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Basic Types and Structural Characteristics of Uplifts: An Overview of Sedimentary Basins in China

HE Dengfa LI Desheng WU Xiaozhi WEN Zhu

地质学报(英文版)2009,Vol.83Issue(2):321-346,26.
地质学报(英文版)2009,Vol.83Issue(2):321-346,26.

Basic Types and Structural Characteristics of Uplifts: An Overview of Sedimentary Basins in China

Basic Types and Structural Characteristics of Uplifts: An Overview of Sedimentary Basins in China

HE Dengfa 1LI Desheng 2WU Xiaozhi 3WEN Zhu3

作者信息

  • 1. School of Energy Resources, China University ofGeosciences, Beijing 100083, China
  • 2. Key Laboratory for Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism, Ministry of Education, China University of Geosciences, Beijing 100083, China
  • 3. PetroChina Research Institute of Exploration and Development, Beijing 100083, China
  • 折叠

摘要

Abstract

The uplift is a positive structural unit of the crust. It is an important window for continental dynamics owing to its abundant structural phenomena, such as fault, fold, unconformity and denudation of strata. Meanwhile, it is the very place to store important minerals like oil, natural gas, coal and uranium. Giant and large-scale oil and gas fields in China, such as the Daqing Oilfield, Lunnan-Tahe Oilfield, Penglai 19-3 Oilfield, Puguang Gas Field and Jingbian Gas Field, are developed mainly on uplifts. Therefore, it is the main target both for oil and gas exploration and for geological study. The uplift can be either a basement uplift, or one developed only in the sedimentary cover. Extension, compression and wrench or their combined forces may give rise to uplifts. The development process of uplifting, such as formation, development, dwindling and destruction, can be taken as the uplifting cycle. The uplifts on the giant Precambrian cratons are large in scale with less extensive structural deformation. The uplifts on the medium- and small-sized cratons or neo-cratons are formed in various shapes with strong structural deformation and complicated geological structure. Owing to changes in the geodynamic environment, uplift experiences a multi-stage or multi-cycle development process. Its geological structure is characterized in superposition of multi-structural layers. Based on the basement properties, mechanical stratigraphy and development sequence, uplifts can be divided into three basic types--the succession, superposition and destruction ones. The succession type is subdivided into the maintaining type and the lasting type. The superposition type can he subdivided into the composite anticlinal type, the buried-hill draped type, the faulted uplift type and the migration type according to the different scales and superimposed styles of uplifts in different cycles. The destruction type is subdivided into the tilting type and the negative inverted type. The development history of uplifts and their controlling effects on sedimentation and fluids are quite different from one another, although the uplifts with different structural types store important minerals. Uplifts and their slopes are the main areas for oil and gas accumulation. They usually become the composite oil and gas accumulation zones (belts) with multiple productive formations and various types of oil and gas reservoirs.

关键词

uplift/geological structure/structural type/continental dynamics/oil and gas accumulation/sedimentary basin/China

Key words

uplift/geological structure/structural type/continental dynamics/oil and gas accumulation/sedimentary basin/China

分类

天文与地球科学

引用本文复制引用

HE Dengfa,LI Desheng,WU Xiaozhi,WEN Zhu..Basic Types and Structural Characteristics of Uplifts: An Overview of Sedimentary Basins in China[J].地质学报(英文版),2009,83(2):321-346,26.

基金项目

The paper is co-supported by the National Key Basic Research and Development Program of China(No.2006CB202300)and the National Natural Science Foundation Important Project(No. 407399061) (No.2006CB202300)

地质学报(英文版)

OACSCD

1000-9515

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