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- W2393640896 abstract "Wulong karst comprises several karst systems which developed independently in the vadose zone of the limestone aquifer under distinct geological structure and core hydrographic conditions. Study of the karst systems in Wulong can elucidate the local tectonic uplift: from the later Neogene or early Pleistocene to present the area has been in a state of continuous uplift without evidence of subsidence. At the beginning of this time range, 80~100Ma of uplift occurred without relative stability. This was followed by uplift and relative stability, with the latter more significant than the former. During the middle Pleistocene large horizontal caves developed which are now found 150~300m above river level in deep gorges related to significant rivers. The uplift and relative stability may have occurred on a fifty-fifty basis since the late Pleistocene." @default.
- W2393640896 created "2016-06-24" @default.
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- W2393640896 date "2007-01-01" @default.
- W2393640896 modified "2023-09-26" @default.
- W2393640896 title "Wulong karst systems and as an indicator of local tectonic uplift" @default.
- W2393640896 hasPublicationYear "2007" @default.
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