Compaction-centrifugal flow percolation and hydrocarbon enrichment of T/C-P unconformable double stratigraphic structure: A case study of Triassic T1b Formation in Madong slope area, Junggar Basin
1. PetroChina Hangzhou Institute of Geology, Hangzhou, Zhejiang 310023, China; 2. PetroChina Research Institute of Exploration and Development, Xinjiang Oilfield, Karamay, Xinjiang 834000, China
Abstract:To discuss the percolation effect of atmospheric fresh water on overlying strata above the unconformable surface, this paper uses data such as seismic-geology comprehensive profile, reservoir physical property, fluid(oil and water) geochemical parameters, formation testing, and pilot production to comprehensive analyze the stratum structure and compaction-centrifugal flow distribution characteristics related to the unconformable surface. It reveals that under the control of the T/C-P unconformable double stratigraphic structure, the vertical percolation of atmospheric fresh water to the overlying strata above the T/P unconformable surface by compaction-centrifugal flow leads to the low oil & gas charging degree of Triassic Baikouquan(T1b) Formation in Madong slope area. The results show that the direction of the fluid potential in the compaction-centrifugal flow percolation zone of T1b Formation above the T/P unconformable surface in the Madong slope area is opposite to that of the gravity potential, which is closely related to the capillary self-imbibition of the mud-rich conglomerate facies at the bottom of T1b Formation and the associated wetting water phase. The atmospheric fresh water percolates upward mainly along the micro-pore throat in the mud-rich conglomerate of the T1b Formation above the T/P unconformable surface, forming a bottom-up compactioncentrifugal flow. The vertical percolation depth of compaction-centrifugal flow is about 45 m, and the plane extension distance is about 28 km. The compaction-centrifugal flow against gravity potential leads to a low degree of oil & gas charging in the T1b Formation, and oil & gas mainly accumulate in the mud-poor conglomerate reservoir with excellent physical properties in the middle and upper part of the sand formation. According to compaction-centrifugal flow percolation and hydrocarbon enrichment characteristics of T/C-P unconformable double stratigraphic structure, logging quantitative identification criteria of the T1b Formation reservoir are lgRT > 1.4 Ω·m(RT > 25 Ω·m) and IMP < 9000 g·cm-3·m·s-1. The RT-IMP joint-constrained oil reservoir quantitative prediction map is used to predict two oil and gas enrichment areas, namely the east wing of Xiazijie Fan(with an area of 98 km2) and the north wing of Madong-Xiayan Fan(with an area of 104 km2).
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