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塔东低凸起震旦系断陷台地沉积特征及发育模式

何金有 李洪辉 罗平 王显东

地质与勘探2017,Vol.53Issue(2):361-370,10.
地质与勘探2017,Vol.53Issue(2):361-370,10.

塔东低凸起震旦系断陷台地沉积特征及发育模式

Sedimentary Characteristics and Evolution Models of the Sinian Rift Platform in the Low-Uplift,Eastern Tarim Basin

何金有 1李洪辉 2罗平 2王显东3

作者信息

  • 1. 中国地质大学(北京)能源学院,北京 100083
  • 2. 中国石油勘探开发研究院,北京 100083
  • 3. 大庆油田有限责任公司勘探开发研究院,黑龙江大庆 163712
  • 折叠

摘要

Abstract

By utilization of drilling cores and seismic data,this work revealed the sedimentary characteristics of Sinian in the low-uplift,eastern Tarim basn and established its evolutionary model.The study suggested that three sedimentary facies were identified in the Sinian dolostones,including tidal fiat,grain beach and ramp types.Well correlation and seismic sections showed that Sinian sedimentary sequences in this area have a wedge-shaped reflective structure,indicating a northward dipping rift basin and overall pattern of high in south and low in north.An evolutionary model of the basin was constructed that shows a change from a northward gentle dipping monocline at the early stage into a rift platform,of which the primary portion is the slope from the well TD-1 to the north of well DT-1.

关键词

断陷台地/白云岩/震旦系/塔东低凸起

Key words

rift platform/dolostone/Sinian System/low-uplift in eastern Tarim basin

分类

能源科技

引用本文复制引用

何金有,李洪辉,罗平,王显东..塔东低凸起震旦系断陷台地沉积特征及发育模式[J].地质与勘探,2017,53(2):361-370,10.

基金项目

国家自然科学青年基金项目(编号:41302105)和中央高校基本科研业务费专项资金(编号:2-9-2015-136)联合资助. (编号:41302105)

地质与勘探

OA北大核心CSCDCSTPCD

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