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| 1 | Multiple-aged granitoids and related tungsten-tin mineralization in the Nanling Range, South China显示文摘The Nanling metallogenic belt in South China is characterized by well-developed tungsten-tin mineralization related to multiple-aged granitoids.This belt is one of the 5 key prospecting and exploration areas among the 19 important metallogenic targets in China.Important progress has been made in recent years in understanding the Nanling granitoids and associated mineralization,and this paper introduces the latest major findings as follows:(1)there exists a series of Caledonian,Indosinian,and Yanshanian W-Sn-bearing granites;(2)the Sn-bearing Yanshanian granites in the Nanling Range form an NE-SW trending aluminous A-type granite belt that stretches over 350 km.The granites typically belong to the magnetite series,and dioritic micro-granular enclaves with mingling features are very common;(3)the Early Yanshanian Sn-and W-bearing granites possess different petrological and geochemical features to each other:most Sn-bearing granites are metaluminous to weakly peraluminous biotite(hornblende)granites,with zircon Hf(t)values of ca.2 to 8,whereas most W-bearing granites are peraluminous two-mica granites or muscovite granites with Hf(t)values of ca.8 to 12;(4)based on the petrology and geochemistry of the W-Sn-bearing granites,mineralogical studies have shown that common minerals such as titanite,magnetite,and biotite may be used as indicators for discriminating the mineralizing potential of the Sn-bearing granites.Similarly,W-bearing minerals such as wolframite may indicate the mineralizing potential of the W-bearing granites.Future studies should be focused on examining the internal relationships between the multiple-aged granites in composite bodies,the metallogenic peculiarities of multiple-aged W-Sn-bearing granites,the links between melt evolution and highly evolved ore-bearing felsic dykes,and the connections between granite domes and mineralization. | CHEN Jun WANG RuCheng ZHU JinChu LU JianJun MA DongSheng | 2013 | Science China Earth Sciences2013，56，12： | 46 |
| 2 | A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts, South Tibet显示文摘The Himalayan leucogranite occurs as two extensive(>1000 km) E-W trending belts on the Tibetan Plateau with the unique features. The leucogranite comprised biotite granite, two-mica/muscovite granite, tourmaline granite and garnet granite, which have been identified in previous studies, as well as albite granite and granitic pegmatite that were identified in this investigation. Fifteen leucogranite plutons were studied and 12 were found to contain rare-metal bearing minerals such as beryl(the representative of Be mineralization), columbite-group minerals, tapiolite, pyrochlore-microlite, fergusonite, Nb-Ta rutile(the representative of Nb-Ta mineralization), and cassiterite(the representative of Sn mineralization) mainly based on the field trip,microscope observation and microprobe analysis. The preliminary result shows that the Himalayan leucogranite is commonly related to the rare-metal mineralization and warrants future investigation. Further exploration and intensive research work is important in determining the rare-metal resource potential of this area. | WANG RuCheng WU FuYuan XIE Lei LIU XiaoChi WANG JiaMin YANG Lei LAI Wen LIU Chen | 2017 | Science China Earth Sciences2017，60，9： | 45 |
| 3 | Formation history and protolith characteristics of granulite facies metamorphic rock in Central Cathaysia deduced from U-Pb and Lu-Hf isotopic studies of single zircon grains显示文摘The petrochemical as well as zircon U-Pb and Lu-Hf isotopic studies of granulite facies metamorphic rock from the Taoxi Group in eastern Nanling Range, Central Cathaysia indicate that its protolith is the sedimentary rock with low maturation index. The clastic materials are mostly from middle Neoproterozoic (~736 Ma) granitoid rocks with minor Neoarchaean and Paleoproterozoic rocks. The timing of this Neoproterozoic magmatism is in agreement with the second period of magmatism widespread surrounding the Yangtze Block. Hf isotopic data indicate that the Neoproterozoic granitoids resulted from the recycled Paleoproterozoic mantle-derived crustal materials. The sedimentary rock was deposited in Late Neoproterozoic Era, and carried into low crust in Early Paleozoic. The partial melting of the meta-sedimentary rock took place at about 480 Ma and subsequently granulite facies metamorphism occurred at ca. 443 Ma. The zircons forming during this time interval (Early Paleozoic) show large Hf isotope variations, and their -Hf(t) values increase from -13.2 to +2.36 with decreasing age, suggesting the injection of mantle-derived materials during partial melting and metamorphism processes in the Early Paleozoic. Calculation results show that this metamorphic rock, if evolved to Mesozoic, has similar isotopic composition to the nearby Mesozoic high Si peraluminous granites, implying that this kind of granulite facies metamorphic rock is probably the source material of some Mesozoic peraluminous granitoids in eastern Nanling Range. | YU Jinhai ZHOU Xinmin Y. S. O'Reilly ZHAO Lei W. L. Griffin WANG Rucheng WANG Lijuan CHEN Xiaomin | 2005 | Chinese Science Bulletin2005，50，18： | 35 |
| 4 | Zircon U-Pb dating confirms existence of a Caledonian scheelite-bearing aplitic vein in the Penggongmiao granite batholith, South Hunan显示文摘Granite at Penggongmiao is a large batholith in the Nanling Range, with an outcrop area of over 900 km 2 . There are many scheelite-quartz veins around the granite. LA-ICP-MS U-Pb dating was carried out for zircons from the granite. The middlecoarse-grained biotite granite has U-Pb ages of 435 to 436 Ma. Ages of 426.5±2.5 Ma were obtained for aplitic dyke cross-cutting the granite. The scheelite of magmatic origin in the aplite dyke was identified from petrographic investigation. This demonstrates that W-bearing granites of Early Paleozoic (corresponding to the Caledonian orogensis in the traditional sense) occur in the Nanling Range. This finding has important implications for the ore-forming potential of Paleozoic granites and on the extent of Mesozoic mineralization. Thus it merits performing an intensive study of Paleozoic granites in South China. The occurrences of aplite or microgranite may be an indicative of the Caledonian tungsten granites and associated W mineralization. | ZHANG WenLan WANG RuCheng LEI ZeHeng HUA RenMin ZHU JinChu LU JianJun XIE Lei CHE XueDong ZHANG RongQing YAO Yuan CHEN Jun | 2011 | Chinese Science Bulletin2011，56，19： | 23 |
| 5 | Diversity of Mesozoic tin-bearing granites in the Nanling and adjacent regions,South China:Distinctive mineralogical patterns显示文摘The Nanling and adjacent regions of South China host a series of tin deposits related to Mesozoic granites with diverse petrological characteristics. The rocks are amphibole-bearing biotite granites, or(topaz-) albite-lepidolite(zinnwaldite) granites,and geochemically correspond to mealuminous and peraluminous types, respectively. Mineralogical studies demonstrate highly distinctive and critical patterns for each type of granites. In mealuminous tin granites amphibole, biotite and perthite are the typical rock-forming mineral association; titanite and magnetite are typical accessory minerals, indicating high fO2 magmatic conditions;cassiterite, biotite and titanite are the principal Sn-bearing minerals; and pure cassiterite has low trace-element contents. However,in peraluminous tin granites zinnwaldite-lepidolite, K-feldspar and albite are typical rock-forming minerals; topaz is a common accessory phase, indicative of high peraluminity of this type of granites; cassiterite is present as a uniquely important tin mineral,typically rich in Nb and Ta. Mineralogical distinction between the two types of tin granites is largely controlled by redox state,volatile content and differentiation of magmatic melts. In oxidized metaluminous granitic melts, Sn4+ is readily concentrated in Ti-bearing rock-forming and accessory minerals. Such Sn-bearing minerals are typical of oxidized tin granites, and are enriched in granites at the late fractionation stage. In relatively reduced peraluminous granitic melts, Sn2+ is not readily incorporated into rock-forming and accessory minerals, except for cassiterite at fractionation stage of granite magma, which serves as an indicator of tin mineralization associated with this type of granites. The nature of magma and the geochemical behavior of tin in the two types of granites thus result in the formation of different types of tin deposits. Metaluminous granites host disseminated tin mineralization,and are locally related to deposits of the chlorite quartz-vein, greisen, and skarn types. Greisen, skarn, and quartz-vein tin deposits can occur related to peraluminous granites, but disseminated mineralization of cassiterite is more typical. | WANG RuCheng XIE Lei LU JianJun ZHU JinChu CHEN Jun | 2017 | Science China Earth Sciences2017，60，11： | 12 |
| 6 | Skarn-type tungsten mineralization associated with the Caledonian(Silurian) Niutangjie granite, northern Guangxi, China显示文摘The Niutangjie tungsten deposit is a bedded skarn-type scheelite deposit and is located at the junction between Ziyuan and Xingan counties in the north of Guangxi,China.The deposit is genetically related to a fine-grained two-mica granite within the orefield.Zircon LA-ICP-MS U-Pb dating of the granite yielded a Silurian(Caledonian)age of 421.8±2.4 Ma,which is contemporaneous with the adjacent Yuechengling batholith.Mineralization within the skarn is associated with a quartz,garnet,and diopside gangue,and scheelite is present in a number of different mineral assemblages,such as quartz-scheelite and quartz-sulfide-scheelite;these assemblages correspond to oxide and sulfide stages of mineralization.Sm-Nd isotope analysis of scheelite yielded an isochron age of 421±24 Ma.Although the uncertainty on this date is high,this age suggests that the scheelite mineralization formed during the Late Caledonian,at a similar time to the emplacement of the Niutangjie granite.Zircons within the granite have?Hf(t)values and Hf two-stage model ages of?6.5 to?11.6,and 1.79 to 2.11 Ga,respectively.These data suggest that the magma that formed the granite was derived from Mesoproterozoic crustal materials.Scheelite?Nd(t)values range from?13.06 to?13.26,also indicative of derivation from ancient crustal materials.Recent research has identified Caledonian magmatism in the western Nanling Range,indicating that this magmatism may be the source of contemporaneous tungsten mineralization. | YANG Zhen WANG RuCheng ZHANG WenLan CHU ZhuYin CHEN Jun ZHU JinChu ZHANG RongQing | 2014 | Science China Earth Sciences2014，57，7： | 11 |
| 7 | Primary Sn-rich titianite in the Qitianling granite, Hunan Province, southern China: An important type of tin-bearing mineral and its implications for tin exploration显示文摘The Qitianling calc-alkaline granite in Hunan Province (South China) has attracted much attention since the discovery of the Furong super-large tin deposit. The present study provides new mineralogical data to address their implications for exploration of tin deposits. In the Taoxiwo granite in the southeastern part of the Qitianling granite body, Sn-rich titanite was identified as an important type of Sn-bearing mineral. The titanite commonly occurs with biotite as euhedral crystals, exhibiting typical envelope-like shape and sector-zoning texture. These indicate that the titanite most likely crystallized in the mag-matic stage. Electron-microprobe analyses show that the titanite is enriched in tin up to 1.12 wt% SnO2, with an average of 0.43 wt%. With the crystallization of the granite, primary minerals undertook hydro-thermal alteration by magma-derived fluids. Subsequently, in the hydrothermal stage, the primary Sn-bearing titanite was altered (at least partially), but still preserved its typical envelope-shaped outline. Micro-scale cassiterite is a representative product of such alteration; other secondary minerals include fluorite, ilmenite, Sn-bearing rutile and quartz. Therefore, the titanite, commonly present in the calc- alkaline granites, can be treated as an important Sn-carrying mineral in the Qitianling granite, reflecting the primary magmatic environment with tin enrichment. The hydrothermal alteration of the primary titanite and subsequent crystallization of cassiterite recorded a process of leaching and accumulation of tin in magmatic-hydrothermal evolution of the Snbearing granite. Thus, this titanite has important implications for tin exploration. | XIE Lei WANG RuCheng CHEN Jun ZHU JinChu ZHANG WenLan WANG DeZi YU APeng | 2009 | Chinese Science Bulletin2009，54，5： | 10 |
| 8 | Timing of hydrothermal activity associated with the Douzhashan uranium-bearing granite and its significance for uranium mineralization in northeastern Guangxi, China显示文摘The Miaoershan uranium(U)ore field in northeastern Guangxi is one of the important granite-related U deposits in south China and is closely related to the Douzhashan U-bearing granite.The Douzhashan granite contains primary U-rich accessory minerals,including monazite(UO2=0.98-1.75 wt%)and xenotime(UO2=1.48-6.14 wt%).Primary monazite and xenotime yield chemical ages of 231±28 Ma and 230±38 Ma by electron microprobe analysis and U-Pb isotopic ages of 220±6 Ma and 211±7 Ma by laser ablation-inductively coupled-mass spectrometry respectively.These ages demonstrate that the Douzhashan granite formed during the period of Indosinian magmatic activity.Back scattered electron imaging shows that monazite and xenotime are commonly altered to assemblages of low-U synchisite and apatite,which was associated with loss of U to hydrothermal fluids.U-Th-Pb analyses of secondary apatite yielded a chemical age of 136±17 Ma,which corresponds to the timing of Cretaceous-Tertiary crustal extension in south China.We suggest that the heat and CO2required for mineralization was the result of Yanshanian crustal extension,and that this triggered the breakdown of U-rich accessory minerals in the Douzhashan U-bearing granite.Uranium remobilization from the Douzhashan granite provided materials for mineralization within the granite and/or surrounding country rocks.Therefore,a combination of Indosinian compression and Yanshanian extensional overprint produced the hydrothermal U deposits associated with the Douzhashan granite. | HU Huan WANG RuCheng CHEN WeiFeng CHEN PeiRong LING HongFei LIU GuoNing | 2013 | Chinese Science Bulletin2013，58，34： | 10 |
| 9 | A study on the Dushiling tungsten-copper deposit in the Miao'ershan-Yuechengling area, Northern Guangxi, China:Implications for variations in the mineralization of multi-aged composite granite plutons显示文摘The polymetallic Dushiling W-Cu deposit is a large, altered, skarn-type deposit, located in the northeastern part of the Miao'ershan-Yuechengling pluton, China. Two types of granite have been identified in the deposit: a medium-grained porphyritic biotite granite, and a medium- to fine-grained biotite granite. Both are spatially and temporally related to ore bodies, suggesting they may be the source of mineralization in the deposit. A medium- to fine-grained porphyritic biotite granite is exposed at the surface in the region of mineralization. U-Pb dating of zircons yielded magmatic ages of 423 Ma for the medium-grained porphyritic biotite granite and 421 Ma for the medium- to fine-grained porphyritic biotite granite, while a younger age(217 Ma) obtained for surface samples indicates later diagenesis. Thus, magmatism occurred during the Caledonian and Indosinian, respectively. The petrological and geochemical characteristics of the two Caledonian granites show that both are calc-alkaline and peraluminous.They are moderately enriched in Cs, Rb, U, and REE, and strongly depleted in Sr,Ba,P,and Ti; they show similar REE behavior,including negative Eu anomalies. These geochemical similarities suggest that the two granites were derived from the same source,although they were emplaced during different stages of the evolution of the magma. Furthermore, the granites are associated with mineralization, suggesting they were the source of mineralization in the Dushiling W-Cu deposit. Sm-Nd ages of scheelite from the Dushiling W-Cu deposit indicate that metallogenesis occurred at 417±35 Ma, while the two types of titanite, intergrown with scheelite, yield U-Pb ages of 423–425 Ma(in altered granite sample) and 218 Ma(in skarn sample). These ages place the main mineralization event in the late Caledonian, and later magmatic-hydrothermal activity occurred in the Indosinian. The ages obtained for the Dushiling W-Cu deposit in the western Nanling Range, northern Yuechengling, together with the occurrence and ages of the Niutangjie W deposit in southern Yuechengling, provide insight into the process of ore concentration during the Caledonian and Indosinian. | CHEN WenDi ZHANG WenLan WANG RuCheng CHU ZhuYin XIAO Rong ZHANG Di CHE XuDong | 2016 | Science China Earth Sciences2016，59，11： | 10 |
| 10 | U-Pb dating of zircon grains from the ore-bearing plagioclase amphibolite in the Dashuigou Te deposit显示文摘The Dashuigou Te deposit is a unique independent one found in the world, and hosted in the plagioclase amphibolite. The upper intercept age of single zircon from the amphibolite can be considered to be the crystallization age of the source-rock of the amphibolite (tholeiitic basalt), while the lower intercept is nearly consistent with the time of the tectono-thermal event. | Shijin Xu Weizhou Shen Rucheng Wang Jianjun Lu Xiaoming Chen Yuping Lin | 1998 | Chinese Science Bulletin1998，43，17： | 5 |
| 11 | A New Potential Caledonian–Indosinian Ore Concentration Area:Evidence from Diagenesis and Mineralization Ages of the Miao'ershan–Yuechengling Region显示文摘Objective The Miao’ershan–Yuechengling composite granite,located in northern Guangxi at the western section of the Nanling Range,is a multi-period and multi-stage composite pluton with an exposed area of more than 3000km2(Fig.1).Paleozoic and Proterozoic strata are exposed around it,and magmatic activities mainly occurred | ZHANG Wenlan CHE Xudong CHEN Wendi WANG Rucheng ZHANG Di | 2017 | Acta Geologica Sinica(English Edition)2017，91，2： | 3 |
| 12 | The P_2O_5 content of feldspars from the Yashan granites,Jiangxi Province, South China显示文摘The P2O5 contents of feldspars in the Yashan F-rich and P-rich granite yield a maximum value of 0.93% (in albite) and a maximum average value of 0.65% (hereinafter weight percent) (in K-feldspar), and is generally between 0.10% and 0.35%. Most of the distribution coefficient Dp[Ab/Kf] values are greater than 1 (1.13—28.9). The study shows that phosphorus could preferably enter the albite structure mainly by PAISi2 substitution relative to K-feldspar. | HUANG Xiaolong, WANG Rucheng , LIU Changshi, YIN Lin, CHEN Xiaoming and CHEN PeirongState Key Laboratory of Mineral Deposit Research , Department of Earth Sciences , Nanjing University, Nanjing 210093 , China Corresponding author | 1999 | Chinese Science Bulletin1999，44，13： | 1 |
| 13 | Accessory minerals in the Xihuashan Y-enriched granitic complex, southern China: A record of magmatic and hydrothermal stages of evolution 显示文摘 | Wang Rucheng Fontan Francois Chen Xiaoming Hu Huan Liu Changshi Xu Shijin and Philippe de Parseval | 2003 | Canadian Mineralogist2003，41，3： | 1 |
| 14 | Vertical variations in the mineralogy of the Yichun Topaz-Lepidolite granite, Jiangxi Province, southern China 显示文摘 | Huang Xiaolong Wang Rucheng Chen Xiaoming Hu Huan Liu Changshi | 2002 | Canadian Mineralogist2002，40，4： | 1 |
| 15 | Designing anticancer combretastatin A-4 analogues with aggregation-induced emission characteristics显示文摘Herein a series of combretastatin A-4(CA-4)analogues with aggregation-induced emission characteristics(compounds a1-a19)were rationally designed and synthesized.The research results showed that the mechanism of AIE of a1-a19 could be attributed to the dual function of the restriction of intramolecular motion(RIM)and J-aggregate formation.Furthermore,the detailed investigation on the action mechanisms revealed that a19 diffused from lysosomes into the cytoplasm,and then targeted the colchicine binding site to induce cell cycle arrest and apoptosis in cancer cells.These results provide new ideas and impetus for the rational design of CA-4 analogues. | Rucheng Zhao Yusheng Wu Yuequn Zhang Jiabao Ling Xinxin Liu Jiaqi Xiang Xiangchao Zeng Tianfeng Chen | 2022 | Science China Chemistry2022，65，4： | 1 |
| 16 | Accessory minerals in the Xihuashan Y-enriched granite complex, southern China: A record of magmatic and hydrothermal stages of evolution显示文摘 | Wang Rucheng Fontan F Chen Xiaoming Hu Huan Liu Changshi Xu Shijin de Parseval P | 2003 | Can Mineral2003，41，3： | 1 |
| 17 | First-principles study of He point-defects in HCP rare-earth metals显示文摘He defect properties in Sc, Y, Gd, Tb, Dy, Ho, Er and Lu were studied using first-principles calculations based on density functional theory. The results indicate that the formation energy of an interstitial He atom is smaller than that of a substitutional He atom in all hcp rare-earth metals considered. Furthermore, the tetrahedral interstitial position is more favorable than an octahedral position for He defects. The results are compared with those from bcc and fcc metals. | YANG LI CHEN RuCheng PENG ShuMing LONG XingGui WU ZhongCheng GAO Fei ZU XiaoTao | 2011 | Science China(Physics,Mechanics & Astronomy)2011，54，5： | 1 |
| 18 | Vertical variations in the mineralogy of the Yichun topaz- lepidolite granite, Jiangxi Province, South China 显示文摘 | Huang Xiaolong Wang Rucheng Chen Xiaoming | 2002 | Can Mineral2002，40，： | 1 |
| 19 | Joint Effects of Heat Stress and PM_(2.5) Exposure on Glucose Metabolism and Hepatic Insulin Signaling显示文摘Background:Heatwave events occur more frequently,accompanied by a significant increase in the ambient concentration of fine particulate matter(PM 2.5).Epidemiological and experimental studies have suggested that heat stress or PM 2.5 exposure would impair glucose homeostasis and insulin sensitivity.Objective:To explore the joint effects of heat stress and PM 2.5 exposure on glucose metabolism and hepatic insulin pathway.Methods:C57BL/6 mice were randomly divided into filtered air(FA)group,fine particulate matter(PM)group,filtered air combined with heat stress(FH)group,and PM combined with heat stress(PH)group.Mice were exposed to PM for a total of 6 weeks,and heat stress combined with PM exposure was applied at the 5th and 6th weeks via a whole-body exposure system.Systemic glucose homeostasis,insulin sensitivity,and circulating inflammatory cytokines were examined.HSP72 expression and insulin signaling in the liver were measured.Results:Glucose tolerance and insulin sensitivity were impaired in response to heat stress,accompanied by less-ened hepatic GLUT2 expression and inhibited insulin signaling pathway.No synergistic effects of heat stress and PM 2.5 exposure on glucose homeostasis were observed,while heat-upregulated HSP72 expression was attenuated with accumulated TNF��induced by further PM 2.5 exposure.Conclusion:Heat stress combined with PM 2.5 exposure induced TNF��,which could inhibit heat-elevated hepatic HSP72 expression.Elevated circulating TNF��impaired hepatic insulin signaling and GLUT2 expression.Then,glucose homeostasis was perturbed,and insulin action was impaired. | Weijia Gu Ziwei Cai Ruiqing Wang Mianhua Zhong Lung-Chi Chen Lu Zhang Rucheng Chen Ran Li Li Qin Qinghua Sun Cuiqing Liu | 2023 | Clinical Complementary Medicine and Pharmacology2023，3，2： | 0 |
| 20 | Mineral Resource Science in China:Review and perspective显示文摘Mineral resources are essential to prosperity and security of modern societies.How mineral resources can guar-antee sustainable development of economy in countries,especially those developing countries,has long been a focus of attention of international communities.This paper provides a comprehensive summary for major ad-vance of the research on mineral resources in past decades,and proposes some key issues regarding ore-forming mechanism,exploration and utilization of major and critical mineral resources.On the basis of these aspects,we also identify four priority science issues to be addressed in the future,including(1)mechanism of both metal circulation and extremely high concentration,(2)theories and technologies of prospecting deep-earth resources,(3)investigation of mineral resources in seafloor and polar regions,and(4)efficient,clean and recycling utiliza-tion of mineral resources.It can be expected that new advances in these four issues would tremendously promote the innovation of mineral resource science,and provide scientific and technologic support to meet the demand of mineral resources for human activities and the harmonious development of both mineral-resource exploration and ecological restoration. | Mingguo Zhai Ruizhong Hu Yan Wang Shaoyong Jiang Rucheng Wang Jianwei Li Huayong Chen Zhiming Yang Qingtian Lü Tao Qi Xuefa Shi Yuansheng Li Jianming Liu Ziying Li Xiyan Zhu | 2021 | Geography and Sustainability2021，2，2： | 0 |
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