Northern margin of Qaidam Basin,No.5 Lenghu structural,Lower Jurassic,Detrital zircon,U-Pb dating.,"/> 柴达木盆地北缘冷湖五号下侏罗统碎屑锆石U—Pb定年及其地质意义

天然气地球科学

• 天然气地质学 • 上一篇    下一篇

柴达木盆地北缘冷湖五号下侏罗统碎屑锆石U—Pb定年及其地质意义

刘伟明,孙国强,谢梅,项燚伟,郭佳佳,陈波,史基安   

  1. 1.甘肃省油气资源研究重点实验室/中国科学院油气资源研究重点实验室,甘肃 兰州 730000;
    2.中国科学院大学,北京 100049;3.中国石油青海油田公司勘探开发研究院,甘肃 敦煌 736202;
    4.广西高校北部湾石油天然气资源有效利用重点实验室,钦州学院,广西 钦州 535000
  • 收稿日期:2017-07-05 修回日期:2017-08-14 出版日期:2017-09-10 发布日期:2017-09-10
  • 通讯作者: 孙国强(1977-),男,河南洛阳人,副研究员,博士,主要从事含油气盆地石油地质学及沉积构造研究. E-mail:sguoqiang@lzb.ac.cn.
  • 作者简介:刘伟明(1991-),男,江西吉安人,硕士研究生,主要从事含油气盆地地质学研究.E-mail:weimingliu6@163.com.
  • 基金资助:

    中国科学院“西部之光”人才培养计划(编号:Y304RC1SGQ);甘肃省自然科学基金(编号:1308RJZA310);甘肃省重点实验室专项(编号:1309RTSA041);广西中青年教师基础能力提升项目(编号:2017KY0787)联合资助.

The detrital zircon U-Pb dating and its geological significance of the Lower Jurassic in No.5 Lenghu,northern margin of Qaidam Basin

Liu Wei-ming, Sun Guo-qiang, Xie Mei,Xiang Yi-wei, Guo Jia-jia,Chen Bo,Shi Ji-an   

  1. 1.Key Laboratory of Petroleum Resources,Gansu Province/Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences,Lanzhou 730000,China;
    2.University of Chinese Academy of Sciences,Beijing 100049,China;
    3.Research Institute of Exploration and Development,PetroChina Qinghai Oilfield Company,Dunhuang 736202,China;
    4.Guanxi Colleges and Universities Key Laboratory of Beibu Gulf Oil and Natural Gas Resource Effective Utilization,Qinzhou University,Qinzhou 535000,China
  • Received:2017-07-05 Revised:2017-08-14 Online:2017-09-10 Published:2017-09-10

摘要:

碎屑锆石U—Pb年代学拓展了盆地物源分析的途径和方法。为进一步完善柴北缘冷湖五号地区源—汇体系分析,利用冷湖五号LK-1井下侏罗统碎屑锆石样品,讨论了冷湖五号早侏罗世不同时期的物源区空间展布规律。结果显示:冷湖五号早侏罗世物源区主要发育在250~300Ma、400~450Ma 2个年龄区间。碎屑锆石年龄组成表现出早侏罗世早期以400~450Ma为主,后期逐渐演变为250~300Ma和400~450Ma共存的局面。其中,年龄为250~300Ma的碎屑锆石主要来源于小赛什腾山,而400~450Ma的碎屑锆石主要来自赛什腾山西段和阿尔金山东段。此外,碎屑组分特征及重矿物组合特征显示下侏罗统碎屑沉积物具有近源和远源混合沉积的特征。碎屑锆石的年龄分布反映研究区存在早古生代和晚古生代晚期2期区域性构造地质事件,暗示这2期岩浆活动和/或变质作用较为活跃,并为冷湖五号地区提供了主要的锆石来源,导致冷湖五号地区下侏罗统具有多时代混合物源特征。

关键词: 柴北缘, 冷湖五号, 下侏罗统, 碎屑锆石, U—Pb定年

Abstract:

Detrital zircon U-Pb geochronology expended the methods of basin provenance analysis.The provenance distribution in different periods of Early Jurassic and zircon U-Pb geochronology analysis were carried out on the LK-1 borehole of No.5 Lenghu area to improve the study of source to sink system in the northern margin of Qaidam Basin.Results show that the provenance area of No.5 Lenghu develops two main age ranges:250-300Ma and 400-450Ma.The detrital zircon age composition shows that the Early Jurassic was dominated by 400-450Ma,and gradually evolved into the coexistence of 250-300Ma and 400-450Ma in the late stage.Among that,the detrital zircon age of 250-300Ma mainly originated from the Xiaosaishiteng mountains,the age of 400-450Ma mainly came from western Saishiteng mountains and eastern Altyn Tagh mountains.The characteristics of clastic components and heavy mineral assemblages show the mixed sediment features of proximal source and distant source.The Early Jurassic sediments zircon U-Pb age distribution in the No.5 Lenghu area shows that the study area has experienced two-period regional tectonic events:the Early Paleozoic and the Late Paleozoic tectonic events.Those two magmatism and/or metamorphism events are relatively active and provide the majority of zircon for No.5 Lenghu area.The provenance of the Lower Jurassic in No.5 Lenghu area has the characteristics of multi-era and mixed sources.
 

Key words: Northern margin of Qaidam Basin')">

中图分类号: 

  • TE13+.1

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