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- W2384662136 abstract "Budong spring is located in flake permafrost(frozen rock) regions,with recharge source from glacial melt water from the main ridge of the southern slope of Kunlun Mountains,precipitation and surface water.Recharge source water runoff into Budong spring NE tension-torsional fault(F2),which is a structure-geothermal talik course,blocked Budong spring NWW compression-scissor fault(F1),and enriched in crossover point of F1 and F2,upwelling to be ascending spring.This is the main mechanism of water controlled by structures and the cause of Budong spring natural ascending spring.In order to solve the local problem of water shortage in winter,water supplied hydro-geological borehole should be arranged in the NW sharing hanging wall which is in the crossover point of F1 and F2,then rich and good quality groundwater could be found.Prospecting water direction in permafrost regions was designated in this study." @default.
- W2384662136 created "2016-06-24" @default.
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- W2384662136 date "2011-01-01" @default.
- W2384662136 modified "2023-09-28" @default.
- W2384662136 title "Study on Mechanism of Water Controlled by Structures in Budong Spring Region along Qinghai-Tibet Highway" @default.
- W2384662136 hasPublicationYear "2011" @default.
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