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Bottom topography, length, chamber structure of Timergazin canyon-like valley and problems of oil and gas exploration in basement

Authors: R.Kh. Muslimov (Kazan State University), A.M. Yakhin, A.I. Lysenkov, M.Z. Shakirov (VNIIGIS), I.A. Yakhina (Geophysical University Ural Department of RAS)

In this article there are specified: a sublatitudinal valley bottom topography of South Tatar arch, valley length and a position of directive pallial-crustal first order fracture. The valley bottom chamber was considered as continental rift structure with fracture-block tectonics in plan. The possible contribution of the valley to hydrocarbon transit from deep formations is estimated. The Subkhankulovsky swell is specified as possible hydrocarbon deposit within the basement.

In this article there are specified: a sublatitudinal valley bottom topography of South Tatar arch, valley length and a position of directive pallial-crustal first order fracture. The valley bottom chamber was considered as continental rift structure with fracture-block tectonics in plan. The possible contribution of the valley to hydrocarbon transit from deep formations is estimated. The Subkhankulovsky swell is specified as possible hydrocarbon deposit within the basement.



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