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Seismic Interpretation in Kunbei Area of Qaidam Basin
详细信息   
摘要
The geologic structure of Kunbei area of Qaidam Basin is discovered through interpretation of amount of 2D and 3D seismic data.The structural features and details are implemented using pre-stack depth migration and interpretation.Commercial pool are found from Q16 and other wells using sequence stratigraphy.The result indicates that the structural framework of Kunbei area shows north-south zonation and east-west segregation,and three tectonic units including Qiexi slope belt-Qiekelike sag-Wudong slope belt,southern piedmont sag belt and central Kunbei fault-step belt are divided by the first-order faults.The upfaulted block faults of the Kunbei fault with mainly SN or NE or NW strike are more broken nearby the major fault and a large number of small faults around.Stratigraphic overlap trap in Lulehe group(E1+2) of Q16 well zone is found.The glutenite of lake system tract is mainly reservoir section and a more stable mudstone with 20~40m thick nearby the maximum flooding surface is regional cap rock.All of these are conducive to form the strati-lithologic trap.Using hydrocarbon detection technology,it is found that the main oil Lulehe group(E1+2) is located near the Q163 well.Prospective oil-bearing area of Q16 well is 33km2.A 12km2 new oil-bearing area located in the east of Q15 well is found.In short,prospective oil-bearing area by hydrocarbon detection is consistent with drilling results.

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