地震地质 ›› 2017, Vol. 39 ›› Issue (3): 497-516.DOI: 10.3969/j.issn.0253-4967.2017.03.005
刘浪涛, 陈杰, 李涛
收稿日期:
2016-03-25
修回日期:
2016-10-26
出版日期:
2017-06-20
发布日期:
2017-07-20
通讯作者:
陈杰,男,研究员,E-mail:chenjie@ies.ac.cn
作者简介:
刘浪涛,男,1982年生,2016年于中国地震局地质研究所获构造地质学专业博士学位,现为河北工程大学讲师,主要从事构造地质学、沉积学以及碎屑锆石年代学研究,电话:18832010608,E-mail:cumtliulangtao@163.com。
基金资助:
LIU Lang-tao, CHEN Jie, LI Tao
Received:
2016-03-25
Revised:
2016-10-26
Online:
2017-06-20
Published:
2017-07-20
摘要: 现代河流沉积物携带了其物源区丰富的地质信息,通过对现代河流沉积物进行碎屑锆石U-Pb测年,可以了解其物源区地质体中锆石U-Pb年龄的组成。文中对帕米尔、南天山及其会聚带14条主干河流采集的现代河沙样品进行了碎屑锆石U-Pb测年,结合前人在该区域的锆石U-Pb测年结果,确定了帕米尔、南天山不同构造单元的碎屑锆石U-Pb年龄特征;结合区域地质图,揭示了不同年龄峰可能的物源地质体,并推测了一些新的地质体的存在。结果显示,该区域不同构造带具有明显不同的锆石U-Pb年龄峰:南天山构造带的主要年龄峰为270~289Ma和428~449Ma,北帕米尔构造带的主要年龄峰为205~224Ma和448~477Ma,中帕米尔构造带的主要年龄峰为36~40Ma,南帕米尔构造带的主要年龄峰为80~82Ma和102~106Ma。这些年龄峰可以作为识别上述构造单元的特征年龄峰,为利用前陆盆地沉积地层碎屑锆石U-Pb年龄来示踪帕米尔和南天山在新生代的会聚过程提供了基础数据。
中图分类号:
刘浪涛, 陈杰, 李涛. 帕米尔、南天山及其会聚带现代河流沉积物碎屑锆石U-Pb测年[J]. 地震地质, 2017, 39(3): 497-516.
LIU Lang-tao, CHEN Jie, LI Tao. DETRITAL ZIRCON U-PB DATING OF MODERN RIVERS' DEPOSITS IN PAMIR, SOUTH TIAN SHAN AND THEIR CONVERGENCE ZONE[J]. SEISMOLOGY AND GEOLOGY, 2017, 39(3): 497-516.
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