HEAT TRANSPORT BY GROUNDWATER FLOW DURING THE BAIKAL RIFT EVOLUTION

dc.contributor.author	Poort J.
dc.contributor.author	Polyansky O.
dc.date.accessioned	2021-06-11T04:57:58Z
dc.date.available	2021-06-11T04:57:58Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=13784549
dc.identifier.citation	Tectonophysics, 2002, 351, 1-2, 75-89
dc.identifier.issn	0040-1951
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/29045
dc.description.abstract	A two-dimensional modelling study of sedimentation, fluid flow, and heat flow in the Baikal rift basin undergoing flank uplift and basin subsidence has been performed in order to understand the impact of these processes on the surface heat flow signal. Heat flow anomalies of different scales and magnitudes have been observed at the sediment surface of the lake Baikal basin, and the presence of a hydrothermal vent suggests that fluids play an important role in the regional distribution of heat flow. The BASIN-code applied for this study allows to simulate topographically and compaction-driven hydrodynamical fluid flow and coupled heat transfer.
dc.title	HEAT TRANSPORT BY GROUNDWATER FLOW DURING THE BAIKAL RIFT EVOLUTION
dc.type	Статья

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