新疆石油地质 ›› 2005, Vol. 26 ›› Issue (4): 373-376.

• 油气勘探 • 上一篇    下一篇

柴达木盆地油砂山油田沉积相

王琳, 贾英兰, 姜义权, 黄振连, 姜明忠   

  1. 中国石油 青海油田分公司勘探开发研究院,甘肃 敦煌736202
  • 收稿日期:2005-01-07 出版日期:2005-08-01 发布日期:2020-11-23
  • 作者简介:王琳(1975-),女,四川内江人,工程师,油藏工程,(Tel)0937-8935472.

Sedimentary] Facies of Y oushashan Oilfield in Qaidam Basin

WANG Lin, JIA Ying-lan, JIANG Yi-quan, HUANG Zhen-lian, JIA NG Ming-zhong   

  1. Research Institute of Exploration and Development, Qinghai Oilfield Company, PetroChina, Dunhuang, Gansu 736202, China
  • Received:2005-01-07 Online:2005-08-01 Published:2020-11-23

摘要: 通过对七个泉地区地质录井和测井曲线资料分析,在下干柴沟组下段识别出2个沉积体系域。体系域主要为湖侵体系域和湖退体系域,其中储集体类型较为丰富,主要为扇三角洲砂体和深湖-伴深湖浊积砂体。将测井层序分析结果和地震储集层预测技术相结合,以体系域进行地震属性分析和沉积相编图,预测在七个泉地区东南部的三角洲前缘和北部的湖底扇砂体能够形成岩性油气藏。

关键词: 柴达木盆地, 油砂山油田, 沉积相

Abstract: The west part of Qaidam basin underwent the lacustrine transgression during E1+2-N11, followed by entering the regression in N21, with large-scale uplfting of Kunlun mountains situated in the southwestern margin of Qaidam basin. Hence the depocenter of lacustrine basin commenced moving from southwest to northeast. Under such a background, Youshashan area was subjected to the deposits of braided stream delta-saucer lake in N1-N12. The XII-I oil measures in Y oushashan oilfield normally assume anticycle deposits shoaling upward. Below VII oil measure (N1) is dominated by braided stream delta front-shore saucer lake deposits; over this oil measure (N12) by braided stream delta plain-front deposits. Laterally, II-V blocks are contolled by the structures in reservoir distribution, with stable sedimentation, while I and VI blocks are mostly influenced by lithogical factors.

Key words: Qaidam basin, Youshashan oilfield, sedimentary facies

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