逆冲推覆构造

  • 网络Thrust faults;thrust nappe;thrust and nappe tectonics
逆冲推覆构造逆冲推覆构造
  1. 进入燕山期,随着桂东南逆冲推覆构造前缘不断地向NW方向扩展,侏罗纪&白垩纪时期的前陆盆地也不断地向NW方向迁移。

    In the Yanshanian period , with continuous NW-directed propagation of the front of the southeastern Guangxi thrust nappe structure , the Jurassic-Cretaceous foreland basin also migrated continuously in a NW direction .

  2. 海南岛西部燕山期逆冲推覆构造特征

    Characteristics of Yanshanian thrust nappe structures in Western Hainan

  3. 结果中卫探区ZW1地震剖面上发育大型的逆冲推覆构造,该逆冲推覆构造形成于晚侏罗世至早白垩世时期。

    Results Large thrust nappe structure was developed along ZW1 seismic survey line , and it was formed during Late Jurassic to Early Cretaceous .

  4. 本文以L14、L55地震大剖面为主,论述了龙门山逆冲推覆构造带北段的结构、模式、形成期、推覆距及油气远景。

    Mainly based on seismic profile L_ ( 14 ) and L_ ( 55 ), the authors discuss the texture , mode , formation time , thrusting distance and oil and gas prospects of the northern sector of thrusting nappe structure of Longmen Mountains .

  5. 闽西南地区东部逆冲推覆构造及其形成机制

    An overthrust tectonic in southwest Fujian and its mechanism of formation

  6. 贵阳市乌当地区逆冲推覆构造的特征分析

    Characteristic analysis of thrust and nappe tectonics in wudang , guiyang

  7. 澜沧地区的逆冲推覆构造研究

    A study on the thrust nappe structure in Lancang region

  8. 试论北京西山煤田逆冲推覆构造样式及成因

    On style of the THRUST-NAPPES in West Hill coal field of Beijing

  9. 羌塘中部后中新世叠瓦式逆冲推覆构造

    Post-Miocene Imbricate Thrust Structures in Middle Qiangtang , Western China

  10. 桐柏山南坡的脆-韧性逆冲推覆构造

    Brittle-ductile thrust nappes on the south slope of Tongbai mountains

  11. 北淮阳地区中生代逆冲推覆构造

    Mesozoic thrust and nappe tectonics in northern Huaiyang region

  12. 燕山板内造山带逆冲推覆构造格局

    The overthrust-nappe tectonic framework of Yanshan intraplate orogenic belt

  13. 秦岭&大别造山带北部中新生代逆冲推覆构造期次及时空迁移规律

    Epochs and space-time migrating of Meso-Cenozoic thrust-nappe tectonics in the North Qinling-Dabie orogen

  14. 下扬子区前陆盆地逆冲推覆构造的研究

    A study on the thrust-nappe strcture of foreland basin in Lower Yangzi Area

  15. 武当隆起与扬子地块接触带逆冲推覆构造的基本特征

    The overthrust nappe structure in the contact zone between Wudang uplift and YANGTZE MASSIF

  16. 江苏南部地区的逆冲推覆构造广泛发育。

    The thrust-nappes exist widely in Southern Jiangsu .

  17. 该地区主要发育两个方向的断裂:北东向的十三陵-下庄逆冲推覆构造等;

    Fault strikes mostly include two direction : northeast faults , e.g.Thirteen Mound-Xiazhuang reverse thrust ;

  18. 粤北新洲地区存在一个中&大型的褶皱式逆冲推覆构造。

    There exists a medium-to-large-scale folded thrust-nappe structure in Xinzhou Area , Northern Guangdong Province .

  19. 汝阳南部逆冲推覆构造的地质特征

    The geological characteristics of thrusting nappe structure in the south of ruyang , henan Province

  20. 井冈山逆冲推覆构造基本特征及找矿意义

    Characteristics of the thrust nappe structrue in Jinggang Mountains and its meaning for ore prospecting

  21. 拉萨地块北部逆冲推覆构造系统

    Thrust System of the North Lhasa Block

  22. 滇西北新生代逆冲推覆构造

    The Cenozoic thrusting nappe in Northwest Yunnan

  23. 华北聚煤区南缘(豫皖)逆冲推覆构造带

    The Thrust and Nappe Tectonics Zone along the Boundary of Coal Accumulation of North China

  24. 造山带逆冲推覆构造研究的主要新进展

    The major progresses in the researches on the thrust and nappe tectonics of orogenic belts

  25. 西南天山柯坪逆冲推覆构造带的地壳缩短分析

    The analysis for crust shortening of Kalpin thrust tectonic zone , south-western tianshan , xinjiang , China

  26. 它们是华力西&印支期板内逆冲推覆构造所形成的断裂变质岩。

    They are fault metamorphic rocks formed in thrusting nappe structure inside continental plate during Variscan-Indonian Stage .

  27. 松树沟逆冲推覆构造研究对恢复蛇绿岩组合层序及其古构造环境具有重要的地质意义。

    Studing the thrust-nappe help us to re-establish the Songshugou ophiolite sequence and its ancient tectonic environment .

  28. 秦岭-大别造山带北部逆冲推覆构造与合肥盆地、周口坳陷控盆断裂

    Overthrust tectonic in northern Qinling Dabie orogenic belt and basin controlling faults in Zhoukou depression and Hefei basin

  29. 北秦岭为一复杂构造带,形成向北反转的叠瓦状逆冲推覆构造。

    The north Qinling is a complicated structural zone , forming an imbricated thrust napped structure overturning northward .

  30. 对玉立群背斜存在与否提出怀疑的意见,并对帕米尔前缘的的逆冲推覆构造样式进行了详细解剖,提出帕米尔山前存在3个相互叠覆推覆体的见解。

    Suggestions are put forward of the existence of three overlapping nappe structures in the piedmont of Pamir .