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| 1 | Polyorogenic evolution of the Paleoproterozoic Trans-North China Belt--New insights from the Luliangshan-Hengshan-Wutaishan and Fuping massifs显示文摘 | Michel Faure Pierre Trap Wei Line Patrick Monié Olivier Bruguier | 2007 | Episodes2007，30，2： | 63 |
| 2 | Palaeozoic tectonic evolution of the Tianshan belt,NW China显示文摘The Chinese Tianshan belt is a major part of the southern Central Asian Orogenic Belt,extending westward to Kyrgyzstan and Kazakhstan.Its Paleozoic tectonic evolution,crucial for understanding the amalgamation of Central Asia,comprises two stages of subduction-collision.The first collisional stage built the Eo-Tianshan Mountains,before a Visean unconformity,in which all structures are verging north.It implied a southward subduction of the Central Tianshan Ocean beneath the Tarim active margin,that induced the Ordovician-Early Devonian Central Tianshan arc,to the south of which the South Tianshan back-arc basin opened.During the Late Devonian,the closure of this ocean led to a collision between Central Tianshan arc and the Kazakhstan-Yili-North Tianshan Block,and subsequently closure of the South Tianhan back-arc basin,producing two suture zones,namely the Central Tianshan and South Tianshan suture zones where ophiolitic mélanges and HP metamorphic rocks were emplaced northward.The second stage included the Late Devonian-Carboniferous southward subduction of North Tianshan Ocean beneath the Eo-Tianshan active margin,underlined by the Yili-North Tianshan arc,leading to the collision between the Kazakhstan-Yili-NTS plate and an inferred Junggar Block at Late Carboniferous-Early Permian time.The North Tianshan Suture Zone underlines likely the last oceanic closure of Central Asia Orogenic Belt;all the oceanic domains were consumed before the Middle Permian.The amalgamated units were affected by a Permian major wrenching,dextral in the Tianshan.The correlation with the Kazakh and Kyrgyz Tianshan is clarified.The Kyrgyz South Tianshan is equivalent to the whole part of Chinese Tianshan(CTS and STS) located to the south of Narat Fault and Main Tianshan Shear Zone;the so-called Middle Tianshan thins out toward the east.The South Tianshan Suture of Kyrgyzstan correlates with the Central Tianshan Suture of Chinese Tianshan.The evolution of this southern domain remains similar from east(Gangou area) to west until the Talas-Ferghana Fault,which reflects the convergence history between the Kazakhstan and Tarim blocks. | Jacques CHARVET SHU LiangShu Sebastien LAURENT-CHARVET WANG Bo Michel FAURE Dominique CLUZEL CHEN Yan Koen De JONG | 2011 | Science China Earth Sciences2011，54，2： | 57 |
| 3 | SHRIMP zircon U-Pb age, fitho- and biostratigraphic analyses of the Huaiyu Domain in South China,— Evidence for a Neoproterozoic orogen, not Late Paleozoic-Early Mesozoic collision显示文摘 | Liangshu Shu Michel Faure Shaoyong Jiang Qun Yang Yujing Wang | 2006 | Episodes2006，29，4： | 47 |
| 4 | 大别山的构造变形期次和超高压岩石折返的动力学显示文摘从构造关系上看,大别山可分为南部,中部和北部3个构造系统。大别山南部构造系统为一套(原地)构造堆叠系统(相对的),从上到下依次为:①未变质的震旦纪—早三叠世沉积盖层,它被造山后的侏罗—白垩纪砂-砾岩不整合覆盖;②弱变质的新元古代板岩;③高压变质岩系(宿松群),这些变质岩系大多退变质为绿片岩相;④含柯石英榴辉岩超高压变质单元的异地系统;⑤未经历超高压变质作用的原地(相对的)片麻岩系。北西-南东向的拉伸线理在各个地质单元均有表现。从动力学上看,上盘指向NW的剪切运动被后期的褶皱所改变。大别山中部为(混合岩)热穹窿改造系统,系经历了超高压变质作用的地体叠加了混合岩化作用的产物,它与超高压变质地体的界限为一拆离断层,而正是这个拆离断层使超高压变质地体向地表折返并经历了角闪岩相的退变质作用。大别山北部为构造堆叠系统,早期的面理和南北向的挤压线理被轴面北倾的褶皱所改造,这种褶皱对应于大别山中部同折返期的韧性变形的隆升构造。同时建立了地球动力学模型并讨论了逆冲作用和正断层的作用。 | 林伟 王清晨 Michel Faure 孙岩 舒良树 Urs Scharer | 2003 | 地质学报2003，77，1： | 42 |
| 5 | 伊犁北部博罗霍努岩体年代学和地球化学研究及其大地构造意义显示文摘博罗霍努岩体是发育在新疆伊犁北部的一个大型海西期花岗岩体,总体沿近 SE—NW 向分布,出露面积逾2000km^2。该岩体主要包括三类花岗岩:灰黑色辉石闪长岩、浅色黑云母花岗岩和紫红色黑云母钾长花岗岩。锆石 U—Pb La-ICP-MS 定年表明,辉石闪长岩的年龄为301±7Ma,黑云母花岗岩的年龄范围为294±7~285±7Ma,而黑云母钾长花岗岩则形成于280±5~266±6Ma。岩石地球化学分析显示,黑云母花岗岩和钾长花岗岩以准铝或弱过铝Ⅰ型花岗岩为主,个别属于弱过铝 S 型花岗岩。在微量元素方面,这些花岗岩均富集轻稀土而亏损重稀土,但来自两个剖面的花岗岩具有不同的稀土元素配分模式,可能代表它们的岩浆源区有所不同,因此需要进一步对这些花岗岩进行同位素地质学研究。相对于洋脊花岗岩而言,博罗霍努岩体的花岗岩明显富集 K,Rb,Ba 和 Th,同时,显著亏损 Nb,Ta,Y 和 Yh。以上地球化学特征及微量元素判别图表明,这些花岗岩类形成于俯冲有关的火山岛弧环境。结合伊犁及邻区岩浆岩的特征及其时代,可以认为博罗霍努岩体的形成与天山北部洋壳向南的俯冲造山作用有关。西天山北部俯冲造山作用最终在中二叠世结束,并在中一晚二叠世进入陆内造山和伸展拉张阶段。 | 王博 舒良树 Dominique CLUZEL Michel FAURE Jacques CHARVET | 2007 | 岩石学报2007，23，8： | 40 |
| 6 | 科克苏-穹库什太古生代构造-岩浆作用及其对西南天山造山时代的约束显示文摘天山造山带是古生代多期碰撞增生作用的产物,其确切的造山时代是当前争议较多的热点问题。分布在西南天山的科克苏-穹库什太剖面经历了复杂的构造变形,最明显的两期变形事件分别为朝北的推覆作用和 NE-SW 韧性走滑作用。本剖面可分为伊犁岩浆岛弧、伊犁结晶基底、高压变质杂岩三个岩石-构造单元。野外可见黑云母花岗闪长岩侵入到绿片岩相变质岩中,岩脉切穿绿片岩中面理构造。通过锆石 U-Pb LA-ICPMS 测年,科克苏剖面钾长花岗岩的年龄为341±6Ma 和338±8Ma,穹库什太黑云母花岗闪长岩的年龄为313±4Ma。其中,花岗闪长岩发生了黑云母定向排列,通过对黑云母进行^(40)Ar/^(39)Ar 测年,获得坪年龄为263.4±0.6Ma,表明该花岗闪长岩受过后期热事件的干扰。地球化学分析表明,黑云母花岗闪长岩属于钙碱性系列,Nb 和 Ta 含量低而 Rb,Ba 和 Th 含量很高,与俯冲作用有关的岛弧岩浆岩地球化学组成非常相似。结合前人对该地区高压变质岩、花岗岩和火山岩的研究成果,本文提出,西南天山俯冲-碰撞造山作用发生在晚石炭世之前,研究区后碰撞区域走滑作用标志着西南天山碰撞造山作用在二叠纪之前全部结束。 | 王博 舒良树 MichelFAURE DominiqueCLUZEL JacquesCHARVET Michel FAURE Dominique CLUZEL Jacques CHARVET | 2007 | 岩石学报2007，23，6： | 25 |
| 7 | 越南东北部早中生代构造事件的年代学约束显示文摘越南东北部-海南岛-粤西南构造带整体上呈NW-SE走向展布于华南板块的南缘,是理解华南构造演化的关键地区。作为印支运动代表性地区的越南东北部地区Song Chay构造带上,下古生界浅变质沉积岩、上古生界至早-中三叠世未变质的沉积盖层中都发育向北东逆冲推覆,韧性变形域表现为NE-SW向的矿物拉伸线理和上部指NE的剪切变形,而脆性变形域则记录了大量NE极性的褶皱和冲断构造。两广交界的云开地体和海南岛地区存在着相同样式的构造变形。关于这期变形的时间,本文通过对野外地层以及所出露不同时期岩体变形特征的综合研究,并结合高质量的锆石U-Pb年代学数据,在越南的东北部厘定为237~228Ma。这期广泛分布于华南板块南缘构造事件的动力学机制同Day Nui Con Voi(大象山)微陆块与华南板块在早中生代的构造拼合事件相关。本文认为华南板块在早三叠世开始沿着越南东北部的Song Chay缝合带俯冲拼合于Day Nui Con Voi微陆块之下,因此在早-中三叠世时期,在作为俯冲盘的华南板块南缘发育一系列的褶皱和逆冲推覆构造,晚三叠世印支造山作用结束。因此,华南板块南缘的越南东北部-海南岛-粤西南构造带被一同卷入早-中三叠世同印支板块的碰撞造山体系之中。 | 陈泽超 林伟 Michel FAURE Claude LEPVRIER 褚杨 王清晨 | 2013 | 岩石学报2013，29，5： | 23 |
| 8 | 华南板块早中生代陆内造山过程--以雪峰山-九岭为例显示文摘雪峰山-九岭造山带位于华南板块的中心区域,是一条典型的陆内造山带。通过详细的野外地质观察,雪峰山在早中生代经历了3期构造变形:D1为上部指向NW的韧性剪切,D2代表了一期反向褶皱-逆冲构造事件,以及D3期的水平挤压形成的直立的褶皱、劈理和线理。而在九岭,早中生代大规模脆-韧性域构造变形叠加在早古生代韧性变形之上,形成了一系列极性NW逆冲断层和不对称褶皱。雪峰山-九岭陆内造山带形成于早中生代,造山作用可以分为两个阶段,即245~225Ma的挤压变形阶段和225~215Ma的垮塌-岩浆侵位阶段。雪峰山-九岭造山带的构造特点表明,华南板块东南缘古太平洋板块向北西方向的俯冲可能引发了早中生代的陆内造山过程。 | 褚杨 林伟 FAURE Michel 王清晨 | 2015 | 岩石学报2015，31，8： | 22 |
| 9 | 胶东半岛中生代构造演化的几何学和运动学显示文摘据岩石的变质相及变形特征可把胶东半岛分为 5个地质单元 ,其构造几何关系由高至低为 :1 )板岩—砂岩单元 ;2 )高压片麻岩—石英岩单元 ;3)大理岩—角闪岩单元 ;4)超高压变质单元 ,它经历了超过 1 5 0km的深俯冲作用并快速折返至地表 ;5 )片理化的混合岩穹隆单元 ,其为超高压变质单元叠加了混合岩化作用。这些构造单元均经历了相同的变形 ,具有NW指向的剪切特征。对比大别山构造学的研究结果 ,这种变形特征代表了超高压变质地体在折返过程中的运动学表现。混合岩穹隆中所残余含柯石英榴辉岩表明了胶东半岛和苏鲁地区具有相同的构造演化过程 ,烟台—青岛—五莲断裂不是华南板块与华北板块间的缝合带。 | 林伟 Michel Faure 王清晨 | 2003 | 地质科学2003，38，4： | 22 |
| 10 | 华南板块南缘早中生代的逆冲推覆构造及其相关的动力学背景显示文摘作为理解华南构造演化的关键地区,在华南板块南缘的云开地体和越北的Song Chay地体发育了早中生代的向北东逆冲推覆的韧性变形。在云开地体,经历角闪岩相和绿片岩相变质的矿物指示了产状平缓的面理上发育明显的北东—南西向矿物拉伸线理。沿着这些矿物拉伸线理,具有上部指向北东的剪切变形。同位素年代学的定年结果指示了变形事件发生在220 Ma左右。在越南北部,Song Chay地体的岩石和构造特征与云开地体极其相似:平缓的面理,北东—南西向的矿物拉伸线理和上部指向北东的剪切变形是其主要的构造特征,这些构造特征均表现为向北东的逆冲推覆,变形时间从晚三叠世至早侏罗世。这期构造事件的动力学机制被认为同印支板块与华南板块晚古生代—早中生代的构造拼合密切相关。我们认为新发现的Song Chay蛇绿混杂带是华南板块同印支板块的碰撞拼合界线。因此,华南板块南缘云开地体和Song Chay地体被一同卷入同印支板块的碰撞造山体系之中。 | 林伟 Michel Faure Claude Lepvrier 陈泽超 褚杨 王清晨 N'guyen Van Vuong Vu Van Tich | 2011 | 地质科学2011，46，1： | 20 |
| 11 | 雪峰山早中生代构造演化:构造学和年代学分析显示文摘雪峰山主体地处湖南省境内,位于华南板块的中心区域,是一条典型的陆内造山带。通过详细的野外地质观察,我们将其分为3个构造单元:西部外区,主要以大型箱状褶皱为主;中部区,与西部区以主逆冲断层相分隔,劈理发育呈扇状,是雪峰山构造带的核心区域,也是变质级别最深、变形最强的区域;东部区,变形集中在脆韧性区域之上,以极性北西构造为主,并有反向构造发育。研究区经历了3期构造变形:D_1为上部指向北西的韧性剪切,广泛发育于整个区域;D_2代表了一期反向褶皱—逆冲构造事件;D_3则以水平挤压为主,形成了直立的褶皱、劈理和线理。雪峰山的构造演化表明华南板块东南缘古太平洋板块向北西方向的俯冲可能引发了早中生代的陆内俯冲造山过程。 | 褚杨 林伟 Michel Faure 王清晨 | 2011 | 地质科学2011，46，1： | 7 |
| 12 | Toward a unified model of Altaids geodynamics:Insight from the Palaeozoic polycyclic evolution of West Junggar(NW China)显示文摘The Altaid tectonic collage extends over Central Asia, exposing numerous accretionary orogens that can account for the Palaeozoic continental crust growth. A pluridisciplinary approach, using geochronological, geochemical, structural and palaeomagnetic tools was carried out to unravel the architecture and the evolution of West Junggar(Northwestern China), a segment of the Altaid Collage. A polycyclic geodynamic evolution is inferred and includes:(1) an Early Palaeozoic cycle, characterized by the closure of two oceanic basins bounded by island-arc systems;(2) an Early Devonian subduction jamming resulting in a minor-scale collision documented by thrusting, syntectonic sedimentation and subsequent crutal thinning associated with alkaline magmatism;(3) a Late Palaeozoic cycle, driven by the evolution of two opposite subduction zones developed upon the Early Palaeozoic basement. Detailed structural analysis and paleomagnetic data provide constraints for the late evolution of Junggar in the frame of the development of the Late Palaeozoic Kazakh orocline, which led to oblique subduction and transpression in the West Junggar accretionary complex. Progressive buckling of the Kazakh orocline further resulted in Late Carboniferous to Permian wrench tectonics, and lateral displacement of lithotectonic units. Block rotations that continued after the Late Triassic are due to diachronous intraplate reactivation. This scenario mirrors the Palaeozoic geodynamics of the Altaid Collage. Multiple Early Palaeozoic collisions of intra-oceanic arcs and micro continents have contributed to the formation of the Kazakhstan Microcontinent. Since the Late Palaeozoic, subductions formed around this microcontinent and the final oblique closure of oceanic domains resulted in the transcurrent collage of Tarim and Siberia cratons. Palaeozoic strike-slip faults were later reactivated during Mesozoic intracontinental tectonics. | Flavien CHOULET Michel FAURE Dominique CLUZEL CHEN Yan LIN Wei WANG Bo XU Bei | 2016 | Science China Earth Sciences2016，59，1： | 6 |
| 13 | Application of thermodesorption and pyrolysis-GC-AED to the analysis of river sediments and sewage sludges for environmental putpose显示文摘 | Faure P Vilmin F Michels R | 2002 | J Anal Appl Pyrolysis2002，62，2： | 1 |
| 14 | The building of south China: collision of Yangzi and Cathaysia blocks, problems and tentative answers显示文摘 | Jacques Charvet Liangshu Shu Yangshen Shi Lingzhi Guo Michel Faure | 1996 | Journal of Southeast Asian Earth Sciences1996，，3： | 1 |
| 15 | Structural development of the Lower Paleozoic belt of South China: Genesis of an intracontinental orogen显示文摘 | Jacques Charvet Liangshu Shu Michel Faure Flavien Choulet Bo Wang Huafu Lu Nicole Le Breton | 2010 | Journal of Asian Earth Sciences2010，，4： | 1 |
| 16 | Paleozoic tectonics of the southern Chinese Tianshan: Insights from structural, chronological and geochemical studies of the Heiyingshan ophiolitic mélange (NW China)显示文摘 | Bo Wang Liangshu Shu Michel Faure Bor-ming Jahn Dominique Cluzel Jacques Charvet Sun-lin Chung Sébastien Meffre | 2010 | Tectonophysics2010，，1： | 1 |
| 17 | Application of thermodesorption and pyrolysis-GC-AED to the analysis of river sediments and sewage sludges for environmental purpose显示文摘 | Faure P Vilmin F Michels R | 2002 | Journal of Analytical and Applied Pyrolysis2002，62，2： | 1 |
| 18 | Syndrome de Rapunzel associé à une intussusception du grêle, une dilatation des voies biliaires et une pancréatite显示文摘 | Bruno Godart Marc Wangermez Carole Doucet Jean-Pierre Faure Michel Beauchant | 2006 | Gastroenterologie Clinique et Biologique2006，，11： | 1 |
| 19 | Evolution of calc-alkaline to alkaline magmatism through Carboniferous convergence to Permian transcurrent tectonics, western Chinese Tianshan显示文摘 | Bo Wang Dominique Cluzel Liangshu Shu Michel Faure Jacques Charvet Yan Chen Sebastien Meffre Koen Jong | 2009 | International Journal of Earth Sciences2009，，6： | 1 |
| 20 | Intracontinental subduction: a possible mechanism for the Early Palaeozoic Orogen of SE China显示文摘 | Michel Faure Liangshu Shu Bo Wang | 2009 | Terra Nova2009，21，5： | 1 |
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