Oil & Gas Geology ›› 2003, Vol. 24 ›› Issue (4): 346-350.doi: 10.11743/ogg20030408

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PATHWAY SYSTEM OF OIL AND GAS MIGRATION IN BACHU-MAIGAITI AREA

She Xiaoyu1,2, Shi Zejin1, Liu Gaobo1   

  1. 1. Chengdu University of Technology, Chengdu, Sichuan;
    2. Jingzhou Branch of New Area Exploration, Exploration & Production Research Institute, SINOPEC, Jingzhou, Hubei
  • Received:2003-08-25 Online:2003-12-25 Published:2012-01-16

Abstract:

The pathways of oil and gas migration in Bachu-Maigaiti areas might consist mainly of faults, unconformity surfaces,as well as vugs,fissures and pores in reservoirs,which might have been connected with each other and constitute the delivery network of oil and gas.Among the 8 major unconformities, the T60 and T55 unconformity surfaces have been open in the whole area,the T70 and T54 unconformity surfaces have been open in the southern structural belt of Bachu uplift.Multiple tectonic movements have resulted in the opening of faults, pores,vugs and fissures,and became effective migration pathways of oil & gas.According to the dynamic theory of hydrocarbon migration and accumulation in late Caledonian-early Hercynian,the major pathway would be the pore-vug-fissure system in lower Cambrian dolomite that occurred in Awati sag and northeastern area of Bachu uplift; in late to last stage of Hercynian,the major pathway would include the boundary faults in the northeastern of Bachu uplift, T60 unconformity surface and pore-vug-fissure system in lower Cambrian;in Himalayan period, the major pathway would be the T60,T55 and T54 unconformity surfaces and the fault belt on the southern boundary of Bachu uplift that occurred mainly in the area including the Maigaiti slope and southern boundary of Bachu uplift.

Key words: pathway, mirgration, unconformity surface, fault, system, dynamic reservoiring

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