书籍详情
中国含油气沉积盆地论（英文版）
作者：田在艺，张庆春 著
出版社：石油工业出版社
出版时间：1997-09-01
ISBN：9787502121297
定价：¥60.00
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内容简介
Since the founding of the People’s Republic of China，glorious achievements in petroleum industry of China have been accomplished. The annual production of crude oil has increased from 120，000 t in 1949 t0 146，000，000 t in 1995， and that of natural gas has reached 17，000，000，000 m3. Meanwhile， Chinese petroleum sci-entists and engineers are open minded， bold in-making innovations， and make painstaking efforts to achieve great successes in creating the theory of petroleum geol-ogy with Chinese characteristics.
作者简介
暂缺《中国含油气沉积盆地论（英文版）》作者简介
目录
FOREWORD
CHAPTER l INTRODUCTION TO PETROLIFEROUS SEDIMENTARY BASIN
1.1 Sedimentary Basin as the Basic Geological Unit for Oil/gas Generation and Occurrence
1.2 Controlling Factors ofS.edimentary Basins on Oil/gas Generation and Occurrence
1.2.1 A sedimentary basin formed under a certain tectonic environment is favorable to oil/gas generation and
evolution, if under long-term continued subsidence
1.2.2 Multi-cyclicity of crustal movement leads to multi-cyclicity of structural evolution and deformat;on of
the basin and the formation of source-reservoir-seal combinations at different stages and various types
of oil/gas pools
1.2.3 Control of palaeoclimate on oil/gas bearing basins
1.2.4 Sedimentary system, facies and diagenetics control the richness of oil/gas
1.2.5 0rganic-rich source rock is the basis for oil/gas generation,and oil-generating sag controls the distribu-tion of oil/gas pools
1.2.6 Appropriate palaeo-geotemperature is critical to oil/gas generation
1.2.7 0il/gas migration is a link in the whole process of generation, migration and accumulation, and hydro-dynamics has an important influence on migration and accumulation
1.2.8 Regional structural style controls the type and distribution of traps
1.2.9 Temporal and spatial matching of source, reservoir, seal, migration, trap, preservation is critical for an
accumulation to become a pool
CHAPTER 2 REGIONAL GEOLOGY OF CHINA
2.1 Regional Tectonic Units and Their Spatial Distribution
2.1.1 North China stable continent tectonic province
2.1.2 Tarim stable continent tectonic province
2.1.3 Qaidam stable continent tectonic province
2.1.4 Yangtze stable continent tectonic province
2.1.5 Gondwana northern margin tectonic province
2.1.6 Tianshan-Hinggan-Mongolia-Jilin/Heilongjiang tectonic province
2.1.7 Qinling-Qilian tectonic province
2.1.8 Kunlun tectonic province
2.1.9 Songpan-Garze tectonic province
2.1.10 Karakorum-Tanggula-Sanjiang tectonic province
2.1.11 South China tectonic province
2.1.12 East continental margin tectonuc province
2.2 Historical Development of Crustal Structure
2.2.1 Fuping Period
2.2.2 Luliang Period
2.2.3 Jinning Period
2.2.4 Caledonian Period
2.2.5 Hercynian Period
2.2.6 Indosinian Period
2.2.7 Yanshanian Period
2.2.8 Himalayan Period
CHAPTER 3 TYPES OF PETROLIFEROUS BASINS IN CHINA
3.1 Significance of Basin Classification and Previous Classifications
3.1.1 Significance of basin classification
3.1.2 Previous basin classification
3.2 Types and Evolution of Petroliferous Sedimentary Basins in China
3.2.1 Basin types
3.2.2 Basin development and formation of Meso-Cenozoic superposed basins
CHAPTER 4 ANALYSIS OF PETROLIFEROUS SEDIMENTARY BASINS
4.1 Introduction
4.1.1 Sigruficance and basic content of analysis of petroliferous sedimentary basins
4.1.2 Multi-factor synthetic analysis of petroliferous sedimentary basins
4.1.3 General guideline for analysis of petroliferous sedimentarv basins
4.2 Analysis of Basin Subsidence and Burial History
4.2.1 Subsidence and fill-up as well as their significance in petroleum geology
4.2.2 Mechanism of basin subsidence
4.2.3 Restoration of subsidence and burial history of sedimentary basins
4.3 Thermal Regimes and Thermal History Analysis of Sedimentary Basins
4.3.1 Geotherm and its significance to hydrocarbon generation
4.3.2 Geotemperature field and thermal regime of sedimentary basin
4.3.3 General methods for reconstructing thermal histories of sedimentarv basins
4.4 Multi-cyclic Evolution of Basins and Multi-stage Association of Source-Reservoir-Seal
4.4.1 Multi-cyclicity of crustal movement and superposed basins
4.4.2 Multi-cyclic evolution of basins and multi-stage hydrocarbon-generating formation
4.4.3 Multi-cyclic sedimentary formations and multi-stage source-reservoir-seal associations
4.5 Depositional Systems, Diagenesis and Their Relationships with Hydrocarbon Accumulation
4.5.1 Depositional systems, sedimentary facies and temporal and spatial distribution of sedimentary basins
4.5.2 Sedimentary facies belt and relatioriship with hydrocarbon accumulation
4.5.3 Diagenesis and- epigenesis of depositional systems and their relationships with oil and gas
4.6 Source Rock Evaluation and Analysis of Hydrocarbon-Generation Histow of Basins
4.6.1 Basic theory of hydrocarbon generation
4.6.2 Evaluation of source rocks in petroliferous basins
4.6.3 Quantitative calculation of hydrocarbon generation history
4.7 Palaeoclimatology and Hydrocarbon-Bearing Features of Sedimentary Basins
4.7.1 Palaeoclimatology and the principle ofits reconstruction
4.7.2 Palaeoclimate condition and oil-bearing features of sedimentary basins
……
CHAPTER l INTRODUCTION TO PETROLIFEROUS SEDIMENTARY BASIN
1.1 Sedimentary Basin as the Basic Geological Unit for Oil/gas Generation and Occurrence
1.2 Controlling Factors ofS.edimentary Basins on Oil/gas Generation and Occurrence
1.2.1 A sedimentary basin formed under a certain tectonic environment is favorable to oil/gas generation and
evolution, if under long-term continued subsidence
1.2.2 Multi-cyclicity of crustal movement leads to multi-cyclicity of structural evolution and deformat;on of
the basin and the formation of source-reservoir-seal combinations at different stages and various types
of oil/gas pools
1.2.3 Control of palaeoclimate on oil/gas bearing basins
1.2.4 Sedimentary system, facies and diagenetics control the richness of oil/gas
1.2.5 0rganic-rich source rock is the basis for oil/gas generation,and oil-generating sag controls the distribu-tion of oil/gas pools
1.2.6 Appropriate palaeo-geotemperature is critical to oil/gas generation
1.2.7 0il/gas migration is a link in the whole process of generation, migration and accumulation, and hydro-dynamics has an important influence on migration and accumulation
1.2.8 Regional structural style controls the type and distribution of traps
1.2.9 Temporal and spatial matching of source, reservoir, seal, migration, trap, preservation is critical for an
accumulation to become a pool
CHAPTER 2 REGIONAL GEOLOGY OF CHINA
2.1 Regional Tectonic Units and Their Spatial Distribution
2.1.1 North China stable continent tectonic province
2.1.2 Tarim stable continent tectonic province
2.1.3 Qaidam stable continent tectonic province
2.1.4 Yangtze stable continent tectonic province
2.1.5 Gondwana northern margin tectonic province
2.1.6 Tianshan-Hinggan-Mongolia-Jilin/Heilongjiang tectonic province
2.1.7 Qinling-Qilian tectonic province
2.1.8 Kunlun tectonic province
2.1.9 Songpan-Garze tectonic province
2.1.10 Karakorum-Tanggula-Sanjiang tectonic province
2.1.11 South China tectonic province
2.1.12 East continental margin tectonuc province
2.2 Historical Development of Crustal Structure
2.2.1 Fuping Period
2.2.2 Luliang Period
2.2.3 Jinning Period
2.2.4 Caledonian Period
2.2.5 Hercynian Period
2.2.6 Indosinian Period
2.2.7 Yanshanian Period
2.2.8 Himalayan Period
CHAPTER 3 TYPES OF PETROLIFEROUS BASINS IN CHINA
3.1 Significance of Basin Classification and Previous Classifications
3.1.1 Significance of basin classification
3.1.2 Previous basin classification
3.2 Types and Evolution of Petroliferous Sedimentary Basins in China
3.2.1 Basin types
3.2.2 Basin development and formation of Meso-Cenozoic superposed basins
CHAPTER 4 ANALYSIS OF PETROLIFEROUS SEDIMENTARY BASINS
4.1 Introduction
4.1.1 Sigruficance and basic content of analysis of petroliferous sedimentary basins
4.1.2 Multi-factor synthetic analysis of petroliferous sedimentary basins
4.1.3 General guideline for analysis of petroliferous sedimentarv basins
4.2 Analysis of Basin Subsidence and Burial History
4.2.1 Subsidence and fill-up as well as their significance in petroleum geology
4.2.2 Mechanism of basin subsidence
4.2.3 Restoration of subsidence and burial history of sedimentary basins
4.3 Thermal Regimes and Thermal History Analysis of Sedimentary Basins
4.3.1 Geotherm and its significance to hydrocarbon generation
4.3.2 Geotemperature field and thermal regime of sedimentary basin
4.3.3 General methods for reconstructing thermal histories of sedimentarv basins
4.4 Multi-cyclic Evolution of Basins and Multi-stage Association of Source-Reservoir-Seal
4.4.1 Multi-cyclicity of crustal movement and superposed basins
4.4.2 Multi-cyclic evolution of basins and multi-stage hydrocarbon-generating formation
4.4.3 Multi-cyclic sedimentary formations and multi-stage source-reservoir-seal associations
4.5 Depositional Systems, Diagenesis and Their Relationships with Hydrocarbon Accumulation
4.5.1 Depositional systems, sedimentary facies and temporal and spatial distribution of sedimentary basins
4.5.2 Sedimentary facies belt and relatioriship with hydrocarbon accumulation
4.5.3 Diagenesis and- epigenesis of depositional systems and their relationships with oil and gas
4.6 Source Rock Evaluation and Analysis of Hydrocarbon-Generation Histow of Basins
4.6.1 Basic theory of hydrocarbon generation
4.6.2 Evaluation of source rocks in petroliferous basins
4.6.3 Quantitative calculation of hydrocarbon generation history
4.7 Palaeoclimatology and Hydrocarbon-Bearing Features of Sedimentary Basins
4.7.1 Palaeoclimatology and the principle ofits reconstruction
4.7.2 Palaeoclimate condition and oil-bearing features of sedimentary basins
……
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