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| 1 | 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 |
| 2 | A review of major non-sulfide zinc deposits in Iran显示文摘The numerous non-sulfide zinc ore deposits were the historical basis for the development of zinc mining in Iran.They include the Mehdiabad,Irankouh and Angouran world-class deposits,as well as the Zarigan and Haft-har deposits.These deposits were formed by supergene oxidation of primary sulfide minerals during the complex interplay of tectonic uplift,karst development,changes in the level of the water table,and weathering.Zn(Pb)carbonates,Zn-hydrosilicates and associated hydrated phases directly replace the primary ore bodies or fill cavities along fractures related to uplift tectonics.Direct replacement of primary sulfides is accompanied by distal precipitation of zinc non-sulfide minerals in cavities or internal sediments filling.The mineralogy of the non-sulfide mineralization in all six deposits is generally complex and consists of smithsonite,hydrozincite,and hemimorphite as the main economic minerals,accompanied by iron and manganese oxy-hydroxides and residual clays.Commonly,non-sulfide minerals in these deposits consist of two types of ore:red zinc ore(RZO),rich in Zn,Fe,Pb-(As)and white zinc ore(WZO),typically with very high zinc grades but low concentrations of iron and lead.Typical minerals of the RZO are Fe-oxyhydroxides,goethite,hematite,hemimorphite,smithsonite and/or hydrozincite and cerussite.Common minerals of the WZO are smithsonite or hydrozincite and only minor amounts of Fe-oxyhydroxides and hemimorphite. | Sajjad Maghfouri Mohammad Reza Hosseinzadeh Abdorrahman Rajabi Flavien Choulet | 2018 | Geoscience Frontiers2018，9，1： | 2 |
| 3 | From oblique accretion totranspression in the evolution of the Altaid collage: New insightsfrom West Junggar, northwestern China 显示文摘 | Choulet F Faure M Cluzel D | 2012 | Gondwana Research2012，21，23： | 1 |
| 4 | 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 |
| 5 | Structural and functional partitioning of bread wheat chromosome 3B 显示文摘 | CHOULET F ALBERTI A THEIL S | 2014 | Science2014，345，12： | 1 |
| 6 | Late Paleozoic paleogeographic reconstruction of Western Central Asia based upon paleomagnetic data and its geodynamic implications显示文摘 | Choulet F Chen Y Wang B Faure M Cluzel D Charvet J Lin W Xu B | 2011 | J Asian Earth Sci2011，42，5： | 1 |
| 7 | From oblique accretion to transpression in the evolution of the Altaid collage: New insights from West Junggar, northwestern China显示文摘 | Choulet F Faure M Cluzel D | 2012 | Gondwana Research2012，21，23： | 1 |
| 8 | From oblique accretion to transpres- sion in the evolution of the Altaid collage: New insights from West Junggar, northwestern China显示文摘 | CHOULET FLAVIEN FAURE MICHEL CLUZEL DO- MINIQUE | 2012 | Gondwana Research2012，21，23： | 1 |
| 9 | Insertion site based polymorphism markers open new perspectives for genome saturation and marker assisted selection in wheat显示文摘 | PAUX E FAURE S CHOULET F | | 0，，02： | 1 |
| 10 | Le Fresnoy国立当代艺术工作室显示文摘法国Le Fresnoy国立当代艺术工作室的竞赛目标是创造一个能为电影、录像和电子传媒等艺术提供展出、表演和制作场地的跨领域设施。将不同门类的艺术置于同一个项目中是教学层面的一次大胆尝试,目的是在不同领域的交叉地带催生实验与创新。 | bernard tschumi francois gillet mark haukos tom kowalski robert young jim sullivan yannis aesopos douglas gauthier eric liftin robert moric sheri olsen jordan parnass tsuto sakamoto henning ehrhardt jean-francois erhel véronique descharrèires vincent tehvenon paul h.huchard louis choulet | 2016 | 城市环境设计2016，0，1： | 0 |
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