In Turpan-Hami basin,multi-source rocks are developed in Xiaocaohu secondary sag,and show good source conditions,abundant petroleum resources and bright prospects for exploration.Three reservoir-cap assemblages develo...In Turpan-Hami basin,multi-source rocks are developed in Xiaocaohu secondary sag,and show good source conditions,abundant petroleum resources and bright prospects for exploration.Three reservoir-cap assemblages developed in Middle Jurassic formed reservoir types in the sag which are structural-lithology oil-gas pools in Sanjian fang formation and Qiketai formation along with deep basinal gas pools in Xishanyao formation of Jurassic.The late Yanshan movement is a major stage for hydrocarbon accumulation in Xiaocaohu secondary sag.The primary controlled factors for its hydrocarbon accumulation is due to its palaeo-structures,tectonic setting and traps with structural-litholo gy feature.The exploratory efforts has good effectiveness based on these main controlled factors for evaluation and optimization of its favorable zones.展开更多
Having undergone four basin forming tectonic cycles--Hercynian, Indosinian, Yanshanian, and Himalayan, the Junggar basin becomes a multi cyclic superposed basin of old and hard mediun block pattern. Its multi cyclic t...Having undergone four basin forming tectonic cycles--Hercynian, Indosinian, Yanshanian, and Himalayan, the Junggar basin becomes a multi cyclic superposed basin of old and hard mediun block pattern. Its multi cyclic tectonic and sedimentary evolution results in five series of hydrocarbon source rock formations--Carboniferous, Permian, Upper Triassic, Middle lower Jurassic, and Lower Tertiary, correspondingly forming five petroleum generation systems, of which the Permian and Middle lower Jurassic petroleum generation systems are the most important with the highest exploration degree. Hydrocarbons are controlled by basin structure as follows: 1) Hydrocarbon accumulations are controlled by the structural styles of paleo uplifts, paleo overthrust belts and contorted anticline belts formed in multi cyclic tectonic movements; 2) Important pathways for long distance lateral and vertical migration are provided respectively by unconformities and faults; 3) The pool forming characteristics of the Permian petroleum system are controlled by paleo structure; 4) The pool forming characteristics of Jurassic and Tertiary petroleum system are controlled by recent structures.展开更多
文摘In Turpan-Hami basin,multi-source rocks are developed in Xiaocaohu secondary sag,and show good source conditions,abundant petroleum resources and bright prospects for exploration.Three reservoir-cap assemblages developed in Middle Jurassic formed reservoir types in the sag which are structural-lithology oil-gas pools in Sanjian fang formation and Qiketai formation along with deep basinal gas pools in Xishanyao formation of Jurassic.The late Yanshan movement is a major stage for hydrocarbon accumulation in Xiaocaohu secondary sag.The primary controlled factors for its hydrocarbon accumulation is due to its palaeo-structures,tectonic setting and traps with structural-litholo gy feature.The exploratory efforts has good effectiveness based on these main controlled factors for evaluation and optimization of its favorable zones.
文摘Having undergone four basin forming tectonic cycles--Hercynian, Indosinian, Yanshanian, and Himalayan, the Junggar basin becomes a multi cyclic superposed basin of old and hard mediun block pattern. Its multi cyclic tectonic and sedimentary evolution results in five series of hydrocarbon source rock formations--Carboniferous, Permian, Upper Triassic, Middle lower Jurassic, and Lower Tertiary, correspondingly forming five petroleum generation systems, of which the Permian and Middle lower Jurassic petroleum generation systems are the most important with the highest exploration degree. Hydrocarbons are controlled by basin structure as follows: 1) Hydrocarbon accumulations are controlled by the structural styles of paleo uplifts, paleo overthrust belts and contorted anticline belts formed in multi cyclic tectonic movements; 2) Important pathways for long distance lateral and vertical migration are provided respectively by unconformities and faults; 3) The pool forming characteristics of the Permian petroleum system are controlled by paleo structure; 4) The pool forming characteristics of Jurassic and Tertiary petroleum system are controlled by recent structures.
