天然气地球科学

• 天然气地质学 • 上一篇    下一篇

柴达木盆地路乐河组粗碎屑沉积成因与青藏高原隆升时限

付玲,关平,简星,刘瑞娟,冯帆,安群,范朝峰   

  1. 1.北京大学地球与空间科学学院,北京 100871;
    2.中国石油测井公司青海事业部,甘肃 敦煌 736202;
    3.中国石油青海油田勘探处,甘肃 敦煌 736202
  • 收稿日期:2012-07-20 修回日期:2012-09-15 出版日期:2012-10-10 发布日期:2012-10-10
  • 通讯作者: 付玲465297887@qq.com E-mail:465297887@qq.com
  • 作者简介:付玲(1989-),女,陕西西安人,博士研究生,主要从事油气地质研究.E-mail:465297887@qq.com.

Sedimentary Genetic Types  of Coarse Fragment of Paleogene Lulehe Formation  in Qaidam Basin and Time Limit of the Tibetan Plateau Uplift

FU Ling, GUAN Ping, JIAN Xing, LIU Rui-juan, FENG Fan, AN Qun, FAN Chao-feng   

  1. 1.School of Earth and Space Sciences,Peking University,Beijing 100871,China;
    2. Qinghai Bussiness Department,Well Logging Corporation of CNPC,Dunhuang 736202,China;
    3. Exploration Department of PetroChina Qinghai Oilfield Company,Dunhuang 736202,China
  • Received:2012-07-20 Revised:2012-09-15 Online:2012-10-10 Published:2012-10-10

摘要:

通过调研野外剖面、钻井岩心、测井及地震等资料,结合分析测试,对古近系路乐河组进行了岩石学、沉积相和测井相方面的综合研究,认为柴达木盆地路乐河组具有显著的山前近源粗碎屑沉积特征,主要发育氧化环境下的典型冲积扇,并往往与下伏中生代地层或古生代基岩呈角度不整合接触,这些沉积特征记录了在白垩纪与新近纪之交柴达木盆地经历的由印度—欧亚板块碰撞而引起的大范围强烈的构造运动。

关键词: 路乐河组, 粗碎屑沉积, 沉积相, 青藏高原隆升, 柴达木盆地

Abstract:

In this study,rock assemblage were interpreted credibly in various aspects,including lithological association,sedimentary facies,well logging and geophysical prospecting,on the basis of outcrops,core drilling and seismic data.The results of Paleogene study in Qaidam basin indicate that the coarse clastic sediments in the lower segment of Lulehe Formation have a nearby source and make typical alluvial fans under the oxidation environment.The Mesozoic strata or Paleozoic rocks are defined by an angular unconformity which is overlain by the segment of Lulehe Formation.Basin comprehensive analysis shows Qaidam basin experienced a large-scale intense tectonic movement at the turn of the Cretaceous and the Paleogene.And the sediment records of Lulehe Formation is the response of the collision between India and Eurasian plates.

 

Key words: Paleogene Lulehe Formation, Coarse clastic rocks, Sedimentary facies, Uplift of the Tibetan Plateau, Qaidam basin

中图分类号: 

  • TE121.3

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