Search results for "Tectonics"

showing 10 items of 385 documents

Segmentation and differential post-rift uplift at the Angola margin as recorded by the transform-rifted Benguela and oblique-to-orthogonal-rifted Kwa…

2010

29 pages; International audience; We analyse tectonic and sedimentary field and subsurface data for the Angola onshore margin together with free-air gravity anomaly data for the offshore margin. This enables us to characterize the mode of synrift tectonism inherited from the Precambrian and its impact on the segmentation of the Angola margin. We illustrate that segmentation by the progressive transition from the Benguela transform-rifted margin segment to the oblique-rifted South Kwanza and orthogonal-rifted North Kwanza margin segments. The spatial variation in the intensity of post-rift uplift is demonstrated by the study of a set of geomorphic markers detected in the post-rift succession…

Angola marginStratigraphyPost-rift upliftStructural basinOceanographyNeogene[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyUnconformityPaleontologyEpeirogenic movementGeomorphologyRiftTransform riftingDeep-sea fanOblique riftingGeologyMargin segmentation[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/Tectonics[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsGeomorphic markerEconomic GeologySedimentary rockQuaternaryCenozoicGeology
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Peri-Gondwanan Ordovician arc magmatism in southeastern Ireland and the Isle of Man: Constraints on the timing of Caledonian deformation in Ganderia

2018

The timing of and tectonic controls on Ordovician magmatism and deformation within accreted terranes are key elements in reconstructing the generation of the Caledonian-Appalachian orogen. This pap ...

Arc (geometry)PaleontologyTectonics010504 meteorology & atmospheric sciencesMagmatismOrdovicianGeologyDeformation (meteorology)010502 geochemistry & geophysics01 natural sciencesGeology0105 earth and related environmental sciencesTerraneGSA Bulletin
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The Mediterranean Sea and the Gulf of Cadiz as a natural laboratory for paleotsunami research: Recent advancements

2021

International audience; After the 2004 Indian Ocean (IOT) and the 2011 Tohoku-oki tsunamis, new research in tsunami-related fields was strongly stimulated worldwide and also in the Mediterranean. This research growth yields substantial advancements in tsunami knowledge.Among these advancements is the “Paleotsunami” research that has marked particular progress on the reconstruction of the tsunami history of a region. As an integration of the historical documentation available in the Mediterranean and the Gulf of Cadiz areas, geological and geoarchaeological records provide the insights to define the occurrence, characteristics, and impact of tsunamis of the past. Here, we present the recent …

ArcheologyHigh-resolution studies010504 meteorology & atmospheric sciences010502 geochemistry & geophysicsGeologic record01 natural sciencesNatural (archaeology)Sedimentary structuresPaleontologyMediterranean seaMediterranean Sea[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology14. Life underwaterHoloceneComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryContinental shelfGeologyPaleotsunami depositsCoringBackwash wave13. Climate actionGeneral Earth and Planetary SciencesSubmarine pipelineGeology
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Anisotropic scaling of tectonic stylolites: A fossilized signature of the stress field?

2010

International audience; [1] Vertical stylolites are pressure solution features, which are considered to be caused by horizontal tectonic loading, with the largest principal compressive stress being (sub-) parallel to the Earth's surface. In the present study we analyze the roughness of such tectonic stylolites from two tectonic settings in southern Germany and northeastern Spain, aiming to investigate their scaling properties with respect to the stress during formation. High-resolution laser profilometry was carried out on opened stylolite surfaces of nine samples. These data sets were then analyzed using one-and two-dimensional Fourier power spectral approaches. We found that tectonic styl…

Atmospheric Science010504 meteorology & atmospheric sciences[SDU.STU]Sciences of the Universe [physics]/Earth SciencesSoil ScienceMineralogyGeometryAquatic Science010502 geochemistry & geophysicsOceanography01 natural sciencesPhysics::GeophysicsStress (mechanics)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)AnisotropyScaling0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and Technology[PHYS]Physics [physics]EcologyCauchy stress tensorPaleontologyForestryStress fieldTectonicsGeophysics13. Climate actionSpace and Planetary ScienceStylolitePressure solutionGeologyJournal of Geophysical Research
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Evidence of positive tectonic inversion in the north-central sector of the Sicily Channel (Central Mediterranean)

2016

In order to unravel the tectonic evolution of the north-central sector of the Sicily Channel (Central Mediterranean), a seismo-stratigraphic analysis of single- and multi-channel seismic reflection profiles has been carried out. This allowed to identify, between 20 and 50 km offshore the central-southern coast of Sicily, a ~80-km-long deformation belt, characterized by a set of WNW–ESE to NW–SE fault segments showing a poly-phasic activity. Within this belt, we observed: i) Miocene normal faults reactivated during Zanclean–Piacenzian time by dextral strike-slip motion, as a consequence of the Africa–Europe convergence; ii) releasing and restraining bend geometries forming well-developed pul…

Atmospheric SciencePiacenzian010504 meteorology & atmospheric sciencesSicily ChannelSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleInversion (geology)Structural basin010502 geochemistry & geophysics01 natural sciencesNappePush-up structureCompressive featuresEarth and Planetary Sciences (miscellaneous)Tectonic inversionForeland basinStrike-slip motion0105 earth and related environmental sciencesWater Science and TechnologyAnticlinePush-up structuresCompressive featureTectonicsSinistral and dextralCompressive features; Push-up structures; Seismic stratigraphy; Sicily Channel; Strike-slip motion; Tectonic inversion; Water Science and Technology; Atmospheric Science; Earth and Planetary Sciences (miscellaneous)SeismologyGeologySeismic stratigraphy
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Modeling suggests that oblique extension facilitates rifting and continental break-up

2012

[1] In many cases the initial stage of continental break-up was and is associated with oblique rifting. That includes break-up in the Southern and Equatorial Atlantic, separation from eastern and western Gondwana as well as many recent rift systems, like Gulf of California, Ethiopia Rift and Dead Sea fault. Using a simple analytic mechanical model and advanced numerical, thermomechanical modeling techniques we investigate the influence of oblique extension on the required tectonic force in a three-dimensional setting. While magmatic processes have been already suggested to affect rift evolution, we show that additional mechanisms emerge due to the three-dimensionality of an extensional syst…

Atmospheric Sciencegeographygeography.geographical_feature_categoryRiftEcologyBreak-UpDeformation (mechanics)PaleontologySoil ScienceOblique caseForestryAquatic ScienceFault (geology)OceanographyGondwanaTectonicsGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Rift zoneSeismologyGeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Solid Earth
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Devonian to Permian plate tectonic cycle of the Paleo-Tethys Orogen in southwest China (II): Insights from zircon ages of ophiolites, arc/back-arc as…

2009

Abstract New SHRIMP zircon ages for ophiolites, arc/back-arc assemblages and within-plate igneous rocks constrain the evolution of the Paleo-Tethys Orogen of southwest China. Ophiolites represent remnants of the Paleo-Tethys ocean, which was divided by the Simao terrane into two tracts, the main ocean in the west (current position) and a branch in the east. The main ocean has been inferred to originate from Gondwana break-up in the Early Devonian, and the heritage is preserved as the Changning-Menglian ophiolite (SSZ-type). The oceanic branch is represented by the Ailaoshan (NMORB-type)–Jinshajinag (EMORB-type) ophiolites. Zircons from a diabase and a plagiogranite of the Ailaoshan ophiolit…

Basaltgeographygeography.geographical_feature_categoryGabbroVolcanic arcLarge igneous provinceGeochemistryGeologyOphioliteVolcanic rockPlate tectonicsGeochemistry and PetrologyGeologyZirconLithos
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The Lefkada barrier and beachrock system (NW Greece) — Controls on coastal evolution and the significance of extreme wave events

2012

Abstract The Lefkada–Preveza coastal zone, NW Greece, is characterised by an active barrier system and related extensive beachrock sequences. Besides the gradual coastal processes of longshore drift and spit evolution, the presence of active tectonics and the occurrence of tsunamis have been documented in previous studies and are part of the coastal geomorphological system. In this paper, we present the results of detailed multi-proxy sedimentological and geomorphological investigations carried out along the northern part of the barrier system and in back-beach positions. Our findings suggest that extreme wave events contributed to coastal and environmental changes and involved temporary br…

BeachrockLongshore driftTectonicsOceanographyCoastal zoneLittoral zoneSedimentary rockGeomorphologyGeologyNatural (archaeology)Earth-Surface ProcessesGeomorphology
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Millstones as indicators of relative sea-level changes in northern Sicily and southern Calabria coastlines, Italy

2011

Abstract New data are presented for late Holocene relative sea-level changes in two coastal sites of Sicily and Calabria, southern Italy. Reconstructions are based on precise measurements of submerged archaeological remains that are valuable indicators of past sea-level position. The archaeological remains are millstone quarries carved on sandstone coastal rocks and nowadays partially submerged which, to the authors’ knowledge, are used for the first time as sea-level markers. Millstones of similar typology are located on the coast of Capo d’Orlando (northern Sicily) and Capo dell’Armi (southern Calabria). When the archeologically-based sea-level position is compared with the shoreline elev…

BeachrockShoregeographygeography.geographical_feature_categoryHolocenePleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaElevationtectonic movements; sea level changes; Holocene;tectonic movementArchaeologyMillstoneTectonicsgeoarcheologyPhysical geographysea level changeSicily and CalabriaSea levelHoloceneGeologyrelative sea-level changeEarth-Surface Processes
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2001

The roles of volume loss, coaxial versus noncoaxial flow, and blueschist exhumation in subduction-related accretionary wedges are still poorly understood. In our study at Leech Lake Mountain in the Eastern belt of the Franciscan subduction complex, we focus on these subjects. In the specific example of the Franciscan, the tectonic significance of the boundary between the Eastern and Central belts remains controversial. The Leech Lake Mountain area in northern California is situated immediately above this boundary and, therefore, appears to be of crucial importance for understanding aspects of the tectonic evolution of the Franciscan. The structural development at Leech Lake Mountain is char…

BlueschistPaleontologyTectonicsSubductionMetamorphic rockMetamorphismCleavage (geology)GeologyForearcSeismologyGeologyTerraneGeological Society of America Bulletin
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