新疆石油地质 ›› 1993, Vol. 14 ›› Issue (4): 323-331.

• 地层与沉积 • 上一篇    下一篇

西准噶尔界山前陆盆地晚期(T 一J)层序地层与油气勘探

赵玉光, 丘东洲, 张继庆   

  1. 研究生 中国地科院成都地矿所 四川成都 610082
  • 发布日期:2020-12-08

SEQUENCE STRATIGR A PHY OF THE LATE FORELAND BASIN (T-J) IN THE WEST JUNGGAR BOUNDARY MOUNTA INS AND PETROL EUM EXPLORATION

Zhao Yuguang, Qiu Dongzhou, Zhang Jiqing   

  1. Gradate Student, Chengdr Geology and Minerals Institade,Chinese Academy of Geologioal Sciences, Chengdu, Sichuan 610082
  • Published:2020-12-08

摘要: 提出了西准噶尔界山前陆盆地发育晚期(T-J)的层序地层学模式及油气勘探预测模型。在同生断裂边缘以湖水与界面断裂的交线为“陆架边角”,克乌断裂带附近为“坡折带”。各体系域所含沉积体系与海相模式不尽相同,Ⅰ型层序体系域构成齐全,Ⅰ型层序缺少低位体系域,Ⅰ 型界面之上直接夜盖湖进体系域, 反映了湖盆基准面升降频度。三叠一侏罗系可划分为3个层序和4 个准层序, 富砂的高位体系域“扇三角洲一浊积扇” 等一系列储集层是今后勘探开发的重要对象。

关键词: 西准噶尔界山, 前陆盆地, 层序地层学

Abstract: In this work, we proposed the sequence stratigraphy model of the late foreland basin (T一J) in the west Junggar boundary mountains and the prediction model of oil and gas exploration. At the edge of growth fault, the crossline of lake water and boundary fault was the edge angle of continental shelf, Major Karamay-Urho faulting zone was the folding slope zone. The depositional systems in each system tract were not all the same as matine patterns. Type Ⅰ sequence system tract included alI the composition,type Ⅱ sequence was lack of low level system tract. Type Ⅱ boundary surface was covered directly with transgtesive system tract and reflected the eustatic frequency of lacustrine level change. riassic-Jurassic was divided into 3 sequences and 4 quasi-sequences, and fan delta-tu:bidite fan and other series of reservoirs in high level system tract which was rich in and were pointed to be important targets in the future oil exploration and development.

Key words: West Junggar boundary mountains, I Foreland basin, Sequence stratigraphy