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dc.contributor.author Seyferth M.
dc.contributor.author Henk A.
dc.date.accessioned 2025-02-22T06:18:20Z
dc.date.available 2025-02-22T06:18:20Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=53177406
dc.identifier.citation International Journal of Earth Sciences, 2006, 95, 2, 189-203
dc.identifier.issn 1437-3254
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48142
dc.description.abstract Basin-scale tectonics and sedimentation are studied using particle flow code (PFC), a special implementation of the distinct-element method (DEM) using circular elements. Special focus is on the development and application of new techniques, which allow for strain weakening and localisation effects and, thus, the formation of discrete fault patterns in high-resolution DE models.Fundamental modelling assumptions and the procedures necessary to define the microproperties of a DE material from given rock mechanical data are first explained. Recent methodical enhancements, consisting of automatic fault detection (AFD) and intelligent crack management (ICM) algorithms are also discussed. Refined DE modelling techniques are then applied to three scenarios of extensional basin formation, i.e. the evolution of halfgrabens above detachments with simple listric and ramp–flat–ramp geometries, respectively. Numerical modelling results compare favourably with the analogue (‘sandbox’) models widely used in this kind of basin studies. Not only do they reproduce the general basin architecture (e.g. roll-over anticlines and crestal collapse grabens), but also detailed fault structure and the sequence of faulting. In addition, numerical models can describe temporal changes in mechanical material properties to model compaction and diagenesis of syntectonic sediments.
dc.subject DISTINCT ELEMENT METHOD
dc.subject FINITE ELEMENT METHOD
dc.subject NUMERICAL MODELING
dc.subject HALF-GRABEN
dc.title A NUMERICAL SANDBOX: HIGH-RESOLUTION DISTINCT ELEMENT MODELS OF HALFGRABEN FORMATION
dc.type Статья
dc.identifier.doi 10.1007/s00531-005-0034-x


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