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东疆与邻区的板块构造及其演化 被引量:10

PLATE TECTONICS AND ITS EVOLUTION OF EASTERN XINJIANG AND ADJACENT AREAS
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摘要 显生宙初,新疆曾是一个统一的陆块。寒武纪晚期开始解体,在新疆东、北部形成斋桑-东准噶尔、康古尔两个洋盆,博格达-哈尔力克、北山两个裂谷系和12条深、大断裂带。从加里东中晚期开始,两个洋盆边拉张达消减,形成3条俯冲带、2个对接带和7个岛弧带,最后于华力西中期沿克拉表里、康古尔塔格两个对接带闭合。以对接带、俯冲带和深断裂带为界,将东疆及其邻区划分为西伯利亚、准噶尔和塔里木三大板块,10个次级构造单元。华力西晚期两个裂谷闭合后,中上部地壳强烈水平挤压,产生一系列逆冲-推覆构造等碰撞期后极内构造效应。 The continental block of Xinjiang and its adjacent areas was broken up in the late Cambriantime.Zaisan-east Junggar and Kangguer OCeanic basins, Bogda-Harlik and North Mount riftS,andtwelve deep fault 'zones were formed in the north and east Xinjiang. Since the middle and late Caledonian, the two basins beg3n opening and closins,and three subduction zones, two collision zones andseven island arc belts were formed. At last, the two collision zones were closed up along Karameili andKangguertag in middle Variscan. The eastern Xinjiang and its adjacent areas were divided into three paleoplates and ten secondary tectonic elementS, bounded by the colliSion zones, subduction zones anddeep fault zones. After the closins of the two riftS in the late Variscan,the crust was compressed strongly and the tectonic effect within the plate occurred after a series of thrust-nappe structures collided.
作者 张朝文
出处 《成都理工学院学报》 CSCD 1994年第4期1-10,共10页 Journal of Chengdu University of Technology
关键词 板块构造 陆块 洋盆 构造演化 新疆 continental block, oceanic basin, rift, subduction zone, collision zone, island arc belt,plate, thrust-nappe structure
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参考文献4

  • 1张朝文,刘援朝,魏显贵.阿尔泰地区韧性剪切带和推覆-滑脱构造[J].成都地质学院学报,1992,19(1):1-7. 被引量:19
  • 2成守德,王广瑞,杨树德,靳金生,祝皆水.新疆古板块构造[J]新疆地质,1986(02).
  • 3刘峰标.阿勒泰古板块与内生矿产[J]西北地质,1983(04).
  • 4黄汲清指导任纪舜等执笔中国大地构造及其演化[M].

二级参考文献2

  • 1张朝文.板块碰撞前后:俯冲向仰冲之转化[J]成都地质学院学报,1985(04).
  • 2马杏垣,索书田.论滑覆及岩石圈内多层次滑脱构造[J]地质学报,1984(03).

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