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| 1 | Sediment-hosted Pb-Zn Deposits in Southwest Sanjiang Tethys and Kangdian Area on the Western Margin of Yangtze Craton显示文摘Yangtze Craton 的西方的边缘作为重要招待沉积的基础金属的总数簇被知道,特别为在中国的 PbZn 存款,例如 Jinding, Daliangzi, Tianbaoshan, Kuangshanchang 和 Qinlinchang 存款。与在世界上的经典 MVT 存款比较,基于招待沉积的 Pb-Zn 存款的基本地质学,这份报纸集中于这存款的 temporalspatial 分发进一步讨论它的大规模矿化作用和构造进化历史。在 SW Sanjiang Thethys, Jinding 沉积物典型地在沙岩和忍受角砾岩的沙岩主要是控制差错、招待的戳,而 MVT 类型存款被岩性学控制并且为招待碳酸盐的岩石与强壮的偏爱差错 / 破裂。最重要地, Jinding PbZn 沉积物不同于它在一个大陆人碰撞地区以内在强烈使变形的低岬盆在被形成的招待沉积的 PbZn 存款的另外的类型。在 Kangdian 区域,招待沉积的 PbZn 存款沿着 Yangtze Craton 在大陆人 orogenic 带的方面上在 extensional 盆被形成。与经典 MVT 存款相比,在 Kangdian 区域的 PbZn 存款属于 MVT 存款。这份报纸是重要的不仅因为招待沉积的 PbZn 的开始的解释扔而且因为利用大贱金属在大沉积目标区域扔。 | WANG Changming DENG Jun ZHANG Shouting XUE Chunji YANG Liqiang WANG Qingfei SUN Xiang | 2010 | Acta Geologica Sinica(English Edition)2010，84，6： | 33 |
| 2 | Helium,Argon,and Xenon Isotopic Compositions of Ore-forming Fluids in Jinding-Baiyangping Polymetallic Deposits,Yunnan,Southwest China显示文摘The Jinding superlarge lead and zinc deposit has attracted the attention of geologists of the world and itsmetal logenesis has long been in dispute. This paper takes the Jinding deposit and the Baiyangping Cu-Ag-Co deposit which was recently found at about 30 km north of Jinding as one ore belt, and, based on researches on the helium, argon, and xenon isotopic compositions of primary inclusions in ore-forming solutions of the main stage, the authors have found that the 3He/4He ratio of the ore-forming fluid is 2.7×10-6 (varying from 0.19 to 1.97 Ra), the 4He/40Ar ratio (0.24-3.12) is close to the mantle characteristic ratio, and the xenon isotopic composition and evolution show characters of the mantle xenon. The above results reveal the characteristics of mantle source and crust-mantle fluid mixing (mantle helium reaching 32%) and the metallogenic contributions of the deep processes in the Jinding-Baiyangping ore belt. | XUE Chunji WANG Denghong CHEN Yuchuan YANG Jianmin YANG Weiguang | 2000 | Acta Geologica Sinica(English Edition)2000，74，3： | 17 |
| 3 | Effects of hydrocarbon generation on fluid flow in the Ordos Basin and its relationship to uranium mineralization显示文摘诺思中国的 Ordos 盆是不仅一个重要的铀矿化作用省,而且在中国的油,气体和煤的一个主要制片人。在铀矿化作用和烃之间的基因关系被认出了由很多以前的研究,而是它很好没以盆液体的水动力学被理解流动。我们在以前的研究证明了在 Ordos 侏罗记节的上面的部分的白垩纪铀矿化作用的优先的本地化可能与在向上的流动之间的接口有关,减少液体并且向下流动,氧化液体。这个接口可能被在与不平衡沉积压缩有关的液体过压之间的相互影响控制了并且它驾驶了向上的流动,和地志的地势,它开车了向下流动。在这研究,我们执行了为对液体过压的发展的油和煤气的产生的贡献的数字建模,除了沉积压缩并且加热。当烃产生没被考虑时,我们的结果显示当烃产生被考虑时,液体过压非常与模拟比较在白垩纪期间被加倍。而且,在沉积的结束的液体过压驱散相对没有烃产生盒子慢下来。这些结果建议烃产生可能在铀矿化作用,不是仅仅在规定减少为矿化作用要求的代理人,而且在贡献驱动力维持向上的流动起了一个重要作用。 | Chunji Xue Guoxiang Chi Wei Xue | 2011 | Geoscience Frontiers2011，2，3： | 12 |
| 4 | An overview of hydrodynamic studies of mineralization显示文摘液体流动是热水的矿化作用的不可分的部分,并且它的分析和描述组成一个矿化作用模型的重要部分。矿化作用的水动力学学习处理分析驱动力,液体压力政体,液体流动率和方向,并且他们与矿化作用的本地化的关系。这份报纸考察矿化作用的水动力学研究的原则和方法,并且为矿石沉积物研究和矿物质探索讨论他们的意义和限制。流动可能与液体过压,地志的消除,构造变丑,和液体密度有关的液体的驱动力由于加热或咸度变化变化,取决于特定的地质的环境和矿化作用过程。学习方法可以被分类进三种类型,放大了(领域) 观察,显微镜的分析,并且数字建模。放大了的特征陈述语气显著地 overpressured (特别 lithostatic 或 supralithostatic ) 液体系统包括水平静脉,沙注射堤,和水力的角砾岩。显微镜的研究,特别液体包括的 microthermometry 和液体包括飞机(联邦信息处理标准) 的 microthermometry 能关于液体温度,压力,和液体结构的关系提供重要信息,因此抑制液体流动模型。数字建模能被执行解决管理液体流动,热转移,岩石变丑和化学反应的部分微分方程,以便模仿液体的分发在 2D 或 3D 空间并且整个时间的压力,温度,液体流动率和方向,和矿物质降水或溶解。矿化作用的水动力学研究的结果能提高我们热水的沉积物的形成过程的理解,并且能在矿物质探索直接或间接地被使用。 | Guoxiang Chi Chunji Xue | 2011 | Geoscience Frontiers2011，2，3： | 11 |
| 5 | Hydrodynamic regime as a major control on localization of uranium mineralization in sedimentary basins显示文摘Uranium deposits in sedimentary basins can be formed at various depths,from near surface to the basement.While many factors may have played a role in controlling the location of mineralization,examination of various examples in the world,coupled with numerical modeling of fluid flow,indicates that the hydrodynamic regime of a basin may have exerted a major control on the localization of uranium deposits.If a basin is strongly overpressured,due to rapid sedimentation,abundance of low-permeability sediments or generation of hydrocarbons,fluid flow is dominantly upward and uranium mineralization is likely limited at shallow depths.If a basin is moderately overpressured,upward moving fluids carrying reducing agents may meet downward moving,oxidizing,uranium-bearing fluids in the middle of the basin,forming uranium deposits at moderate depths.If a basin is weakly or not overpressured,either due to slow sedimentation or dominance of high-permeability lithologies,minor topographic disturbance or density variation may drive oxidizing fluids to the bottom of the basin,leaching uranium either from the basin or the basement,forming unconformity-type uranium deposits.It is therefore important to analyze the hydrodynamic regime of a basin in order to predict the most likely type and location of uranium deposits in the basin. | CHI GuoXiang XUE ChunJi | 2014 | Science China Earth Sciences2014，57，12： | 6 |
| 6 | Hydrodynamic analysis of clastic injection and hydraulic fracturing structures in the Jinding Zn-Pb deposit,Yunnan,China显示文摘Jinding Zn-Pb 存款通常被考虑了以一个相对被动的方法从传播 basinal 液体形成了,与液体流动被结构和沉积外形正在控制,类似于许多另外的招待沉积的底金属存款。然而,几最近的研究在 Jinding 存款的开的坑揭示了沙注射结构,恼人的角砾岩,和水力的破裂的存在并且建议存款从 overpressured 液体的爆炸版本被形成。这研究报导液体的新观察过压相关从地下的活动方式(Paomaping 和 Fengzishan ) 组织,它比在开的坑显示出更清楚的横切的关系。观察结构包括:1 ) 沙(楳湧晩捩湡汴 ? 潣瑮楲畢整琠? 桴 ? 潴慴? 票牤 ' 夷典? | Guoxiang Chi Chunji Xue Hairuo Qing Wei Xue Jiangwei Zhang Yunqiang Sun | 2012 | Geoscience Frontiers2012，3，1： | 5 |
| 7 | Hydrodynamic Links between Shallow and Deep Mineralization Systems and Implications for Deep Mineral Exploration显示文摘Deep mineral exploration is increasingly important for finding new mineral resources but there are many uncertainties.Understanding the factors controlling the localization of mineralization at depth can reduce the risk in deep mineral exploration.One of the relatively poorly constrained but important factors is the hydrodynamics of mineralization.This paper reviews the principles of hydrodynamics of mineralization,especially the nature of relationships between mineralization and structures,and their applications to various types of mineralization systems in the context of hydrodynamic linkage between shallow and deep parts of the systems.Three categories of mineralization systems were examined,i.e.,magmatic-hydrothermal systems,structurally controlled hydrothermal systems with uncertain fluid sources,and hydrothermal systems associated with sedimentary basins.The implications for deep mineral exploration,including potentials for new mineral resources at depth,favorable locations for mineralization,as well as uncertainties,are discussed. | CHI Guoxiang XU Deru XUE Chunji LI Zenghua Patrick LEDRU DENG Teng WANG Yumeng SONG Hao | 2022 | Acta Geologica Sinica(English Edition)2022，96，1： | 5 |
| 8 | An Updated Database and Spatial Distribution of Landslides Triggered by the Milin, Tibet M_(w)6.4 Earthquake of 18 November 2017显示文摘The M_(w)6.4 earthquake on November 18, 2017 in Milin County, Nyingchi City, Tibet triggered thousands of landslides. By comparing visual interpretation of satellite images acquired shortly before and after the earthquake and field survey, we have created a new landslide database which includes 3 130 coseismic landslides, each with an area of 0.01 to 4.35 km^(2). Six factors(elevation, slope angle, slope aspect, lithology, distance from the epicenter and distance from the seismogenic fault) were selected to correlate with the coseismic landslides. In addition, the area and density of landslides were counted as indicators. Results show that most landslides occurred where the elevation is between 2 000–3 000 m, with a 40°–50° slope angle and S, E or SE slope aspect, schist or gneiss lithologies, 10–15 km from the epicenter, and 5 km within the seismogenic fault. Most of the landslides, triggered by the M_(w)6.4 earthquake, are concentrated near the seismogenic fault rather than at the epicenter, indicating that the seismogenic structure is more influential than the location of the epicenter. Our findings may differ from other landslide database due to temporal image acquisition, interference from weather, and image resolution. | Yuandong Huang Chong Xu Xiaolong Zhang Chunji Xue Shiyuan Wang | 2021 | Journal of Earth Science2021，32，5： | 4 |
| 9 | Cenozoic Mineralization in China,as a Key to Past Mineralization and a Clue to Future Prospecting显示文摘Many Cenozoic metal deposits have been found during the past decade. Among them, the Fuwan Ag deposit in Guangdong is the largest Ag deposit in China. Besides, the largest Cu deposit of China in Yulong, Tibet, the largest Pb-Zn deposit of China in Jinding, Yunnan, and the largest Au deposit of China in Jinguashi,Taiwan, were also formed in the Cenozoic. Why so many important 'present' deposits formed during such a short period of geological history is the key problem. The major reason is that different tectonic settings control different kinds of magmatic activity and mineralization at the same time. In southwestern China, porphyry-type Cu deposits such as Yulong were formed during the early stage of the Himalayan orogeny, sediment-hosted Pb-Zn deposits such as Jinding were formed within intermontane basins related to deep faults, and carbonatite-related deposits such as the Maoniuping REE deposit and alkalic magmatic rock-related deposits such as the Beiya Au deposit originated from the mantle source. | WANG Denghong CHEN Yuchuan XU Jue YANG Jianmin XUE Chunji YAN Shenghao | 2000 | Acta Geologica Sinica(English Edition)2000，74，3： | 4 |
| 10 | Expansion of the South China Sea basin:Constraints from magnetic anomaly stripes,sea floor topography,satellite gravity and submarine geothermics显示文摘The widely distributed E-W-trending magnetic anomaly stripes in the central basin and the N-Etrending magnetic anomaly stripes in the southwest sub-basin provide the most important evidence for Neogene expansion of the South China Sea.The expansion mechanism remains,however,controversial because of the lack of direct drilling data,non-systematic marine magnetic survey data,and irregular magnetic anomaly stripes with two obvious directions.For example,researchers have inferred different ages and episodes of expansion for the central basin and southwest sub-basin.Major controversy centers on the order of basinal expansion and the mechanism of expansion for the entire South China Sea basin.This study attempts to constrain these problems from a comprehensive analysis of the seafloor topography,magnetic anomaly stripes,regional aeromagnetic data,satellite gravity,and submarine geothermics.The mapped seafloor terrain shows that the central basin is a north-south rectangle that is relatively shallow with many seamounts,whereas the southwest sub-basin is wide in northeast,gradually narrows to the southwest,and is relatively deeper with fewer seamounts.Many magnetic anomaly stripes are present in the central basin with variable dimensions and directions that are dominantly EWtrending,followed by the NE-,NW- and NS-trending.Conversely such stripes are few in the southwest sub-basin and mainly NE-trending.Regional magnetic data suggest that the NW-trending Ailaoshan-Red River fault extends into the South China Sea,links with the central fault zone in the South China Sea,which extends further southward to Reed Tablemount.Satellite gravity data show that both the central basin and southwest sub-basin are composed of oceanic crust.The Changlong seamount is particularly visible in the southwest sub-basin and extends eastward to the Zhenbei seamount.Also a low gravity anomaly zone coincides with the central fault zone in the sub-basin.The submarine geothermic distribution demonstrates that the southwest sub-basin has a higher geothermal value than the central basin,and that the central fault zone is defined by a low thermal anomaly.This study suggests that NW-SE expansion of the southwest subbasin is later than the N-S expansion of the central basin with the sub-basin extending into the central basin and with both expansions ending at the same time.The expansion of southwestern sub-basin,similar to the Japanese Sea,is likely caused by left-lateral strike slip on the central fault zone in the South China Sea,which may have significance for finding oil and gas in this region. | Xuezhong Yu Chunji Xue Haigang Shi Weiping Zhu Yinghui Liu Hang Yin | 2017 | Geoscience Frontiers2017，8，1： | 3 |
| 11 | Geologic, fluid inclusion and isotopic characteristics of the Jinding Zn-Pb deposit, western Yunnan, South China : a review 显示文摘 | XUE Chunji ZENG Rong LIU Shuwen | 2007 | Ore Geology Reviews2007，31，1234： | 1 |
| 12 | Engineering porosity into trimetallic PtPdNi nanospheres for enhanced electrocatalytic oxygen reduction activity显示文摘Platinum(Pt)-based multi-metallic nanostructures show great promise as electrocatalysts for the oxygen reduction reaction(ORR) in fuel cell cathodes. Herein, we report a simple, one-step surfactant-directed synthetic strategy to directly synthesize tri-metallic PtPdNi mesoporous nanospheres(PtPdNi MNs) in a high yield. The synthesis could be accomplished in aqueous solution at mild reaction temperature(40C)without needing any organic solvent, yielding well-dispersed PtPdNi MNs with uniform shape and narrow size distribution. Benefitting from their unique mesoporous and highly open structure and tri-metallic composition, the as-synthesized PtPdNi MNs demonstrate superior catalytic activity and stability for ORR in acidic solution in comparison with PtPdNi nanodendrites(PtPdNi NDs), PtPd MNs and commercial Pt/C catalyst. The present approach may open a reliable path to the design of advanced electrocatalysts with desired performance. | Chunjie Li You Xu Yinghao Li Hongjie Yu Shuli Yin Hairong Xue Xiaonian Li Hongjing Wang Liang Wang | 2018 | Green Energy & Environment2018，3，4： | 1 |
| 13 | Sand injection and Liquefaction structures in the Jinding Zn-Pb deposit,Yunnan, China: indicators of an overpressured fluid system and implications for mineralization 显示文摘 | Chi Guoxiang Xue Chunji Lai Jianqing | 2007 | Economic Geology2007，102，4： | 1 |
| 14 | Mierogranular enclaves in island- arc andesites: A possible link between known epithermal Au and potential porphyry Cu-Au deposits in the Tulasu ore cluster, western Tianshan, Xinjiang, China显示文摘 | Zhao Xiaobo Xue Chunji David T A Symons | 2014 | Journal ofAsian Earth Sciences2014，85，： | 1 |
| 15 | Multiple and prolonged porphyry Cue Au mineralization and alteration events in the Halasu deposit, Chinese Altai, Xinjiang,northwestern China显示文摘The Halasu area is located in the southeastern margin of the Chinese Altai in Xinjiang, China. It is part of the Altaid orogenic collage where a number of porphyry-type Cue Moe Au deposits have been discovered in recent years. Geological mapping and drilling indicate the presence of various mineralized porphyritic intrusions in the Halasu Cue Au deposit, which is currently under exploration. Ue Pb dating of zircon crystals from four different mineralized porphyries reveals three significantly different ages of magmatic intrusion, i.e., ca. 372e382 Ma granodioritic porphyry and porphyritic granite, ca. 266 Ma quartz monzonitic porphyry, and ca. 216 Ma quartz dioritic porphyry. Ree Os dating of molybdenite from veinletdissemination ores in the granodioritic porphyry yields an age of mineralization of ca. 377 Ma, and Ar e Ar dating of K-feldspar from K-feldsparequartzechalcopyrite veins produces ages of ca. 269 and ca.198 Ma. The mineralization(and alteration) ages correspond broadly to the three episodes of magmatic intrusion, suggesting three overprinting porphyry mineralization events that are significantly separated in time. The first episode of porphyry intrusion and mineralization may be related to the magmatic arc being above a plate subduction zone, and the second was formed in a late-collisional environment during the closing of the Junggar Ocean, whereas the third episode of mineralization took place in the postcollisional stage. This case study suggests that in orogens where major porphyry deposits have been found in magmatic arc environments, the potential of discovering late- to post-collisional porphyry deposits cannot be neglected; conversely, in orogens where most porphyry deposits have late- to postcollisional ages, more attention should be paid to porphyries that were formed earlier in magmatic arc environments. | Chunji Xue Guoxiang Chi Xiaobo Zhao Ganguo Wu Zhanfeng Zhao Lianhui Dong | 2016 | Geoscience Frontiers2016，7，5： | 1 |
| 16 | Sand in- jection and Liquefaction structures in the Jinding Zn-Pb deposit, Yunnan, China : indicators of an overpressured fluid system and implications for mineralization 显示文摘 | Chi Guoxiang Xue Chunji Lai Jianqing | 2007 | Eco- nomic Geology2007，102，4： | 1 |
| 17 | Modeling of fluid pressure evolution related to sediment loading and thrust faulting in the Lanping basin: Implications for the formation of the Jinding Zn-Pb deposit, Yunnan, China 显示文摘 | Chi Guoxiang Qing Hairuo Xue Chunji Zeng Rong | 2006 | J Geochem Explor2006，89，13： | 1 |
| 18 | Two fluid systems in the Lanping basin, Yunnan, China - Their interaction and implications for mineralization 显示文摘 | Xue Chunji Chi Guoxiang Chen Yuchuan Wang Denghong Qing Hairuo | 2006 | J Geochem Explor2006，89，13： | 1 |
| 19 | Geologic, fluid inclusion and isotopic characteristics of the Jinding Zn-Pb deposit, western Yunnan, South China: A review 显示文摘 | Xue Chunji Zeng Rong Liu Shuwen Chi Guoxiang Qing Hairuo Chen Yuchuan Yang Jianmin Wang Denghong | 2007 | Ore Geol Rev2007，31，14： | 1 |
| 20 | Introduction to thematic section on hydrodynamic studies of mineralization显示文摘1.Introduction Most metallic mineral deposits formed from hydrothermal fluids,and the mineralization processes include both chemical (e.g.,fluid-rock and fluid-fluid interactions)and physical(e.g., fluid flow)aspects.More attention has been paid to the chemical processes than the physical ones,even though the latter is equally important in controlling the formation of mineral deposits and their localization.Nevertheless,a number of studies have been carried out regarding the hydrodynamics of fluid flow associated with ore mineralization(e.g.,Cathles,1981,1997; Garven and Raffensperger,1997;Cathles and Adams,2005; Cox,2005;Ingebritsen et al.,2006),and it is timely to eval- | Guoxiang Chi Department of Geology,University of Regina, Regina,Saskatchewan,Canada Chunji Xue State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences, Xueyuan Road 29,Beijing 100083,China | 2011 | Geoscience Frontiers2011，2，3： | 0 |
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