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- W2384879964 abstract "The Sudeerte buried-hills are very important reservoirs in the Hailaer Basin.The best reservoirs are generally developed on top of the Triassic metamorphosed silici-clastic rocks called Budate Group and with a thickness from several tens to over 100 meters.The so-called bi-media pore spaces composed of pore and fractures are the prevailing reservoir types with mean porosity of 5.0% and permeability of 0.03×10-3μm2.Two genetic types of the buried-hills can be recognized,faulted block and weathered peleo-uplift.With southwards subduction of the Mongolia-Okhotsk plate north of the studied area during Triassic to early Cretaceous,the Hailaer Basin suffered uplifting and weathering,secondary burying and block faulting,volcanism and fluid alteration,which constructed the buried-hill reservoirs there." @default.
- W2384879964 created "2016-06-24" @default.
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- W2384879964 date "2007-01-01" @default.
- W2384879964 modified "2023-09-23" @default.
- W2384879964 title "Geological Features and Genetic Interpretation of Sudeerte Buried-Hill Traps of Hailaer Basin,NE China" @default.
- W2384879964 hasPublicationYear "2007" @default.
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