Search results for "Hydrocarbon exploration"

showing 4 items of 4 documents

Subsurface geometries in central sicily FTB as a premise for hydrocarbon exploration

2008

The study concerns a sector of the Maghrebian Sicilian Fold and Thrust Belt (FTB), located in central Sicily between the southern edge of the Madonie Mts. and the Caltanissetta trough. Interpretation of recently acquired seismic profiles, constrained by joint detailed stratigraphy and field investigation, revealed the structure of the study area as formed by a thick pile of deep water carbonate (Imerese and Sicanian) thrusts lying on carbonate platform imbricates. In the forward migration of the FTB, two main tectonic events were envisaged; shallow and deep seated thrusts occurred during the Miocene-early Pleistocene time interval that deformed the former sedimentary cover of the continenta…

geographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformTrough (geology)chemistry.chemical_compoundPaleontologyTectonicschemistryContinental marginFold and thrust beltHYDROCARBON EXPLORATIONCarbonateSedimentary rockCENTRAL SICILYPetrologyHydrocarbon explorationGeology
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Influence of surface processes and initial topography on lateral fold growth and fold linkage mode

2015

Elongation of randomly distributed fold segments and their potential linkage are important for hydrocarbon exploration because it can greatly influence the morphology of the reservoir and both migration and accumulation of hydrocarbons in antiformal traps. Here we study the effects of surface processes and the presence of a topographic slope on the different linkage modes that can occur, and how these parameters affect the required horizontal offset for perturbations to link. The proposed numerical model represents a sedimentary cover detached over a much weaker basal decollement layer. The upper surface is modified by mass redistribution, which is achieved by a combination of fluvial and h…

DécollementTectonicsGeophysicsGeochemistry and PetrologyAnticlineFluvialSedimentary rockFold (geology)ElongationHydrocarbon explorationGeomorphologyGeologyTectonics
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Modeling of wind gap formation and development of sedimentary basins during fold growth: application to the Zagros Fold Belt, Iran

2016

Mountain building and landscape evolution are controlled by interactions between river dynamics and tectonic forces. Such interactions have been extensively studied, however a quantitative evaluation of tectonic/geomorphic feedbacks, which is imperative for understanding sediments routing within orogens and fold-and-thrust belts, remains to be undertaken. Here, we employ numerical simulations to assess the conditions of uplift and river incision necessary to deflect an antecedent drainage network during the growth of one, or several, folds. We propose that a partitioning of the river network into internal (endorheic) and longitudinal drainage arises as a result of lithological differences w…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeography Planning and DevelopmentFluvialFold (geology)Sedimentary basin010502 geochemistry & geophysics01 natural sciencesTectonicsMountain formationEarth and Planetary Sciences (miscellaneous)Sedimentary rockDrainageHydrocarbon explorationGeomorphologyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesEarth Surface Processes and Landforms
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Intact seismic-scale platforms and ramps in the Lower to Middle Jurassic of Morocco: implications for stratal anatomy and lithofacies partitioning.

2017

9 pages; International audience; The Jurassic carbonate platforms of the central High Atlas in Morocco are well known for several high-quality outcrops. In the central High Atlas, there are two complementary locations that offer critical lessons for our understanding of Jurassic carbonate system evolution in extensional basins: a Lower Jurassic high-relief, carbonate platform with steep slopes that developed on the footwall of a rotating fault block in an active half-graben (Djebel Bou Dahar [DBD]) and an upper Lower to Middle Jurassic low-angle prograding carbonate ramp rich in ooids (Amellago ramp [AR]). The DBD and AR outcrops provide superbly exposed, structurally intact, and fully acce…

010506 paleontologyRiftCarbonate platformOutcropEnergy Engineering and Power TechnologyGeology010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentchemistry.chemical_compoundPaleontologyFuel TechnologychemistryGeochemistry and Petrology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesEarth and Planetary Sciences (miscellaneous)CarbonateFault blockHydrocarbon explorationGeology0105 earth and related environmental sciences
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