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- W2378587662 abstract "The water in coal strata mainly come from the under Ordovician carbonate in many coal mine of China. So the study of the Ordovician carbonate and its hydrousity is important for the solution of water abruption happened in the coal bed. It is difficult to recognize the Ordovician interface, because the great difference of the coal seam and its surrounding lithology, and the smaller distance between coal and the Ordovician sediment, so that the Ordovician reflection is shielded and weak contrast to the coals reflecting. And the study of the Ordovician interface and its inner structure can not be gotten through the common high resolution 3 D seismic exploration. In Talimu basin, the western of China, we had successfully traced the Ordovician interface in 5500 meters depth and restored the ancient Karst and grotto landform, which greatly affect the oil and gas exploration, with the objective seismic exploration. If this technique is applied to the coal mine seismic exploration and more emphasis can be given in the field designation and sampling, including the processing and interpretation, the water abruption problem should be solved more efficiently." @default.
- W2378587662 created "2016-06-24" @default.
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- W2378587662 date "2002-01-01" @default.
- W2378587662 modified "2023-09-25" @default.
- W2378587662 title "The possibility of detecting water in the Ordovician carbonate with objective seismic exploration" @default.
- W2378587662 hasPublicationYear "2002" @default.
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