and geochemical evidence for magmatic origin of Li-Rb-Cs in geothermal waters of the Yangbajing-Gulu Rift, Tibet
Wenjie Sun, Jiabin Duan, Mingliang Liu, Fangyang Hu, Xiaodong Jiang, Yanlong Kong
Geothermics, 2026
Geothermal waters in certain regions of Tibet, particularly those characterized by intense tectonic activity, are exceptionally enriched in lithium (Li), rubidium (Rb), and cesium (Cs). However, the primary sources of these elements within Tibetan geothermal systems remain debated. Clarifying whether these elements are derived predominantly from water-rock interaction or magmatic fluid input is essential for a comprehensive understanding of the region’s geothermal systems. Previous studies lacked quantitative analysis methods using water-rock interaction simulation experiments. To address this gap, we conducted laboratory simulations using 10-million-years-old biotite granite from the Yangbajing area, performing high-temperature and high-pressure experiments at 200 °C and 20 MPa over 62 days. The results yield a Li:Rb:Cs ratio of approximately 48:64:1, which starkly contrast with the ratio observed in natural geothermal waters (around 5.7:1:2.1). This significant discrepancy suggests that there must be an additional geochemical process that strongly modifies the Li, Rb, and Cs ratios in natural geothermal waters. Moreover, in the Yangbajing-Gulu rift, the concentrations of Li, Rb, and Cs show a strong correlation with Cl, a tracer indicative of magmatic fluid input, while the correlations between δ¹⁸O and the concentrations of Li, Rb, and Cs are weaker. The geothermal waters exhibit a Cs > Rb pattern, similar to other geothermal systems with magmatic fluid input. Combined with geophysical evidence of shallow melt bodies beneath the rift, these findings indicate that magmatic fluid input is a key factor controlling the enrichment of Li, Rb, and Cs in the geothermal waters of the Yangbajing-Gulu rift. This study highlights the magmatic source mechanism for rare metal supply in Tibetan geothermal waters and provides critical insights into the metallogenic models of Tibetan geothermal systems.
Discovery of a Late Eocene–Early Oligocene ultra-high temperature (UHT) migmatite in the Gangdese batholith at Nyingchi, southern Tibet and its tectonic implications
Hehe Jiang, Xu Chu, Jia-Min Wang, Wei-Qiang Ji, Wenrong Cao, Fangyang Hu, Xiao-Chi Liu, Fu-Yuan Wu
Lithos, 2026
Early Precambrian rare-metal mineralization in the North China Craton
FuYuan WU, , JiaHui XU, MenPin ZHANG, YueHeng YANG, FangYang HU, Hao YANG, Peng PENG, , and
Acta Petrologica Sinica, 2026
世界上主要克拉通大多都曾发育早前寒武纪伟晶岩型稀有金属成矿作用,但我国华北克拉通似乎是个例外。到目前为止,还没有在该区发现具有可观工业价值的早前寒武纪稀有金属伟晶岩。总结华北地区目前已有的研究线索发现,早前寒武纪稀有金属伟晶岩在华北克拉通普遍发育,并可划分为两个阶段。其一是太古宙晚期25亿年的伟晶岩,它主要分布在辽北-冀东-鲁西一带的太古宙地体上,与25亿年左右的早期克拉通化关系密切。此阶段伟晶岩赋存在太古宙绿岩地体的基性-超基性变火山岩中,其成矿类型以锂和钽为主,分别以山东新泰石棚锂辉石伟晶岩和辽宁新宾李家堡子铌钽矿伟晶岩为代表,代表了一种Li-Cs-Ta型伟晶岩的稀有金属成矿作用。其二是古元古代18亿年左右的伟晶岩,它遍布整个华北地区,但主要分布在古元古宙的辽吉活动带、内蒙古孔兹岩带和华北中部碰撞带等,与华北克拉通内部块体拼贴、碰撞及后期广泛的克拉通化有关。该期伟晶岩主要赋存在变质的表壳岩系之中,其成矿类型以铍、铌、钽、铀和稀土为主,以辽宁海城含铌铀伟晶岩和内蒙古乌拉山含铍伟晶岩为典型代表。目前在区内还没发现此期伟晶岩存在锂矿化的痕迹,反映了Nb-Y-F型为主的稀有金属成矿作用。通过与世界上典型克拉通(如澳大利亚、非洲、波罗的、北美等克拉通)稀有金属伟晶岩的对比发现,华北克拉通具有与它们基本一致的稀有金属成矿特征。华北克拉通早前寒武纪稀有金属伟晶岩型矿床稀少的原因,一方面与它较高的变质程度(或较强的剥蚀程度)有关,但研究和勘查程度不高可能也是不可忽视的重要因素。未来,在加强与世界典型克拉通对比研究的同时,应着重研究华北克拉通内部不同时代岩浆作用的背景、源区和演化特征,以期理解太古宙LCT型和古元古宙NYF型伟晶岩差异形成的原因,为华北早前寒武纪伟晶岩型稀有金属资源的突破提供理论依据。
The indicative significance of apatite in the Ganfang region for lithium mineralization
Ke Huang, Miao Yu, Chunli Guo, Xinghua Ma, JianZhong Niu, Junxing Zhao, Fangyang Hu, Xiaochi Liu
Ore Geology Reviews, 2026
• Apatite U–Pb dating from stockscheider and pegmatite veins constrains the formation age of the Ganfang Li deposit. • Trace-element compositions of apatite reveal the relationship between hydrothermal alteration and Li mineralization. • A genetic model for Li mineralization in the Ganfang area is proposed based on apatite trace-element signatures. Granite-related Li-Nb-Ta deposits, characterized by extensive albitization within plutons, represent a novel lithium resource. The Ganfang area, one of the important granite-type lithium deposits in South China, features a vertical lithological sequence from top to bottom of stockscheider, albitized granite, and K-feldspar granite. The ore-bearing stratum is dominated by albitized granite. Our study focuses on elucidating the connection between magmatic differentiation, hydrothermal alteration, and lithium mineralization in albitized granites. By analyzing geochemical trends in apatite from stockscheiders, pegmatite veins, and altered granites, we aim to unravel the petrogenetic and metallogenic mechanisms of rare metal lithium. Apatite serves as a geochemical tracer, recording the intensity of fluid alteration processes and their impact on lithium enrichment. The U-Pb dating results (142.2–143.2 Ma and 128.8 Ma) of apatite from the stockscheiders and pegmatite vein show that mineralization in the Ganfang area occurred during the Late Yanshanian period and associated with the melting of the lower crust. Strontium (Sr), (La/Yb) N, and (La/Sm) N can indicate that mineralization in this area is closely associated with fluid activity. Our findings highlight distinct differences in trace element contents of apatite between upper ore-bearing albitized granite and lower barren K-feldspar granite, with specific trace element ratios (e.g., Ge-Ga, Ce/Pb-Th/U, ΣREE + Y-Mn/Fe, and Sr/Y-ΣLREE) serving as indicators of metallogenic potential. The ore-bearing albitized granite exhibits high concentrations of Ga and Ge, with a strong positive correlation between the two elements, this phenomenon may be related to the hydrothermal metasomatism of topaz. In addition, the ore-bearing granite exhibits relatively high Ce/Pb, light rare earth element (LREE), and total rare earth elements plus yttrium (ΣREE + Y) contents. This study indicates that lithium mineralization in the Ganfang area is closely linked to multistage fluid activity in a sealed-system, with a formation process involving the upward dissolution of Na and Li-rich fluids to form stockscheider, and followed by downward migration to replace fresh monzonite granites, forming ore-bearing albitized granite and barren K-feldspar granite.
Evolution of Cretaceous Sediment Provenance in the Danxia Basin, Southeast China: Implications for Tectonic and Landscape Reorganization in Cathaysia
Guohui Chen, Kaijie Zha, Hongwei Li, Liangkai Cheng, Yifan Jia, Rongli Huang, Carlos Zavala, Yecai Xie, Fangyang Hu
Tectonics, 2026
Understanding how tectonic uplift and drainage reorganization controlled sediment dispersal during the Cretaceous is critical for reconstructing the topographic evolution of southeast China. This study examines how sediment sources and routing systems evolved during the Cretaceous, using the Danxia Basin as a key archive and adjacent basins for regional comparison. We integrate sedimentological observations, detrital zircon U‐Pb‐Hf isotopic data, whole‐rock Pb isotope geochemistry and source unmixing results from the Danxia Basin deposits, together with published Jurassic to Paleogene zircon age data sets from nine adjacent basins. The results reveal a regional provenance shift from dominant northern cratonic sources (North China and Yangtze blocks) during the Jurassic to increasing Cathaysian sources during the Cretaceous, including the Wuyishan and Yunkai terranes and the Nanling Tectonic Belt. Within the Danxia Basin, Cretaceous lithologies record a two‐stage provenance evolution: Early Cretaceous sediments mainly derived from the Wuyishan Terrane, whereas Late Cretaceous deposits show mixed input from the Yunkai Terrane, Nanling Tectonic Belt and Wuyishan Terrane, reflecting drainage expansion and/or sediment‐routing reorganization. Published thermochronological data indicate enhanced uplift and exhumation in the Yunkai Terrane and Nanling regions during the Late Cretaceous, driving increased sediment flux to both inland and coastal basins. During the Paleocene‐Eocene, sediment supply became increasingly dominated by the Nanling region as exhumation in Yunkai region waned. These observations support a dynamic “seesaw” topographic model, in which alternating uplift of northern cratonic and eastern Cathaysian source regions governed sediment dispersal, basin architecture and paleoenvironmental evolution across southeast China.
High geothermal gradients facilitating lithium mineralization: Insights from the Ke’eryin–Taiyanghe plutons, central China
Fangyang Hu, Mihai N. Ducea, James B. Chapman, Lei Yang, Guohui Chen, Chunli Guo, Fu-Yuan Wu
Earth and Planetary Science Letters, 2025
Highly fractionated granite and high-purity quartz
FuYuan WU, , XiaoChi LIU, JiaMin WANG, HouBin CHEN, FangYang HU, ZhiChao LIU, , and
Acta Petrologica Sinica, 2025
高纯石英(High-purity quartz, HPQ)是一种由高纯石英矿提纯而至的关键基础材料。作为我国刚刚被定义的新矿种，高纯石英矿是指在当前技术经济条件下，经选矿、提纯可获得二氧化硅(SiO2)纯度不低于99.995%(4N5)，杂质元素含量及配型、包裹体含量以及粒度满足半导体、光伏、光学等高新领域应用要求的岩石。根据这一新的定义，结合产业需求，本文将石英分为低纯石英(99.9%-3N)、中纯石英(99.99%-4N)、高纯石英(99.995%-4N5)和超高纯石英(99.998%-4N8)四类。尽管大部分杂质矿物包裹体和气液包裹体可在后期破碎和焙烧等纯化过程中得以剔除，但晶格杂质元素很难有效排除，其含量多少决定了石英纯度的高低和最终品质。石英中杂质元素的含量与其结晶时的温度、压力、介质成分等因素相关，即石英原料矿的性质决定了高纯石英的产出情况。国内外情况的汇总发现，目前高纯石英原料矿主要为水晶、脉石英、石英岩、伟晶岩和花岗岩五大类。水晶和脉石英一般规模较小，很难形成规模应用；石英岩成因复杂，石英内部杂质元素含量稳定性稍差；而半导体和光伏行业中最重要的4N8以上的超高纯石英砂主要来自花岗伟晶岩和花岗岩。大多数花岗伟晶岩具有明显的岩相分带，其石英杂质元素组成呈现很大的空间变化，给工业应用带来困难。然而，暗色矿物含量低的白岗岩不仅杂质元素含量低，且含量较为稳定，是4N8型超高纯石英的主要原料。对美国Spruce Pine白岗岩-伟晶岩和我国河南东秦岭漂池白岗岩-伟晶岩的研究发现，该类石英原料矿实际上是一种经历适度结晶分异作用的花岗岩，它表现为下部为黑云母花岗岩、二云母花岗岩，上部为白云母花岗岩和伟晶岩的垂向岩性分布格局，具有侵位深度大、钛含量低的特点，并经历过后期变质变形的改造。未来我国超高纯石英矿的寻找，应围绕经历过一定程度结晶分异作用的未分带伟晶岩和白岗岩进行，过低或过高分异的花岗岩-伟晶岩均不是超高纯石英矿的潜在对象。晚期韧性变形可一定程度上改变石英中气液包裹体的分布样式，但对杂质元素的影响方式，未来仍需深入研究。
Trace element compositions of quartz in granites and pegmatites from the Sanmudaimiao region, northern margin of the North China Craton and their implications for the formation of high-purity quartz
XiaoYa DUAN, , FangYang HU, ShaoHua ZHANG, ZhanJiang FENG, Yong LIANG, YanHu LIU, ZhiQiang WANG, HaiBao LI, YiNan YAN, , , , and
Acta Petrologica Sinica, 2025
高纯石英是我国最新公布确认的矿种, 理解其形成机制和主控因素对于未来寻找相关资源至关重要。然而, 目前关于其成因机制的研究仍较为匮乏, 对于何种地质条件有利于高纯石英的形成尚存争议。本文以华北克拉通北缘三木代庙地区花岗岩和伟晶岩中的石英作为研究对象, 探讨花岗岩-伟晶岩演化过程和变形作用对石英中微量元素含量的影响, 并对该地区的高纯石英成矿潜力进行初步厘定。本研究的主要研究对象包括未变形二云母花岗岩、变形二云母花岗岩、未成矿伟晶岩及锂辉石-锂云母成矿伟晶岩中的石英。分析结果显示, 不同类型岩石的石英微量元素组成差异显著, 主要受控于岩浆性质、分异程度及结晶物理条件。二云母花岗岩石英整体Ti和Al含量较高, 超出高纯石英相关标准(Al < 30×10-6, Ti < 10×10-6), 而Li含量则基本达到高纯石英的标准(Li < 5×10-6), 这与岩浆相对较高的温度和较低的演化程度有关, 而Al的富集则可能与围岩混染关系密切。相比于未变形二云母花岗岩, 变形二云母花岗岩的石英Li含量显著偏低, 但Al和Ti含量则变化有限, 表明变形作用对该地区石英的纯化有一定促进作用。由于伟晶岩的岩浆演化程度高并伴随流体活动, 导致其中石英的Li、Al和Ge含量普遍较高, 远超高纯石英标准。相比于锂成矿伟晶岩, 未成矿伟晶岩的杂质含量整体低于成矿伟晶岩, 而成矿伟晶岩的边部带(块体长石带和层状细晶岩带)杂质相对核部偏低。由此, 对于伟晶岩而言, 低演化的伟晶岩边部可能为形成高纯石英的有利部位, 而核部因高岩浆演化程度和强流体活动导致其杂质元素含量偏高。综上, 低温、低演化、低混染并伴随后期变形作用是形成高纯石英的有利条件。三木代庙地区目前花岗岩-伟晶岩的石英整体不满足高纯石英要求, 但考虑到该地区与东秦岭、阿勒泰等已知存在高纯石英的地区地质条件具有一定相似性, 该地区局部可能具有高纯石英的找矿潜力, 其成矿条件有待进一步系统分析。
Lithium Isotope Fractionation during Granitic Magma Differentiation: Insights from Whole Rock and Mineral Analyses
Zi-Yi Ding, Shan-Ke Liu, Ben-Xun Su, Wen-Jun Li, Fang-Yang Hu, Patrick Asamoah Sakyi
Journal of Petrology, 2025
Despite extensive studies on whole-rock lithium (Li) isotope geochemistry, the fractionation of Li isotopes among minerals in granitic magmatic systems is still poorly understood. To investigate the magnitude and mechanism of inter-mineral and inter-sample Li isotope fractionation during granitic magma differentiation, we present high-precision Li isotope data from a suite of well-characterized granitoids (quartz diorite, granodiorite, and monzogranite) and their minerals from the Tagong pluton in NE Tibetan Plateau. The whole rocks exhibit δ7Li variation from −1.73 ± 0.15 to 1.30 ± 0.08‰, indicating insignificant Li isotope fractionation at the whole-rock scale. The constituent mafic minerals show δ7Li values varying from −1.68 ± 0.05 to 1.76 ± 0.15‰ in biotite, −2.08 ± 0.15 to 2.53 ± 0.13‰ in amphibole, and −1.72 ± 0.21 to 0.74 ± 0.08‰ in clinopyroxene, demonstrating equilibrium isotope fractionation between these coexisting phases during magma differentiation. The comparable δ7Li values between whole rocks and biotite suggest that crystallization of the Li-richest phase (biotite Li = 139–361 μg/g) is the key factor controlling whole-rock Li isotope compositions. In contrast, quartz, K-feldspar, and plagioclase display significant inter-mineral and inter-sample Li isotope variations with δ7Li ranges of 15.09 ± 0.14 to 26.00 ± 0.33‰, 1.69 ± 0.10 to 8.53 ± 0.01‰, and −2.23 ± 0.08 to 6.50 ± 0.19‰, respectively. Rayleigh fractionation alone cannot fully account for the Li isotope variations in these felsic minerals. Plagioclase in the K-feldspar-rich granodiorites and monzogranites is isotopically lighter and more variable than in the K-feldspar-free quartz diorites, indicating competition for Li isotopes between K-feldspar and plagioclase during simultaneous crystallization. The Li isotope variation in quartz that has low Li content (0.67 to 2.82 μg/g) may be related to the diffusion process. Furthermore, mafic microgranular enclaves, typically observed in granitoid rocks, show whole-rock and mineral Li isotope compositions similar to the counterparts of their host rocks, suggesting that they are of schlieren origin. This provides further evidence for minimal Li isotope fractionation at the whole-rock level. In comparison to the low-silica (SiO2 &lt; 65 wt %) and uniform whole-rock Li isotope characteristics of the granitoid samples studied here, global high-silica (SiO2 &gt; 65 wt %) granitic rocks exhibit highly variable δ7Li values from −3.0 to 8.0‰. This variability can be attributed to the fractional crystallization of felsic minerals, which are more abundant in the high-silica rocks.
Neoarchean orogenic belt evolution in the northeast North China Craton: Implications for the reconstruction of early Earth's microplates
Guozheng Sun, Shuwen Liu, Sanzhong Li, Timothy M. Kusky, Fangyang Hu, Han Bao, Lei Gao, Yalu Hu, Shengyao Yu, Liming Dai, Lintao Wang, Xi Wang
Precambrian Research, 2025
Miocene magmatic evolution and rare-metal mineralization in the Lhasa terrane, Tibetan Plateau
LI JiaLiang, , JI WeiQiang, HU FangYang, XU Qiang
Yanshi Xuebao Acta Petrologica Sinica, 2025
Discovery of the Mustang spodumene-bearing pegmatites in the Himalaya orogenic belt and its geological significance
LI XueZhen, , LIU XiaoChi, XING LuYao, ZHAO XiangYing, PU HaoLan, HU FangYang, WU FuYuan, and
Yanshi Xuebao Acta Petrologica Sinica, 2025
Discovery of spodumene pegmatites in the Kangmar, Xizang and the lithium resource prospects in the Tethyan Himalaya
DunZhu CIREN, , XiaoChi LIU, GuoZheng MAO, ChengLin LIU, Wei WU, XiangYing ZHAO, LuYao XING, FangYang HU, JunXing ZHAO, JunYu LI, Ji DOR, FuYuan WU, , , and
Yanshi Xuebao Acta Petrologica Sinica, 2025
Himalayan Leucogranites: Rare-metal Resources
Fu-Yuan Wu, Xiao-Chi Liu, Fang-Yang Hu, Lei Xie, Ru-Cheng Wang
Elements, 2024
Latitude-dependent oxygen fugacity in arc magmas
Fangyang Hu, Hehe Jiang, Bo Wan, Mihai N. Ducea, Lei Gao, Fu-Yuan Wu
Nature Communications, 2024
Tracking the magmatic-hydrothermal evolution during lithium mineralization with zircon trace elements
Dizhi Xuebao Acta Geologica Sinica, 2024
Crystal mush rejuvenation in the formation of Triassic dacites in Mengku, SE Tibetan Plateau
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, Xiao-Ming Huang
Journal of Asian Earth Sciences, 2024
Identification of Indian crustal melting beneath Gangdese arc during India-Asia collision
Shao-Xiong He, Christopher J. Spencer, Xiao-Chi Liu, Fangyang Hu, Jia-Min Wang, Wei-Qiang Ji, Fu-Yuan Wu
Lithos, 2024
Petrogenetic link between leucogranite and spodumene pegmatite in Lhozhag, eastern Himalaya: Constraints from U–(Th)–Pb geochronology and Li–Nd–Hf isotopes
Lei Yang, Jia-Min Wang, Xiao-Chi Liu, Fang-Yang Hu, Kang-Shi Hou, Jian-Gang Fu, Guang-Ming Li, Yu-Lu Tian, Fu-Yuan Wu
Lithos, 2024
Early Neoarchean alternation of plate subduction and deep mantle upwelling
Wei Wang, Shuwen Liu, Peter A. Cawood, Jiachen Yao, Lei Gao, Rongrong Guo, Fangyang Hu, Denggang Lu, Xin He
Precambrian Research, 2024
Skarn-type rare metal mineralization in the Mount Shisha Pangma region: Petrological characteristics,mineralization age and its geological significance
KangShi HOU, , JiaMin WANG, FangYang HU, Lei YANG, , , and
Yanshi Xuebao Acta Petrologica Sinica, 2024
A preliminary study on petrogenesis of the Shisha Pangma leucogranites
XiaoChi LIU, , Lei YANG, ShaoXiong HE, FangYang HU, JiaMin WANG, , and
Yanshi Xuebao Acta Petrologica Sinica, 2024
South Tibetan Detachment System activity and leucogranite emplacement:Insights from the Shisha Pangma regions
Yang CHU, , YiLin GUO, TanJie LIU, XiaoChi LIU, FangYang HU, YiYang LEI, Wei LIN, , and
Yanshi Xuebao Acta Petrologica Sinica, 2024
Discovery of the Gangbu spodumene-bearing pegmatite in the Shisha Pangma region and its geological significance
FangYang HU, , HaoLan PU, Zhao GUO, TanJie LIU, XiaoChi LIU, ShaoXiong HE, FuYuan WU, , , and
Yanshi Xuebao Acta Petrologica Sinica, 2024
Cesium-rubidium mineralization in Himalayan leucogranites
Fangyang Hu, Xiaochi Liu, Shaoxiong He, Jiamin Wang, Fuyuan Wu
Science China Earth Sciences, 2023
A combined methodology for reconstructing source-to-sink basin evolution, exemplified by the Triassic Songpan–Ganzi basin, central China
Guohui Chen, Fangyang Hu, Alastair H.F. Robertson, Eduardo Garzanti, Shaohua Zhang, Fu-Yuan Wu
Sedimentary Geology, 2023
Mineralogy, petrology and P-T conditions of the spodumene pegmatites and surrounding meta-sediments in Lhozhag, eastern Himalaya
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, Fu-Yuan Wu
Lithos, 2023
In situ Rb-Sr dating of mica by LA-ICP-MS/MS
Chao Huang, Hao Wang, Wenbei Shi, Jinfeng Sun, Fangyang Hu, Lei Xu, Yueheng Yang, Shitou Wu, Liewen Xie, Jinhui Yang
Science China Earth Sciences, 2023
Potassium isotope fractionation during granite differentiation and implications for crustal K isotope heterogeneity
Zi-Yi Ding, Shan-Ke Liu, Ben-Xun Su, Wen-Jun Li, Yang Bai, Qi-Qi Pan, Fang-Yang Hu, Kwan-Nang Pang
Lithos, 2023
Petrogenesis of the highly fractionated granites and their mineralizations in Nanling Range, South China
FuYuan WU, , ChunLi GUO, FangYang HU, XiaoChi LIU, JunXing ZHAO, XiaoFeng LI, KeZhang QIN, , , and
Yanshi Xuebao Acta Petrologica Sinica, 2023
Oxidation of Archean upper mantle caused by crustal recycling
Lei Gao, Shuwen Liu, Peter A. Cawood, Fangyang Hu, Jintuan Wang, Guozheng Sun, Yalu Hu
Nature Communications, 2022
Quantifying the growth of continental crust through crustal thickness and zircon Hf-O isotopic signatures: A case study from the southern Central Asian Orogenic Belt
Yujian Wang, Dicheng Zhu, Chengfa Lin, Fangyang Hu, Jingao Liu
Bulletin of the Geological Society of America, 2022
Does Large-Scale Crustal Flow Shape the Eastern Margin of the Tibetan Plateau? Insights From Episodic Magmatism of Gongga-Zheduo Granitic Massif
Fangyang Hu, Fu‐Yuan Wu, Mihai N. Ducea, James B. Chapman, Lei Yang
Geophysical Research Letters, 2022
Newly discovered Early Carboniferous and Late Permian magmatic rocks in eastern Myanmar: Implications for the tectonic evolution of the eastern Paleo-Tethys
Fangyang Hu, Fu-Yuan Wu, Jian-Gang Wang, Mihai N. Ducea, James B. Chapman, Khin Zaw, Wei Lin, Kyaing Sein, Sebastien Meffre
Journal of Asian Earth Sciences, 2022
The critical factors of lithium enrichment in the metasedimentary wall rocks of granitic pegmatite-type lithium deposit: Insights from the Ke'eryin area n the eastern Songpan-Ganzi Belt
HU FangYang, , WU FuYuan, CHEN GuoHui, YANG Lei, , , , and
Yanshi Xuebao Acta Petrologica Sinica, 2022
Thermal state and evolving geodynamic regimes of the Meso- to Neoarchean North China Craton
Guozheng Sun, Shuwen Liu, Peter A. Cawood, Ming Tang, Jeroen van Hunen, Lei Gao, Yalu Hu, Fangyang Hu
Nature Communications, 2021
Multistage magmatism recorded in a single gneiss dome: Insights from the Lhagoi Kangri leucogranites, Himalayan orogen
Shao-Xiong He, Xiao-Chi Liu, Lei Yang, Jia-Min Wang, Fang-Yang Hu, Fu-Yuan Wu
Lithos, 2021
Petrogenesis of the Main Range and Eastern Province granites in eastern Myanmar: New insights from zircon U–Pb ages and Sr–Nd isotopes
Feng Cong, Fu-Yuan Wu, Wen-Chang Li, Jian-Gang Wang, Fang-Yang Hu, De-Feng He, Wei-Qiang Ji, Wei Lin, Kyaing Sein
Lithos, 2021
Geochronology, source features and the characteristics of fractional crystallization in pegmatite at the qongjiagang giant pegmatite-type lithium deposit, himalaya, tibet
ZHAO JunXing, , HE ChangTong, QIN KeZhang, SHI RuiZhe, LIU XiaoChi, HU FangYang, YU KeLong, SUN ZhengHao, , and
Yanshi Xuebao Acta Petrologica Sinica, 2021
Discovery of spodumene- bearing pegmatites from Ra Chu in the Mount Qomolangma region and its implications for studying rare-metal mineralization in the Himalayan orogen
LIU XiaoChi, , WU FuYuan, WANG RuCheng, LIU ZhiChao, WANG JiaMin, LIU Chen, HU FangYang, YANG Lei, HE ShaoXiong, , , , and
Yanshi Xuebao Acta Petrologica Sinica, 2021
Late Neoarchean metavokanics and geodynamics regime in central and eastern North China Cratoa
LIU ShuWen, , BAO Han, GAO Lei, SUN GuoZheng, WANG Wei, GUO RongRong, GUO BoRan, FU JingHao, HU YaLu, BAI Xiang, HU FangYang, , , , , , , and
Yanshi Xuebao Acta Petrologica Sinica, 2021
Early Mesozoic magmatism and tectonic evolution of the Qinling Orogen: Implications for oblique continental collision
Fangyang Hu, Shuwen Liu, Mihai N. Ducea, James B. Chapman, Fuyuan Wu, Timothy Kusky
Gondwana Research, 2020
Quantitatively Tracking the Elevation of the Tibetan Plateau Since the Cretaceous: Insights From Whole-Rock Sr/Y and La/Yb Ratios
Fangyang Hu, Fuyuan Wu, James B. Chapman, Mihai N. Ducea, Weiqiang Ji, Shuwen Liu
Geophysical Research Letters, 2020
Origin of the Triassic Lincang granites in the southeastern Tibetan Plateau: Crystallization from crystal mush
Feng Cong, Fu-Yuan Wu, Wen-Chang Li, Chuan-Long Mou, Xiao-Ming Huang, Bao-Di Wang, Fang-Yang Hu, Zhi-Min Peng
Lithos, 2020
Mesozoic crustal growth in Mainland Southeast Asia: Zircon U-Pb and Hf isotopic evidence from the Late Cretaceous Luyingtang granitic pluton in the northernmost SE Asian granite Province, SW China
Feng Cong, Wen-Chang Li, Fu-Yuan Wu, Liang Huang, Xiao-Ming Huang, Jie Sun, Xiao-Chi Liu, Fang-Yang Hu, Shi-Xue Hu, Guang-Hui Wu
Journal of Asian Earth Sciences, 2020
Diverse middle Neoarchean granitoids and the delamination of thickened crust in the Western Shandong Terrane, North China Craton
Yalu Hu, Shuwen Liu, Lei Gao, Guozheng Sun, Rongrong Guo, Jinghao Fu, Maojiang Wang, Fangyang Hu
Lithos, 2019
Precambrian Hongqiyingzi Complex at the northern margin of the North China Craton: Its zircon U-Pb-Hf systematics, geochemistry and constraints on crustal evolution
Shuwen Liu, Jinghao Fu, Yong-Jun Lu, Xu Chen, Maojiang Wang, Fangyang Hu, Lei Gao, Guozheng Sun, Yalu Hu
Precambrian Research, 2019
Neoarchean sanukitoids and associated rocks from the Tengzhou-Pingyi intrusive complex, North China Craton: Insights into petrogenesis and crust-mantle interactions
Guozheng Sun, Shuwen Liu, Lei Gao, Yalu Hu, Rongrong Guo, Jinghao Fu, Maojiang Wang, Chenchen Ma, Fangyang Hu
Gondwana Research, 2019
Neoarchean crust-mantle interactions in the Yishui Terrane, south-eastern margin of the North China Craton: Constraints from geochemistry and zircon U-Pb-Hf isotopes of metavolcanic rocks and high-K granitoids
Lei Gao, Shuwen Liu, Guozheng Sun, Yalu Hu, Rongrong Guo, Jinghao Fu, Maojiang Wang, Fangyang Hu
Gondwana Research, 2019
Neoarchean magmatic arc in the Western Liaoning Province, northern North China Craton: Geochemical and isotopic constraints from sanukitoids and associated granitoids
Jinghao Fu, Shuwen Liu, Peter A. Cawood, Maojiang Wang, Fangyang Hu, Guozheng Sun, Lei Gao, Yalu Hu
Lithos, 2018
Petrogenesis of late Neoarchean high-K granitoids in the Western Shandong terrane, North China Craton, and their implications for crust-mantle interactions
Lei Gao, Shuwen Liu, Guozheng Sun, Rongrong Guo, Yalu Hu, Jinghao Fu, Maojiang Wang, Chenchen Ma, Fangyang Hu
Precambrian Research, 2018
Interaction among magmas from various sources and crustal melting processes during continental collision: Insights from the Huayang intrusive complex of the South Qinling Belt, China
Fangyang Hu, Shuwen Liu, Mihai N Ducea, Wanyi Zhang, James B Chapman, Jinghao Fu, Maojiang Wang
Journal of Petrology, 2018
Lithological Assemblages of Archean Meta-Igneous Rocks in Eastern Hebei-Western Liaoning Provinces of North China Craton, and Their Geodynamic Implications
树文刘, 伟王, 翔白, 荣荣郭, 敬浩付, 博然郭, 方泱胡, 茂江王
Diqiu Kexue Zhongguo Dizhi Daxue Xuebao Earth Science Journal of China University of Geosciences, 2018
Quantifying Crustal Thickness in Continental Collisional Belts: Global Perspective and a Geologic Application
Fangyang Hu, Mihai N. Ducea, Shuwen Liu, James B. Chapman
Scientific Reports, 2017
Late Neoarchean monzogranitic–syenogranitic gneisses in the Eastern Hebei–Western Liaoning Province, North China Craton: Petrogenesis and implications for tectonic setting
Jinghao Fu, Shuwen Liu, Maojiang Wang, Xu Chen, Boran Guo, Fangyang Hu
Precambrian Research, 2017
A reworked ∼3.45 Ga continental microblock of the North China Craton: Constraints from zircon U-Pb-Lu-Hf isotopic systematics of the Archean Beitai-Waitoushan migmatite-syenogranite complex
Shuwen Liu, Maojiang Wang, Yusheng Wan, Rongrong Guo, Wei Wang, Kang Wang, Boran Guo, Jinghao Fu, Fangyang Hu
Precambrian Research, 2017
The geochemical evolution of the granitoid rocks in the South Qinling Belt: Insights from the Dongjiangkou and Zhashui intrusions, central China
Fangyang Hu, Shuwen Liu, Mihai N. Ducea, Wanyi Zhang, Zhengbin Deng
Lithos, 2017
A westward propagating slab tear model for Late Triassic Qinling Orogenic Belt geodynamic evolution: Insights from the petrogenesis of the Caoping and Shahewan intrusions, central China
Fangyang Hu, Shuwen Liu, Wanyi Zhang, Zhengbin Deng, Xu Chen
Lithos, 2016
Petrogenesis of the Guangtoushan granitoid suite, central China: Implications for Early Mesozoic geodynamic evolution of the Qinling Orogenic Belt
Zhengbin Deng, Shuwen Liu, Wanyi Zhang, Fangyang Hu, Qiugen Li
Gondwana Research, 2016
Chronology and tectonic implications of Neoproterozoic blocks in the South Qinling Orogenic Belt, Central China
Fangyang Hu, Shuwen Liu, M. Santosh, Zhengbin Deng, Wei Wang, Wanyi Zhang, Ming Yan
Gondwana Research, 2016
Precambrian geodynamics (VII): Formation and evolution of early continental crust
Earth Science Frontiers, 2015
Geochemistry and zircon U-Pb chronology of Shuangshanzi Group in the eastern Hebei province, North China Craton: Constraints on petrogenesis and tectonic setting
Yanshi Xuebao Acta Petrologica Sinica, 2014

Fangyang Hu

RESEARCH, TEACHING, or OTHER INTERESTS

Scopus Publications

RECENT SCHOLAR PUBLICATIONS

MOST CITED SCHOLAR PUBLICATIONS