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北京西山沿河城地区早白垩世火山-沉积盆地的充填过程及构造意义

渠洪杰 王猛 余佳 冯卉 康艳丽 陶涛 宋立才

地质论评2016,Vol.62Issue(6):1403-1418,16.
地质论评2016,Vol.62Issue(6):1403-1418,16.DOI:10.16509/j.georeview.2016.06.004

北京西山沿河城地区早白垩世火山-沉积盆地的充填过程及构造意义

Early Cretaceous Volcano-Sedimentary Basin---Filling Process and Tectonic Implication in Yanhecheng Area,Western Hills of Beijing

渠洪杰 1王猛 2余佳 3冯卉 4康艳丽 4陶涛 4宋立才4

作者信息

  • 1. 北京探矿工程研究所,北京,100083
  • 2. 中国地质科学院地质力学研究所,北京,100081
  • 3. 中国五矿集团公司,北京,100010
  • 4. 中国地质科学院地质力学研究所,北京,100081
  • 折叠

摘要

Abstract

Western Hills of Beijing locates in the intersection part of Taihang and Yanshan tectonic belts, there were a series of Early Cretaceous volcano—sedimentary basins in northwest of Western Hills of Beijing,and preserved a set of volcanic rocks and clastic rocks,named by the Donglingtai formation which can be divided into four sections.Basin fills consist predominantly of alluvial fan,braided river,lacustrine and volcaniclstic deposits. The series of alluvial fan conglomerate were preserved in the lower part of first and second section of Donglingtai formation,respectively.Braided river deposits composed mainly of the upper layers of the second section. Lacustrine facies developed in the Yanhecheng basin,and along two border faults,the Yanhecheng fault and the Hengling—Yanhekou fault.Paleocurrent and gravel composion stastistics indicate that the Proterozoic Wumishan formation northeast of basins provided most deposits at first,after that mainly from the west area of basins,and the same period of volcanic gravels.The pyroclastic rocks of the bottom of first section zircon U-Pb age revealed the initial and inverive time of basin as 140.7Ma and 132.24Ma,respectively.Based on the characteristic of Basin-margin structure,filling process,the normal fault in Donglingtai formation,and evolution of regional geology,the north-east direction of Yanhecheng fault is thought to have played a critical role by left-lateral transtension,and created extensional stress along the southwestern Hengling—Yanhekou fault.The left-lateral transtension during the early stage of early Cretaceous may has played an important role in adjustment from compression to extension in late Mesozoic in eastern of North China.

关键词

北京西山/沉积作用/物源/左行走滑伸展/早白垩世

Key words

Western Hills of Beijing/sedimentary/provenance/left-lateral transtension/Early Cretaceous

引用本文复制引用

渠洪杰,王猛,余佳,冯卉,康艳丽,陶涛,宋立才..北京西山沿河城地区早白垩世火山-沉积盆地的充填过程及构造意义[J].地质论评,2016,62(6):1403-1418,16.

基金项目

本文由国家自然科学青年基金项目(编号41102057)和中国地质调查项目(编号1212011121095)联合资助。AcknowledgementsThis study was financially supported by the NSFC (No.41102057)and CGS (No.1212011121095). ()

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