中國含油氣沉積盆地論

內(nèi)容概要

　　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.

書籍目錄

FOREWORDCHAPTER l INTRODUCTION TO PETROLIFEROUS SEDIMENTARY BASIN1.1 Sedimentary Basin as the Basic Geological Unit for Oil/gas Generation and Occurrence1.2 Controlling Factors ofS.edimentary Basins on Oil/gas Generation and Occurrence1.2.1 A sedimentary basin formed under a certain tectonic environment is favorable to oil/gas generation andevolution, if under long-term continued subsidence1.2.2 Multi-cyclicity of crustal movement leads to multi-cyclicity of structural evolution and deformat;on ofthe basin and the formation of source-reservoir-seal combinations at different stages and various typesof oil/gas pools1.2.3 Control of palaeoclimate on oil/gas bearing basins1.2.4 Sedimentary system, facies and diagenetics control the richness of oil/gas1.2.5 0rganic-rich source rock is the basis for oil/gas generation,and oil-generating sag controls the distribu-tion of oil/gas pools1.2.6 Appropriate palaeo-geotemperature is critical to oil/gas generation1.2.7 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 accumulation1.2.8 Regional structural style controls the type and distribution of traps1.2.9 Temporal and spatial matching of source, reservoir, seal, migration, trap, preservation is critical for anaccumulation to become a poolCHAPTER 2 REGIONAL GEOLOGY OF CHINA2.1 Regional Tectonic Units and Their Spatial Distribution2.1.1 North China stable continent tectonic province2.1.2 Tarim stable continent tectonic province2.1.3 Qaidam stable continent tectonic province2.1.4 Yangtze stable continent tectonic province2.1.5 Gondwana northern margin tectonic province2.1.6 Tianshan-Hinggan-Mongolia-Jilin/Heilongjiang tectonic province2.1.7 Qinling-Qilian tectonic province2.1.8 Kunlun tectonic province2.1.9 Songpan-Garze tectonic province2.1.10 Karakorum-Tanggula-Sanjiang tectonic province2.1.11 South China tectonic province2.1.12 East continental margin tectonuc province2.2 Historical Development of Crustal Structure2.2.1 Fuping Period2.2.2 Luliang Period2.2.3 Jinning Period2.2.4 Caledonian Period2.2.5 Hercynian Period2.2.6 Indosinian Period2.2.7 Yanshanian Period2.2.8 Himalayan PeriodCHAPTER 3 TYPES OF PETROLIFEROUS BASINS IN CHINA3.1 Significance of Basin Classification and Previous Classifications3.1.1 Significance of basin classification3.1.2 Previous basin classification3.2 Types and Evolution of Petroliferous Sedimentary Basins in China3.2.1 Basin types3.2.2 Basin development and formation of Meso-Cenozoic superposed basinsCHAPTER 4 ANALYSIS OF PETROLIFEROUS SEDIMENTARY BASINS4.1 Introduction4.1.1 Sigruficance and basic content of analysis of petroliferous sedimentary basins4.1.2 Multi-factor synthetic analysis of petroliferous sedimentary basins4.1.3 General guideline for analysis of petroliferous sedimentarv basins4.2 Analysis of Basin Subsidence and Burial History4.2.1 Subsidence and fill-up as well as their significance in petroleum geology4.2.2 Mechanism of basin subsidence4.2.3 Restoration of subsidence and burial history of sedimentary basins4.3 Thermal Regimes and Thermal History Analysis of Sedimentary Basins4.3.1 Geotherm and its significance to hydrocarbon generation4.3.2 Geotemperature field and thermal regime of sedimentary basin4.3.3 General methods for reconstructing thermal histories of sedimentarv basins4.4 Multi-cyclic Evolution of Basins and Multi-stage Association of Source-Reservoir-Seal4.4.1 Multi-cyclicity of crustal movement and superposed basins4.4.2 Multi-cyclic evolution of basins and multi-stage hydrocarbon-generating formation4.4.3 Multi-cyclic sedimentary formations and multi-stage source-reservoir-seal associations4.5 Depositional Systems, Diagenesis and Their Relationships with Hydrocarbon Accumulation4.5.1 Depositional systems, sedimentary facies and temporal and spatial distribution of sedimentary basins4.5.2 Sedimentary facies belt and relatioriship with hydrocarbon accumulation4.5.3 Diagenesis and- epigenesis of depositional systems and their relationships with oil and gas4.6 Source Rock Evaluation and Analysis of Hydrocarbon-Generation Histow of Basins4.6.1 Basic theory of hydrocarbon generation4.6.2 Evaluation of source rocks in petroliferous basins4.6.3 Quantitative calculation of hydrocarbon generation history4.7 Palaeoclimatology and Hydrocarbon-Bearing Features of Sedimentary Basins4.7.1 Palaeoclimatology and the principle ofits reconstruction4.7.2 Palaeoclimate condition and oil-bearing features of sedimentary basins……

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