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潜江凹陷东部地区新沟咀组下段浅水三角洲沉积模式

胡忠贵 胡明毅 胡九珍 刘冬梅

中国地质2011,Vol.38Issue(5):1263-1273,11.
中国地质2011,Vol.38Issue(5):1263-1273,11.

潜江凹陷东部地区新沟咀组下段浅水三角洲沉积模式

Shallow water delta depositional model of the lower segment of the Xingouzui Formation in eastern Qianjiang depression

胡忠贵 1胡明毅 2胡九珍 1刘冬梅2

作者信息

  • 1. 长江大学油气资源与勘探技术教育部重点实验室,湖北荆州434023
  • 2. 长江大学地球科学学院,湖北荆州434023
  • 折叠

摘要

Abstract

The lower segment of the Xingouzui Formation in eastern Qianjiang depression is an important horizon for finding lithologic hydrocarbon reservoir in the future. Based on a synthetic analysis of core description as well as thin section and logging data in combination with sedimentary marks of lithology.paleoclimate, sedimentary structure,and the depositional background of weak tectonic movement and flattened palaeotopography.the authors hold that the lower segment of the Xingouzui Formation is of a shallow water delta depositional system. The shallow water delta has the following characteristics: ①there exist well-developed underwater distributary channel microfacies, underdeveloped mouth bar,extensive sand sheet,and frequently alternate pre-delta and front deposition; ②various fades belts are smoothly connected with each other without apparent slope gradient; ③depositional model has no three-layer structures like "Gilber delta". During the depositional evolution,the shallow water delta deposition was affected by such factors as palaeoclimate,density contrast of stream and salt lake, fluviatile action and lake surface fluctuation., and the shape and the development extent of the underwater distributary channel were especially apparently controlled by these factors, forming strong or weak reformed front sand. Favorable allocation for generating reservoirs and cap rocks in the lower segment of the Xingouzui Formation was favorable for forming lithologic hydrocarbon reservoirs.

关键词

潜江凹陷东部/新沟咀组下段/浅水三角洲/沉积模式

Key words

eastern Qianjiang depression/lower segment of Xingouzui Formation/shallow water delta/depositional model

分类

天文与地球科学

引用本文复制引用

胡忠贵,胡明毅,胡九珍,刘冬梅..潜江凹陷东部地区新沟咀组下段浅水三角洲沉积模式[J].中国地质,2011,38(5):1263-1273,11.

基金项目

国家重大专项子课题"大面积砂岩、台缘礁滩沉积机理与有利储集体展布"(2008ZX05007-002-001)资助. (2008ZX05007-002-001)

中国地质

OA北大核心CSCDCSTPCD

1000-3657

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