Tarim basin locates in the southern part of Xinjiang Uygur Autonomous Region. Geographically，it is circled by the huge Tianshan and Karakunlun Mountains and Altuntag， occurs as a large intra continental， inter mountainous basin with an extent of 560 000 km2. Taklamkan Desert， 330 000 km2， situates in the central part. Great foothill alluvial fan and flood plain surround the basin.Tarim Basin is the largest sedimentary basin of China. The remaining thickness of sedimentary rocks is 16 000 m， maximum accumulated thickness is 25 000 m. Residual total volume of sedimentary rocks is 400 milLion m3. Stratum involves Sinian to lower Permian of marine to paralic facies and upper Permian to Quaternary of continental facies. After works for more than 30 years， specially intensive exploration in recent 6 years， 8 fields with proven and control reserves of over 40 m：illion tons and a lot of other discoveries are obtained by China National Petroleum Corporation. The second round petroleum resource assessment held by CNPC estimates the total petroleum resource is 19.15 trillion tons. Tarim is one of large unexplored basin. Tarim is the hope of Chinese petroleum future， attracts the interest of major oil companies.
作者簡介
暫缺《中國塔里木盆地構(gòu)造特征與油氣（英文版）》作者簡介
圖書目錄
1 TECTOMC 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 GEOPIIYSICAL FIELD AND DEEP STRUCTURE CHARACTERS OF TARIM BASIN 2.1 Natural etuthquake converted wave sounding profile and custal structure 2.1.1 Overview 2.1.2 Korla-Ruoqiangprofile 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 ofgravity field 2.2.3 Characters of aeromagnetic anomaly and basement structure 2.3 Geothermal field, heat flow and lithosphenc 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 flowin Tarim 2.3.4 Thermal stmcture and theology oflithosphere 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 Vitrinitereflectance 2.4.4 Evolution ofpaleo temperature 3 TECTOMC CHARACTERISTICS OF TARIM PLATE 3.1 Overview on the tectorucs of Tarim plate 3.1.1 PreCambrian basement ofTarim plate 3.1.2 Boundary ofTarim plate and regionalisation 3.1.3 Evolutionary characteristics 3.2 Drifting history and paleo magnetic evidences 3.2.1 Paleomagnetic results and the establishment ofapparent polar wandering path 3.2.2 Drifting history of Tarim plate 3.2.3 Relationshipwith surroundingplates 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 andimplication 3.5.1 Distribution ofvolcanic rock 3.5.2 Compositionofvolcanic rocks 3.5.3 Tectonic model andimplication 4 TECTONICS AND EVOLUTION OF TARIM BASIN 4.1 Evolutionary stages ofthe basin 4.1.1 Siximportant 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 …… 5 STRUCTURAL CHARACTERS OFINTRACRATOMC PALEO UPLIFTS 6 FORELAND BASIN AND THRUST BELT 7 TECTONICS AND PETROLEUM ACCUMULATION REFERENCE
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