Search results for " thermal modelling"

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Thermal and structural modeling of the Scillato wedge-top basin source-to-sink system. Insights into the Sicilian fold-and-thrust belt evolution (Ita…

2019

AbstractTemperature-dependent clay mineral assemblages, vitrinite reflectance, and one-dimensional (1-D) thermal and three-dimensional (3-D) geological modeling of a Neogene wedge-top basin in the Sicilian fold-and-thrust belt and its pre-orogenic substratum allowed us to: (1) define the burial history of the sedimentary succession filling the wedge-top basin and its substratum, (2) reconstruct the wedge-top basin geometry, depocenter migration, and sediment provenance through time in the framework of a source-to-sink system, and (3) shed new light into the kinematic evolution of the Apennine-Maghrebian fold-and-thrust belt.The pre-orogenic substratum of the Scillato basin shows an increase…

010504 meteorology & atmospheric sciencesmixed layers illite-smectiteStratigraphyCenozoic deformation[SDU.STU]Sciences of the Universe [physics]/Earth SciencesReflectionStructural basin010502 geochemistry & geophysics01 natural sciencesWedge (geometry)Paleontologywedge-top basin; vitrinite reflectance; mixed layers illite-smectite; thermal modelling; source-to-sink systems; Sicilian fold-and-thrust beltSicilian fold-and-thrust beltThermalthermal modellingClay mineralSedimentologySource to sinkEurope faultsvitrinite reflectancesource-to-sink systems0105 earth and related environmental sciencesMesozoic sedimentary rocks tectonicsgeographygeography.geographical_feature_categoryFaultingGeologySedimentology15. Life on landwedge-top basinlanguage.human_languageStratigraphyFold and thrust beltlanguageThree dimensional computer graphicsSicilianGeologyTertiary
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3D structural modeling and restoration in fold-and-thrust belts: examples from the Kumeta and Busambra Mts., NW Sicily (Italy)

2018

The Sicilian Fold and Thrust belt (SFTB) is a structurally complex area where along-strike variations of structural styles, shortening amounts, exhumation rates and amounts of syn-tectonic sedimentation frequently occur. Moreover strong differential clockwise rotations around vertical axes affected the different tectonic units during their emplacement. This complexity, coupled with debatable or incomplete subsurface dataset (e.g., available 2D onshore seismic lines) allowed previous authors to propose different interpretations for the tectonic evolution of the SFTB since Cenozoic time. The study area, located in the Western sector of the SFTB comprises the Kumeta and Busambra ridges (derive…

Settore GEO/03 - Geologia StrutturaleSicilian FTB 3D model thermal modelling along strike variation of structures
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