塔里木北缘前寒武基底隆升剥露史:来自磷灰石裂变径迹的证据

朱文斌 张志勇 舒良树 万景林 卢华复 王胜利 杨伟 苏金宝. 塔里木北缘前寒武基底隆升剥露史:来自磷灰石裂变径迹的证据[J]. 岩石学报, 2007, 23(7): 1671-1682.
引用本文: 朱文斌 张志勇 舒良树 万景林 卢华复 王胜利 杨伟 苏金宝. 塔里木北缘前寒武基底隆升剥露史:来自磷灰石裂变径迹的证据[J]. 岩石学报, 2007, 23(7): 1671-1682.
ZHU WenBin, ZHANG ZhiYong, SHU LiangShu, WAN JingLin , LU HuaFu , WANG ShengLi , YANG Wei,SU JinBao. Uplift and exhumation history of the Precambrian basement, Northern Tarim: Evidence from apatite fission track data[J]. Acta Petrologica Sinica, 2007, 23(7): 1671-1682.
Citation: ZHU WenBin, ZHANG ZhiYong, SHU LiangShu, WAN JingLin , LU HuaFu , WANG ShengLi , YANG Wei,SU JinBao. Uplift and exhumation history of the Precambrian basement, Northern Tarim: Evidence from apatite fission track data[J]. Acta Petrologica Sinica, 2007, 23(7): 1671-1682.

塔里木北缘前寒武基底隆升剥露史:来自磷灰石裂变径迹的证据

  • 基金项目:

    国家重点基础研究发展规划项目(2007CB411301),国家自然科学基金项目(40573038,40472112)和地震动力学国家重点实验室开放基金项目(No.LED0507)合作资助的研究成果.

Uplift and exhumation history of the Precambrian basement, Northern Tarim: Evidence from apatite fission track data

  • 库鲁克塔格隆起位于塔里木盆地北缘,广泛出露前寒武基底岩石。辛格尔村附近出露的太古宙杂岩,包括灰色片麻岩、角闪岩、片岩、混合岩和大理岩。新元古代地层出露在库鲁克塔格隆起西部的兴地、西山口、辛格尔和杀马山附近,不整合在古元古代和中元古代的片麻岩、角闪岩和片岩之上,并被早古生代的地层不整合。因此,该地区是了解塔里木盆地前寒武基底热演化史的理想地区。本研究的目的是为了探索:①塔里木基底岩石最初于何时剥露于地表?②塔里木基底剥露以后是否经历过再次埋藏和剥露?③塔里木基底岩石构造热演化过程对大陆边缘不同构造事件的响应。为了获取塔里木北缘剥露史和冷却过程信息,我们开展了裂变经迹的研究。含磷灰石的样品采自库鲁克塔格隆起的兴地断裂两侧。样品池年龄介于146.0±13.4和67.6±6.7Ma之间,平均经迹长度介于.11.79±0.14和13.89±0.27μm之间。根据样品年龄和样品所处的构造位置,样品可以分为3组。A组样品包括F2、F3、F4、F5和F8,裂变经迹表观年龄约100~110Ma,通常位于未遭断层变形的地区。B组样品包括F7、D和F10,裂变经迹表观年龄小于80Ma,构造上位于断层上盘并靠近断层。c组样品F11具有最大的裂变经迹表观年龄146.0±13.4Ma。热模拟表明,库鲁克塔格地区的隆升剥露作用可以划分为四期,分别是早侏罗世晚期(180Ma)、晚侏罗世-早白垩世(144~118Ma)、晚白垩世早期(94~82Ma)和新生代晚期(约10Ma)。裂变经迹记录的库鲁克塔格多阶段隆升作用,是对亚洲南缘多期地体碰撞增生的响应。
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修回日期:  2007-03-22
刊出日期:  2007-07-31

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