0000000000368028

AUTHOR

Olivier Fabbri

showing 2 related works from this author

Variation in structural styles within fold-and-thrust belts: Insights from field mapping, cross-sections balancing, and 2D-kinematic modelling in the…

2021

Abstract Fold-and-thrust belts developed above an evaporite decollement host structural traps where geofluids, including hydrocarbons, can accumulate. A valid and accurate structural style intepretation is therefore crucial to understand the three-dimensional geometries in the subsurface, in order to better model geofluid reservoirs and to increase success during exploration. Here, we present a multidisciplinary approach to unravel the subsurface structural styles of the Jura fold-and-thrust belt (eastern France), combining geological mapping, from regional to outcrop scale, with cross-section balancing and 2D-kinematic forward modelling. Results show that the Jura fold-and-thrust belt is c…

[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsDécollementgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesEvaporiteOutcropGeologyFold (geology)010502 geochemistry & geophysicsGeologic map01 natural sciencesThrust tectonicsFold and thrust beltSedimentary rockPetrologyComputingMilieux_MISCELLANEOUSGeology0105 earth and related environmental sciencesJournal of Structural Geology
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U-Pb dating of middle Eocene-middle Pleistocene multiple tectonic pulses in the Alpine foreland

2021

Foreland fold-and-thrust belts record long-lived tectonic-sedimentary activity, from passive margin sedimentation, flexuring, and further involvement into wedge accretion ahead of an advancing orogen. Therefore, dating fault activity is fundamental for plate movement reconstruction, resource exploration, or earthquake hazard assessment. Here, we report U-Pb ages of syntectonic calcite mineralizations from four thrusts and three tear faults sampled, at the regional scale, across the Jura fold-and-thrust belt in the northwestern Alpine foreland (eastern France). Four regional tectonic phases are recognized in the middle Eocene-middle Pleistocene interval: (1) pre-orogenic faulting at 44.7&thi…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesContinental collisionFault (geology)010502 geochemistry & geophysics01 natural sciencesTectonicsPaleontologyPlate tectonicsPassive marginForebulgeAccretion (geology)human activitiesForeland basinGeology0105 earth and related environmental sciences
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