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东秦岭商丹地区武关岩群斜长角闪片岩LA-ICP-MS锆石UPb年龄及其地质意义

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高峰, 裴先治, 李瑞保, 李佐臣, 裴磊, 刘成军, 陈有炘, 王盟, 李宗耀. 东秦岭商丹地区武关岩群斜长角闪片岩LA-ICP-MS锆石UPb年龄及其地质意义[J]. 西北地质, 2017, 50(1): 198-211.
引用本文: 高峰, 裴先治, 李瑞保, 李佐臣, 裴磊, 刘成军, 陈有炘, 王盟, 李宗耀. 东秦岭商丹地区武关岩群斜长角闪片岩LA-ICP-MS锆石UPb年龄及其地质意义[J]. 西北地质, 2017, 50(1): 198-211.
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GAO Feng, PEI Xianzhi, LI Ruibao, LI Zuocheng, PEI Lei, LIU Chengjun, CHEN Youxin, WANG Meng, LI Zongyao. LA-ICP-MS Zircon U-Pb Ages of the Plagioclase-Amphibole Schist from the Wuguan Group in Shangdan Area, East Qingling, and Its Geological Significance[J]. Northwestern Geology, 2017, 50(1): 198-211.
Citation: GAO Feng, PEI Xianzhi, LI Ruibao, LI Zuocheng, PEI Lei, LIU Chengjun, CHEN Youxin, WANG Meng, LI Zongyao. LA-ICP-MS Zircon U-Pb Ages of the Plagioclase-Amphibole Schist from the Wuguan Group in Shangdan Area, East Qingling, and Its Geological Significance[J]. Northwestern Geology, 2017, 50(1): 198-211.
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东秦岭商丹地区武关岩群斜长角闪片岩LA-ICP-MS锆石UPb年龄及其地质意义

  • 1.

    长安大学地球科学与资源学院, 陕西 西安 710054

  • 2.

    长安大学地球科学与资源学院, 陕西 西安 710054;国土资源部岩浆作用成矿与找矿重点实验室, 陕西 西安 710054

  • 3.

    中国地质大学地球科学与资源学院, 北京 100083

  • 基金项目: 国家自然科学基金项目“东昆仑东段晚古生代-早中生代构造演化与造山过程研究”（41472191），“东昆仑东段东昆中蛇绿岩年代学及构造属性研究”（41502191），“东昆仑南缘布青山构造混杂岩带的组成、结构与构造演化过程”（41172186），“西秦岭北缘变形构造解析及其祁连-秦岭构造交接关系研究”（40972136），“扬子地块西北缘后龙门东段变质核杂岩形成机制和区域构造背景”（40572121）

LA-ICP-MS Zircon U-Pb Ages of the Plagioclase-Amphibole Schist from the Wuguan Group in Shangdan Area, East Qingling, and Its Geological Significance

  • 1.

    School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China

  • 2.

    School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China;Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR, Xi'an 710054, Shaanxi, China

  • 3.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

    摘要
  • 东秦岭商丹地区武关岩群鮸鱼咀斜长角闪岩单元中的斜长角闪片岩缺乏较为精确的年代学资料，制约着对武关岩群形成时代及其构造属性的认识。利用LA-ICP-MS锆石U-Pb同位素测年技术对武关岩群中斜长角闪片岩进行锆石U-Pb年龄测定，所得年龄数据显示出大致5组年龄，分别为~2.45Ga，~1.7~2.0Ga，~0.95Ga~0.85Ga，~0.71~0.74Ga，除年龄值最新的一组锆石外，其余锆石均属于斜长角闪片岩的原岩岩浆在上升过程中捕获自地壳物质的继承锆石，记录了南秦岭地区基底增长的过程。据此认为斜长角闪片岩的原岩（玄武岩）的形成时代应为~730Ma，与新元古代中晚期Rodinia超大陆的裂解有关。
    There lacks accurate chronology information about the plagioclase-amphibole schist from the Wuguan Group of Mianyuzhui Unit in Shangdan area, East Qinling, which cause the formation age and tectonic attributes of Wuguan Group cannot to be understand. The LA-ICP-MS U-Pb dating on the zircons from the plagioclase-amphibole schist yield four age clusters of~2.45Ga,~1.7~2.0Ga,~0.95Ga,~0.85Ga. Except for the youngest one group of zircon ages, the others indicate that these zircons were inherited from the crustal materials during the ascending of basaltic magma, which were sourced from the protolith magma of plagioclase-amphibole schist and recorded the growth process of South Qinling. This result suggests that the crystal age of plagioclase-amphibole schist's protolith is~730Ma, corresponding to the break-up of the Rodinia supercontinent in Middle-LateNeoproterozoic.
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收稿日期:  2016-10-01
修回日期:  2016-11-28
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