A UNIFIED APPROACH TO MECHANICAL COMPACTION, PRESSURE SOLUTION, MINERAL REACTIONS AND THE TEMPERATURE DISTRIBUTION IN HYDROCARBON BASINS

dc.contributor.author	Yang X.S.
dc.date.accessioned	2021-02-10T04:02:05Z
dc.date.available	2021-02-10T04:02:05Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=554024
dc.identifier.citation	Tectonophysics, 2001, 330, 1-2, 141-151
dc.identifier.issn	0040-1951
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/24615
dc.description.abstract	In modelling sediment compaction and mineral reactions, the rheological behaviour of sediments is typically considered as poroelastic or purely viscous. In fact, compaction due to pressure solution and mechanical processes in porous media is far more complicated. A generalised model of viscoelastic compaction and the smectite to illite mineral reaction in hydrocarbon basins is presented. A one-step dehydration model of the mineral reaction is assumed. The obtained non-linear governing equations are solved numerically and different combinations of physical parameters are used to simulate realistic situations in typical sedimentary basins. Comparison of numerical simulations with real data has shown very good agreement with respect to both the porosity profile and the mineral reaction.
dc.subject	COMPACTION
dc.subject	MINERAL REACTION
dc.subject	VISCOELASTICITY
dc.subject	SEDIMENTARY BASINS
dc.subject	PRESSURE SOLUTION
dc.title	A UNIFIED APPROACH TO MECHANICAL COMPACTION, PRESSURE SOLUTION, MINERAL REACTIONS AND THE TEMPERATURE DISTRIBUTION IN HYDROCARBON BASINS
dc.type	Статья

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