Search results for "Crust"

showing 10 items of 599 documents

The emissions of CO2 and other volatiles from the world’s subaerial volcanoes

2019

AbstractVolcanoes are the main pathway to the surface for volatiles that are stored within the Earth. Carbon dioxide (CO2) is of particular interest because of its potential for climate forcing. Understanding the balance of CO2 that is transferred from the Earth’s surface to the Earth’s interior, hinges on accurate quantification of the long-term emissions of volcanic CO2 to the atmosphere. Here we present an updated evaluation of the world’s volcanic CO2 emissions that takes advantage of recent improvements in satellite-based monitoring of sulfur dioxide, the establishment of ground-based networks for semi-continuous CO2-SO2 gas sensing and a new approach to estimate key volcanic gas param…

geographyMultidisciplinarygeography.geographical_feature_category010504 meteorology & atmospheric sciencesSubductionEarth sciencelcsh:Rlcsh:MedicineCrustRadiative forcing010502 geochemistry & geophysics01 natural sciencesMantle (geology)chemistry.chemical_compoundchemistryVolcanovolcanic gasesSubaerialCarbon dioxidelcsh:QCO2lcsh:ScienceSulfur dioxide0105 earth and related environmental sciences
researchProduct

Solution and recrystallisation processes and associated landforms in gypsum outcrops of Sicily

2003

Abstract Four small areas of Messinian (Upper Miocene) age gypsum, outcropping in western Sicily, are described. Messinian age evaporites are found in Sicily over a 1000-km 2 area. Here, gypsum outcrops extensively as a consequence of soil erosion induced by human impact. Geomorphological maps show how the rocky surfaces are characterized by a wide range of forms. There are large, medium, small, and microsized forms, which can be identified as belonging to different morphotypes. The morphotypes can be classified into two main categories: those that originated by solution and those that originated through recrystallisation. Four areas, illustrated by geomorphological maps, were specifically …

geographyRecrystallization (geology)geography.geographical_feature_categoryGypsumEvaporiteOutcropGeochemistryMineralogyCrustWeatheringengineering.materialKarstengineeringSedimentary rockGeologyEarth-Surface ProcessesGeomorphology
researchProduct

Structure, evolution, and dynamics of the Norwegian-Greenland Sea in the Blue Road Geotraverse area

1981

The orogeny of the Scandinavian and Greenland Caledonides is shortly reviewed, and a structural sketch map of the Scandinavian Caledonide part of the Geotraverse is presented. Post-Caledonian rifting episodes prior to the formation of the North Atlantic Ocean are briefly discussed, as well as the opening of the northern North Atlantic Ocean and its spreading rates. Computations of density models carried out on the basis of the Simplex-Algorithm which allows a least-squares solution under certain constraints show clearly a Moho-depression beneath the Caledonides and a comparatively thick oceanic crust in the Norwegian Sea. The transition zone oceanic continental crust has a complex structure…

geographyRiftgeography.geographical_feature_categoryPlateauContinental crustOrogenyEscarpmentPaleontologyOceanographyOceanic crustTransition zoneGeneral Earth and Planetary SciencesStructural geologyGeologyGeologische Rundschau
researchProduct

High-temperature metamorphism and crustal melting at ca. 3.2 Ga in the eastern Kaapvaal craton, southern Africa

2018

Abstract The question of whether high-grade metamorphism and crustal melting in the early Archaean were associated with modern-style plate tectonics is a major issue in unravelling early Earth crustal evolution, and the eastern Kaapvaal craton has featured prominently in this debate. We discuss a major ca. 3.2 Ga tectono-magmatic-metamorphic event in the Ancient Gneiss Complex (AGC) of Swaziland, a multiply deformed medium- to high-grade terrane in the eastern Kaapvaal craton consisting of 3.66–3.20 Ga granitoid gneisses and infolded greenstone remnants, metasedimentary assemblages and mafic dykes. We report on a 3.2 Ga granulite-facies assemblage in a metagabbro of the AGC of central Swazi…

geographyUnderplatinggeography.geographical_feature_categoryP-T reconstruction010504 meteorology & atmospheric sciencesArcheanGeochemistryMetamorphismGeologyCrustKaapvaal craton010502 geochemistry & geophysicsGrey gneiss01 natural sciencesMesoarchaeanCratonZircon ageHf-Nd isotopesGeochemistry and PetrologySwazilandMaficMetamorphic faciesGeology0105 earth and related environmental sciencesTerranePrecambrian Research
researchProduct

Deep structural setting of the North American-Caribbean plate boundary in eastern Guatemala

2009

Se presenta un modelo bidimensional de gravedad para determinar la estructura en profundidad del sistema de fallas lateral-izquierda de Motagua-Polochic, que son parte del límite de las placas América del Norte y del Caribe. Estos elementos tectónicos, sismicamente activos, atraviesan oeste-este la región de Guatemala y se sobreponen a una línea de sutura donde afloran cuerpos ophiolíticos. En las principales zonas de desplazamiento de las fallas se han desarrollado cuencas de pull-apart y regiones de restricción (push-up). El análisis estructural de algunas de estas fallas, situadas a lo largo del valle Izabal y del valle Motagua, en combinación con los datos obtenidos del satélite, ha per…

geographyeducation.field_of_studygeography.geographical_feature_categoryLineamentSettore GEO/03 - Geologia StrutturalePopulationMotagua transform systemsEastern Guatemaladeep crustal structurePolochic-Motagua transform systemsStructural basinSedimentary basinTectonicsPlate tectonicsgravity modelingGeneral EnergyGeophysicsPolochicCiencias de la TierraSuture (geology)Eastern Guatemala Polochic-Motagua transform system gravity modelling deep crustal structure.educationGeologySeismologyBouguer anomalyGeofísica Internacional
researchProduct

Reply to comment by Ngako and Njonfang on “The Adamawa-Yade domain, a piece of Archaean crust in the Neoproterozoic Central African Orogenic belt (Ba…

2018

Abstract V. Ngako and E. Njonfang addressed in their comment an interesting and debated issue about the collision geodynamics of the Pan-African Central African Orogenic Belt (CAOB) in Cameroon. However, the reason for this comment is still not clear to us since it mainly deals with issues far away from the scope of our study, namely, the pre-collisional set up of the belt. The comment raises two main points – the reworking process during plate collision and the Pan-African strain pattern – not discussed in our paper for the simple reason that it was not our goal and because our data set does not even allow such discussion. Having said that, the comment gives us the opportunity to clarify o…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesArchean[SDU.STU]Sciences of the Universe [physics]/Earth SciencesGeologyCrustGeodynamics010502 geochemistry & geophysics01 natural sciencesDomain (software engineering)PrecambrianPaleontologyCratonStrain patternGeochemistry and Petrology[SDU]Sciences of the Universe [physics]GeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences
researchProduct

Quantifying the impact of mechanical layering and underthrusting on the dynamics of the modern India-Asia collisional system with 3-D numerical models

2014

The impact of mechanical layering and the strength of the Indian lower crust on the dynamics of the modern India-Asia collisional system are studied using 3-D thermomechanical modeling. The model includes an Indian oceanic domain, Indian continental domain, and an Asian continental domain. Each domain consists of four layers: upper/lower crust, and upper/lower lithospheric mantle. The Tarim and Sichuan Basins are modeled as effectively rigid blocks and the Quetta-Chaman and Sagaing strike-slip faults as vertical weak zones. The geometry, densities, and viscosities are constrained by geophysical data sets (CRUST2.0, gravity, and seismology). Both static (no horizontal movement of model bound…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesContinental collisionCrustGeophysicsFault (geology)010502 geochemistry & geophysicsOverburden pressure01 natural sciencesOverpressureTectonicsGeophysics13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyLithosphereEarth and Planetary Sciences (miscellaneous)LayeringGeology0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
researchProduct

Eastern Ancient Terrane of the North China Craton

2016

Based on the spatial distribution of ancient rocks and zircons, three ancient terranee older than ca. 2.6 Ga have recently been identified in the North China Craton, namely the Eastern, Southern, and Central Ancient Terranee. The Eastern Ancient Terrane is the best studied and understood of the three ancient terranes. It has a long geological history back to ca. 3.8 Ga ago and includes the areas of Anshan-Benxi, eastern Hebei, eastern Shandong and western Shandong. In Anshan-Benxi, several different types of 3.8 Ga rocks were discovered together with 3.1–3.7 Ga rocks, whereas 2.9–3.0 Ga K-rich granites and 2.5 Ga syenogranite occur on larger scales. In eastern Hebei, 3.0–3.4 Ga rocks and ol…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesContinental crustArcheanCrustal recyclingGeology010502 geochemistry & geophysics01 natural sciencesMantle (geology)CratonPaleontologySyenograniteGeology0105 earth and related environmental sciencesZirconTerraneActa Geologica Sinica - English Edition
researchProduct

The Adamawa-Yadé domain, a piece of Archaean crust in the Neoproterozoic Central African Orogenic belt (Bafia area, Cameroon)

2017

Abstract New field observations, ages and geochemical data are presented for the Adamawa-Yade domain, forming part of Central African Orogenic Belt in Cameroon. This belt delineates the northern margin of the Congo craton and is part of the Braziliano/Pan-African orogenic system, which was formed during amalgamation of the West Gondwana continent at the end of the Neoproterozoic. U–Pb dating indicates that the protoliths of some orthogneisses from the Adamawa-Yade domain were emplaced during three distinct periods. Tonalite-Trondhjemite-Granodiorite (TTG) suites in the Makenene area intruded at ca. 3.0–2.5 Ga, and were affected by partial melting at ca. 2.08–2.07 Ga, during the Eburnean oro…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesContinental crustArcheanGeochemistry[SDU.STU]Sciences of the Universe [physics]/Earth SciencesGeologyCrustOrogeny15. Life on land010502 geochemistry & geophysics01 natural sciencesGondwanaCratonContinental marginGeochemistry and Petrology[SDU]Sciences of the Universe [physics]PetrologyProtolithGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences
researchProduct

Zircon ages, geochemistry and Nd isotopic systematics for the Palaeoproterozoic 2.3–1.8 Ga Kuilyu Complex, East Kyrgyzstan – The oldest continental b…

2017

Abstract Precambrian microcontinents represent key tectonic units in the accretionary collages of the western Central Asian Orogenic Belt (CAOB), and their geological history is reasonably well established since the Mesoproterozoic but remains weakly constrained for older epochs due to a scarcity of exposed Palaeoproterozoic and Archaean rocks. Early Precambrian rocks were previously reported from several metamorphic complexes in the Kyrgyz Tianshan orogenic belt, mainly based on multigrain conventional zircon dating, but the present study only confirmed such rocks at one site, namely in the Kuilyu Complex of eastern Kyrgyzstan. New single grain SHRIMP II zircon ages, geochemical data, and …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesContinental crustGeochemistryMetamorphismGeology010502 geochemistry & geophysics01 natural sciencesDioriteCratonPrecambrianProtolithGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTerraneZirconJournal of Asian Earth Sciences
researchProduct