《中國塔里木盆地構造特徵與油氣(英文版)》內容簡介：《中國塔里木盆地構造特徵與油氣(英文版)》是作者精心為廣大讀者朋友們編寫而成的此書，可以讓更多的讀者朋友們從書中了解到更多的知識。《中國塔里木盆地構造特徵與油氣(英文版)》通過中國石油天然氣總公司illion噸和許多其他的發現。第二輪油氣資源評價由中國石油天然氣集團公司估計總石油資源19150000000000噸。塔里木盆地是一個大型未開發的。塔里木盆地是中國石油未來的希望，吸引了主要石油公司的利益。
基本介紹
- 書名：中國塔里木盆地構造特徵與油氣
- 作者：賈承造 等
- 出版日期：1997年8月1日
- 語種：簡體中文, 英語
- ISBN：9787502119560
- 外文名：TECTONIC CHARACTERISTICS and PETROLEUM TARIM BASIN CHINA
- 出版社：石油工業出版社
- 頁數：295頁
- 開本：16
- 品牌：石油工業出版社
內容簡介,圖書目錄,
內容簡介
《中國塔里木盆地構造特徵與油氣(英文版)》由石油工業出版社出版。
圖書目錄
1 TECTONIC ELEMENTS AND STRATIGRAPHY OF TARIM BASIN
1.1 Tectonic elements
1.1.1 Rises
1.1.2 Depressions
1.1.3 Periphyeral fault rises
1.2 Stratigraphy
1.2.1 Stratigraphic scheme
1.2.2 Sequence and distribution
2 GEOPHYSICAL FIELD AND DEEP STRUCTURE CHARACTERS OF TARIM BASIN
2.1 Natural earthquake converted wave sounding profile and crustal structure
2.1.1 Overview
2.1.2 Korla—Ruoqiang profile
2.1.3 Aksu—Yecheng profile
2.1.4 Kuqa—Tazhong—Tanan profile
2.1.5 Crustal structure of Tarim basin and its geodynamic implication
2.2 Gravity and magnetic field characteristics and crustal structure
2.2.1 Density and magnetic texture of cover and crust
2.2.2 Characters of gravity field
2.2.3 Characters of aeromagnetic anomaly and basement structure
2.3 Geothermal field， heat flow and lithospheric thermal structure
2.3.1 Data on thermal measurement and heat conductivity of rocks
2.3.2 Geothermal field of shallow part
2.3.3 Heat flow in Tarim
2.3.4 Thermal structure and rheology of lithosphere
2.4 Paleo temperature characteristics and its evolution
2.4.1 Implication of paleo temperature study and methods
2.4.2 Fission track of apatite after annealing
2.4.3 Vitrinite reflectance
2.4.4 Evolution of paleo temperature
TECTONIC CHARACTERISTICS OF TARIM PLATE
3.1 Overview on the tectonics of Tarim plate
3.1.1 PreCambrian basement of Tarim plate
3.1.2 Boundary of Tarim plate and regionalisation
3.1.3 Evolutionary characteristics
3.2 Drifting history and paleo magnetic evidences
3.2.1 Paleomagnetic results and the establishment of apparent polar wandering path
3.2.2 Drifting history of Tarim plate
3.2.3 Relationship with surrounding plates
3.3 Sinian to Paleozoic
3.3.1 Northern margin of Tarim plate
3.3.2 Southwest margin of Tarim plate
3.3.3 Altuntag and southeast margin of Tarim plate
3.4 Mesozoic to Cenozoic
3.4.1 Orogeny in northern margin of Tethyes
3.4.2 Basin character of Tarim in Mesozoic and Cenozozic
3.5 Volcanic rocks and implication
3.5.1 Distribution of volcanic rock
3.5.2 Composition of volcanic rocks
3.5.3 Tectonic model and implication
4 TECTONICS AND EVOLUTION OF TARIM BASIN
4.1 Evolutionary stages of the basin
4.1.1 Six important unconformities
4.1.2 Basin's prototypes
4.1.3 Tectonic evolution
4.2 Sinian to Ordovician， cratonic marginal aulacogen stage
4.2.1 Tectonic background and proto type basin
4.2.2 Sedimentary characters
4.2.3 Major tectonic events
4.2.4 Deformation at the end of Ordovician
4.3 Silurian to Devonian， marginal foreland basin stage
4.3.1 Tectonic background and proto type basin
4.3.2 Sedimentary characters
4.3.3 Major tectonic events
4.3.4 Deformation at the end of Devonian
4.4 Carboniferous to Permian， cratonic margin and intracratonic rift stages
4.4.1 Tectonic background and proto type basin
4.4.2 Sedimentary and structure characters
4.4.3 Tectonic event and deformation
4.5 Triassic， foreland basin stage
4.5.1 Tectonic background and proto type basin
4.5.2 Sedimentary and structure characters
4.5.3 Tectonic event and deformation
4.6 Jurassic to early Tertiary， fault depression stage
4.6.1 Tectonic background and proto type basin
4.6.2 Sedimentary and structure characters
4.6.3 Major tectonic events and deformation
4.7 Late Tertiary to Quaternary， composite foreland basin stage
4.7.1 Tectonic background
4.7.2 Sedimentary and structure characters
4.7.3 Deformation
4.8 Fault systems
4.8.1 Periphyeral fault system
4.8.2 Basement fault system
4.8.3 Cover fault system
5 STRUCTURAL CHARACTERS OF INTRACRATONIC PALEO UPLIFTS
5.1 Paleo uplifts of cratonic basin
5.1.1 Concept on cratonic basin and paleo uplift
5.1.2 Basic types and characters of paleo uplift
5.1.3 Evolution of three types of paleo uplift
5.2 Tazhong stable paleo uplift
5.2.1 Present characters
5.2.2 Evolution
5.2.3 Deformation at the end of Devonian
5.2.4 Local structure and trap
5.3 Tabei residual paleo uplift
5.3.1 Regionalisation
5.3.2 Evolution
5.3.3 Deformation at the end of early Permian
5.3.4 Local structure and trap
5.4 Tadong residual paleo uplift
5.4.1 Present characters
5.4.2 Evolution
5.4.3 Local structure and trap
5.5 Bachu active paleo uplift
5.5.1 Present characters
5.5.2 Evolution
5.5.3 Local structure and trap
5.6 Tanan active paleo uplift
5.6.1 Present characters
5.6.2 Evolution
5.6.3 Local structure and trap
6 FORELAND BASIN AND THRUST BELT
6.1 Nature of foreland and analysis on subsidence history
6.1.1 Nature of Mesozoic and Cenozoic foreland basin
6.1.2 Evolution in Mesozoic and Cenozoic
6.1.3 Subsidence history of foreland basin
6.2 Northwest strike—slip structure and Kalpin transpressional structure
6.2.1 Northwest strike—slip structure
6.2.2 Kalpin transpressional structure
6.3 Thrust belt of Kuqa Depression
6.3.1 Kuqa rejuvenation foreland thrusts
6.3.2 Strike—slip fault and Baicheng pull—apart basin
6.3.3 Balanced section
6.4 Mesozoic and Cenozoic inversion tectonics of Tabei Rise and Bachu Fault Uplift
6.4.1 Negative inversion tectonics of Tabei Rise
6.4.2 Positive inversion tectonics of Bachu Fault Uplift
6.5 Cenozoic structure of Southwest Tarim Depression
6.5.1 Foreland thrust belt
6.5.2 Strike—slip structure
6.6 Mesozoic and Cenozoic structure of Altuntag fault， southeast Tarim
6.6.1 Distribution of Altuntag fault system
6.6.2 Mesozoic and Cenozoic behavoir
7 TECTONICS AND PETROLEUM ACCUMULATION
7.1 Tectonics of Tarim Basin
7.1.1 Basin type and geophysical properties
7.1.2 Tarim plate
7.1.3 Evolution history of the basin
7.1.4 Cratonic paleo uplift
7.1.5 Foreland basin and thrust belt
7.2 Petroleum geology， a synthesis
7.2.1 Source rock and potential
7.2.2 Reservoir and seal
7.2.3 Traps and hydrocarbon play
7.3 Controlling factor of tectonics to petroleum accumulation
7.3.1 Petroleum accumulation of cratonic basin is under the control of paleo uplift and its slope
7.3.2 Petroleum accumulation of Mesozoic and Cenozoic foreland basin is under the control of Himalayan thrust belt
7.3.3 Pools controlled by fault and unconformity
7.4 Future petroleum exploration directions and suggestions
REFERENCE
1.1 Tectonic elements
1.1.1 Rises
1.1.2 Depressions
1.1.3 Periphyeral fault rises
1.2 Stratigraphy
1.2.1 Stratigraphic scheme
1.2.2 Sequence and distribution
2 GEOPHYSICAL FIELD AND DEEP STRUCTURE CHARACTERS OF TARIM BASIN
2.1 Natural earthquake converted wave sounding profile and crustal structure
2.1.1 Overview
2.1.2 Korla—Ruoqiang profile
2.1.3 Aksu—Yecheng profile
2.1.4 Kuqa—Tazhong—Tanan profile
2.1.5 Crustal structure of Tarim basin and its geodynamic implication
2.2 Gravity and magnetic field characteristics and crustal structure
2.2.1 Density and magnetic texture of cover and crust
2.2.2 Characters of gravity field
2.2.3 Characters of aeromagnetic anomaly and basement structure
2.3 Geothermal field， heat flow and lithospheric thermal structure
2.3.1 Data on thermal measurement and heat conductivity of rocks
2.3.2 Geothermal field of shallow part
2.3.3 Heat flow in Tarim
2.3.4 Thermal structure and rheology of lithosphere
2.4 Paleo temperature characteristics and its evolution
2.4.1 Implication of paleo temperature study and methods
2.4.2 Fission track of apatite after annealing
2.4.3 Vitrinite reflectance
2.4.4 Evolution of paleo temperature
TECTONIC CHARACTERISTICS OF TARIM PLATE
3.1 Overview on the tectonics of Tarim plate
3.1.1 PreCambrian basement of Tarim plate
3.1.2 Boundary of Tarim plate and regionalisation
3.1.3 Evolutionary characteristics
3.2 Drifting history and paleo magnetic evidences
3.2.1 Paleomagnetic results and the establishment of apparent polar wandering path
3.2.2 Drifting history of Tarim plate
3.2.3 Relationship with surrounding plates
3.3 Sinian to Paleozoic
3.3.1 Northern margin of Tarim plate
3.3.2 Southwest margin of Tarim plate
3.3.3 Altuntag and southeast margin of Tarim plate
3.4 Mesozoic to Cenozoic
3.4.1 Orogeny in northern margin of Tethyes
3.4.2 Basin character of Tarim in Mesozoic and Cenozozic
3.5 Volcanic rocks and implication
3.5.1 Distribution of volcanic rock
3.5.2 Composition of volcanic rocks
3.5.3 Tectonic model and implication
4 TECTONICS AND EVOLUTION OF TARIM BASIN
4.1 Evolutionary stages of the basin
4.1.1 Six important unconformities
4.1.2 Basin's prototypes
4.1.3 Tectonic evolution
4.2 Sinian to Ordovician， cratonic marginal aulacogen stage
4.2.1 Tectonic background and proto type basin
4.2.2 Sedimentary characters
4.2.3 Major tectonic events
4.2.4 Deformation at the end of Ordovician
4.3 Silurian to Devonian， marginal foreland basin stage
4.3.1 Tectonic background and proto type basin
4.3.2 Sedimentary characters
4.3.3 Major tectonic events
4.3.4 Deformation at the end of Devonian
4.4 Carboniferous to Permian， cratonic margin and intracratonic rift stages
4.4.1 Tectonic background and proto type basin
4.4.2 Sedimentary and structure characters
4.4.3 Tectonic event and deformation
4.5 Triassic， foreland basin stage
4.5.1 Tectonic background and proto type basin
4.5.2 Sedimentary and structure characters
4.5.3 Tectonic event and deformation
4.6 Jurassic to early Tertiary， fault depression stage
4.6.1 Tectonic background and proto type basin
4.6.2 Sedimentary and structure characters
4.6.3 Major tectonic events and deformation
4.7 Late Tertiary to Quaternary， composite foreland basin stage
4.7.1 Tectonic background
4.7.2 Sedimentary and structure characters
4.7.3 Deformation
4.8 Fault systems
4.8.1 Periphyeral fault system
4.8.2 Basement fault system
4.8.3 Cover fault system
5 STRUCTURAL CHARACTERS OF INTRACRATONIC PALEO UPLIFTS
5.1 Paleo uplifts of cratonic basin
5.1.1 Concept on cratonic basin and paleo uplift
5.1.2 Basic types and characters of paleo uplift
5.1.3 Evolution of three types of paleo uplift
5.2 Tazhong stable paleo uplift
5.2.1 Present characters
5.2.2 Evolution
5.2.3 Deformation at the end of Devonian
5.2.4 Local structure and trap
5.3 Tabei residual paleo uplift
5.3.1 Regionalisation
5.3.2 Evolution
5.3.3 Deformation at the end of early Permian
5.3.4 Local structure and trap
5.4 Tadong residual paleo uplift
5.4.1 Present characters
5.4.2 Evolution
5.4.3 Local structure and trap
5.5 Bachu active paleo uplift
5.5.1 Present characters
5.5.2 Evolution
5.5.3 Local structure and trap
5.6 Tanan active paleo uplift
5.6.1 Present characters
5.6.2 Evolution
5.6.3 Local structure and trap
6 FORELAND BASIN AND THRUST BELT
6.1 Nature of foreland and analysis on subsidence history
6.1.1 Nature of Mesozoic and Cenozoic foreland basin
6.1.2 Evolution in Mesozoic and Cenozoic
6.1.3 Subsidence history of foreland basin
6.2 Northwest strike—slip structure and Kalpin transpressional structure
6.2.1 Northwest strike—slip structure
6.2.2 Kalpin transpressional structure
6.3 Thrust belt of Kuqa Depression
6.3.1 Kuqa rejuvenation foreland thrusts
6.3.2 Strike—slip fault and Baicheng pull—apart basin
6.3.3 Balanced section
6.4 Mesozoic and Cenozoic inversion tectonics of Tabei Rise and Bachu Fault Uplift
6.4.1 Negative inversion tectonics of Tabei Rise
6.4.2 Positive inversion tectonics of Bachu Fault Uplift
6.5 Cenozoic structure of Southwest Tarim Depression
6.5.1 Foreland thrust belt
6.5.2 Strike—slip structure
6.6 Mesozoic and Cenozoic structure of Altuntag fault， southeast Tarim
6.6.1 Distribution of Altuntag fault system
6.6.2 Mesozoic and Cenozoic behavoir
7 TECTONICS AND PETROLEUM ACCUMULATION
7.1 Tectonics of Tarim Basin
7.1.1 Basin type and geophysical properties
7.1.2 Tarim plate
7.1.3 Evolution history of the basin
7.1.4 Cratonic paleo uplift
7.1.5 Foreland basin and thrust belt
7.2 Petroleum geology， a synthesis
7.2.1 Source rock and potential
7.2.2 Reservoir and seal
7.2.3 Traps and hydrocarbon play
7.3 Controlling factor of tectonics to petroleum accumulation
7.3.1 Petroleum accumulation of cratonic basin is under the control of paleo uplift and its slope
7.3.2 Petroleum accumulation of Mesozoic and Cenozoic foreland basin is under the control of Himalayan thrust belt
7.3.3 Pools controlled by fault and unconformity
7.4 Future petroleum exploration directions and suggestions
REFERENCE
