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| 1 | A review of mineral systems and associated tectonic settings of northern Xinjiang,NW China显示文摘在这份报纸我们在场在北 Xinjiang 的矿物质系统的评论, NW 中国,集中于 Tianshan,韦斯特和东方 Junggar 和 Altay orogenic 系上带子,所有哪个是更大的中央亚洲 Orogenic 带(CAOB ) 的部分。CAOB 是古老的 microcontinents,岛弧,海洋的 plateaux 和海洋的盘子的复杂大杂烩,它在早 Palaeozoic 被混合并且增大到早二叠的时间。CAOB 大杂烩的建立被罢工滑倒运动跟随并且由 intraplate magmatism 影响了,连接了到披风羽毛活动,最好由 250 个妈西伯利亚的陷井和 280 妈 Tarim 事件例示。在北 Xinjiang,有众多、经济地重要的矿物质系统。在这贡献,我们描述代表性的矿藏的一种选择,包括 subduction 相关的斑岩和 epithermal 沉积物, volcanogenic 巨大的硫醚和 skarn 系统。砍招待地区的 Au 矿脉可能是首先形成了在罢工滑倒期间侵入相关、随后重做变丑。Intraplate magmatism 导致了炮兵阵地同中心地 zoned (阿拉斯加人风格) maficultramafic 侵入,许多哪个主人 orthomagmatic 硫醚沉积物。在 Altay orogen 的伟晶岩的一条巨大的带,局部地招待世界级的稀罕金属沉积物。转动前面,招待沙岩的 U mineralisation 完成北 Xinjiang 岩层的富有的矿物质天赋。 | Franco Pirajno Reimar Seltmann Yongqiang Yang | 2011 | Geoscience Frontiers2011，2，2： | 39 |
| 2 | The Muruntau gold deposit(Uzbekistan)--A unique ancient hydrothermal system in the southern Tien Shan显示文摘The Muruntau gold deposit in the Central Kyzylkum,Uzbekistan is one of the largest single gold deposits worldwide.Data available from the literature are reviewed with the aim to(1) integrate the present knowledge on this unique deposit from Russian and English literature;(2) show the considerable progress made in the understanding of the genesis of the Muruntau deposit during the last decades;and(3) point to problems still open for future research.Deposit formation occurred through a multi-stage process involving sedimentation,regional metamorphism including thrusting,magmatism with formation of hornfels aureoles and several stages of hydrothermal activity.According to recent knowledge,synsedimentary or pure metamorphic formation of gold mineralization seems unlikely.The role of granite magmatism occurring roughly within the same time interval as the main hydrothermal gold precipitation remains uncertain.There are no signs of interaction of matter between the magma(s) and the hydrothermal system(s).On the other hand,there was an intense,high-temperature(above 400 ℃)fluid- wall rock interaction resulting in the formation of gold-bearing,cone-like stockworks with veins,veinlets and gold-bearing metasomatites.Several chemical and isotope indicators hint at an involvement of lower-crustal or mantle-related sources as well as of surface waters in ore formation.Deposit formation through brecciation involving explosion,hydrothermal or tectonic breccias might explain these data.Further investigations on breccia formation as well as on the exact timing of relevant sedimentary,metamorphic,magmatic and hydrothermal events are recommended. | Ulf Kempe Torsten Graupner Reimar Seltmann Hugo de Boorder Alla Dolgopolova Maarten Zeylmans van Emmichoven | 2016 | Geoscience Frontiers2016，7，3： | 7 |
| 3 | 锡石LA-ICP-MSU-Pb定年在稀有金属矿床研究中的应用显示文摘原生锡矿床具多种类型,如矽卡岩型、云英岩型、石英脉型、斑岩型、花岗岩型、伟晶岩型和喷流沉积型。如何厘定与锡矿有关的花岗岩的结晶时间,目前已经有了较成熟的原位单矿物U-Pb同位素定年方法,用于定年的副矿物通常包括锆石、独居石、榍石、铌钽矿、磷钇矿等。然而。 | 章荣清 孙卫东 Bernd Lehmann Reimar Seltmann 李聪颖 | 2015 | 矿物学报2015，35，S1： | 2 |
| 4 | Multiple sources for mineralizing fluids in the Charmitan gold(-tungsten) mineralization (Uzbekistan)显示文摘 | Torsten Graupner Samuel Niedermann Dieter Rhede Ulf Kempe Reimar Seltmann C. Terry Williams Reiner Klemd | 2010 | Mineralium Deposita2010，，7： | 1 |
| 5 | Geodynamics and metallogeny of the central Eurasian porphyry and related epithermal mineral systems: A review显示文摘 | Reimar Seltmann T. Mike Porter Franco Pirajno | 2013 | Journal of Asian Earth Sciences2013，，： | 1 |
| 6 | Multiple sources for mineralizing fluids in the Charmitan gold(-tungsten) mineralization (Uzbekistan)显示文摘 | Torsten Graupner Samuel Niedermann Dieter Rhede Ulf Kempe Reimar Seltmann C. Terry Williams Reiner Klemd | 2010 | Mineralium Deposita2010，，7： | 1 |
| 7 | Melt inclusions in quartz from an evolved peraluminous pegmatite: Geochemical evidence for strong tin enrichment in fluorine-rich and phosphorus-rich residual liquids显示文摘 | James D. Webster Rainer Thomas Dieter Rhede Hans-Jürgen F?rster Reimar Seltmann | 1997 | Geochimica et Cosmochimica Acta1997，，13： | 1 |
| 8 | Late Paleozoic–Mesozoic tectonic evolution of the Trans-Altai and South Gobi Zones in southern Mongolia based on structural and geochronological data显示文摘 | Alexandra Guy Karel Schulmann Norbert Clauer Pavlina Hasalová Reimar Seltmann Robin Armstrong Ondrej Lexa Antonio Benedicto | 2014 | Gondwana Research2014，，1： | 1 |
| 9 | Hercynian post-collisional A-type granites of the Kokshaal Range,Southern Tien Shah, Kyrgyzstan显示文摘 | Konopelko Dmitry Biske Georgy Seltmann Reimar | 1997 | Lithos1997，2007，： | 1 |
| 10 | Geodynamics and metallogeny of the central Eurasian porphyry and related epithermal mineral systems: A review显示文摘 | Reimar Seltmann T. Mike Porter Franco Pirajno | 2013 | Journal of Asian Earth Sciences2013，，： | 1 |
| 11 | Geochemical evolution of halogen-enriched granite magmas and mineralizing fluids of the Zinnwald tin-tungsten mining district, Erzgebirge, Germany显示文摘 | Jim Webster Rainer Thomas Hans-Jürgen F?rster Reimar Seltmann Christine Tappen | 2004 | Mineralium Deposita2004，，4： | 1 |
| 12 | Re–Os ages for the Shameika porphyry Mo deposit and the Lipovy Log rare metal pegmatite, central Urals, Russia显示文摘 | Jingwen Mao Andao Du Reimar Seltmann Jinjie Yu | 2003 | Mineralium Deposita2003，，2： | 1 |
| 13 | Re–Os ages for the Shameika porphyry Mo deposit and the Lipovy Log rare metal pegmatite, central Urals, Russia显示文摘 | Jingwen Mao Andao Du Reimar Seltmann Jinjie Yu | 2003 | Mineralium Deposita2003，，2： | 1 |
| 14 | Joint Field Workshop of IGCP 473 and IGCP 486显示文摘 | Nigel Cook Reimar Seltmann Rustam Koneev | 2006 | Episodes2006，29，3： | 0 |
| 15 | Interim IAGOD Conference on “Metallogeny of the Pacific Northwest: Tectonics, Magmatism, and Metallogeny of Active Continental Margins”显示文摘 | Dr.Galina A. Gonevchuk Dr. Reimar Seltmann | 2005 | Episodes2005，28，3： | 0 |
| 16 | 12th Quadrennial Symposium of the International Association on the Genesis of Ore Deposits (IAGOD)Moscow, Russia, August 20-24, 2006显示文摘 | Sergei Cherkasov Nigel Cook Reimar Seltmann | 2006 | Episodes2006，29，4： | 0 |
| 17 | The influence of fractionation of REE-enriched minerals on the zircon partition coefficients显示文摘Zircon is widely used to simulate melt generation,migration and evolution within the crust and mantle.The achievable performance of melt modelling generally depends on the availability of reliable trace element partition coefficients(D).However,a large range of D_(REE) values for zircon from natural samples and experimental studies has been reported,with values spanning up to 3 orders of magnitude.Unfortunately,a gap of knowledge on this variability is evident.In this study we model the crystallization processes of common REE-bearing minerals from granitic melts and show that the measured zircon D_(REE) would be elevated if there is crystallization of REE-enriched minerals subsequent to zircon.Nevertheless,compared to zircon D_(REE) values measured from experimental studies,this mechanism appears to have a less significant influence on those from natural granite samples since the quantity of crystallized REE-enriched minerals is very low in natural magmatic systems and/or most of them crystallize prior to zircon.Combined with recently published studies,this work supports that analysis of natural zircon/host groundmass pairs provides more robust D_(REE) values applicable to natural systems than those measured from experimental studies,which can be used to constrain the provenance of detrital zircons. | Shihua Zhong Sanzhong Li Reimar Seltmann Zhiqing Lai Jie Zhou | 2021 | Geoscience Frontiers2021，12，3： | 0 |
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