Search results for "subduction zones"

showing 4 items of 4 documents

Partitioning of nitrogen during melting and recycling in subduction zones and the evolution of atmospheric nitrogen

2019

Abstract The subduction of sediment connects the surface nitrogen cycle to that of the deep Earth. To understand the evolution of nitrogen in the atmosphere, the behavior of nitrogen during the subduction and melting of subducted sediments has to be estimated. This study presents high-pressure experimental measurements of the partitioning of nitrogen during the melting of sediments at sub-arc depths. For quantitative analysis of nitrogen in minerals and glasses, we calibrated the electron probe micro-analyzer on synthetic ammonium feldspar to measure nitrogen concentrations as low as 500 μg g−1. Nitrogen abundances in melt and mica are used together with mass balance calculations to determi…

010504 meteorology & atmospheric sciencesAnalytical chemistrychemistry.chemical_element[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysicsFeldspar01 natural sciencesMantle (geology)Geochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySubduction zonesNitrogen cycle0105 earth and related environmental sciencesMantle metasomatismSubductionGeologyNitrogenPartition coefficientchemistry13. Climate action[SDU]Sciences of the Universe [physics]visual_art[SDE]Environmental Sciencesvisual_art.visual_art_mediumSlabAtmosphere evolutionMicaGeologyNitrogen cycling
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Two-Stage Origin of K-Enrichment in Ultrapotassic Magmatism Simulated by Melting of Experimentally Metasomatized Mantle

2019

The generation of strongly potassic melts in the mantle requires the presence of phlogopite in the melting assemblage, while isotopic and trace element analyses of ultrapotassic rocks frequently indicate the involvement of subducted crustal lithologies in the source. However, phlogopite-free experiments that focus on melting of sedimentary rocks and subsequent hybridization with mantle rocks at pressures of 1&ndash

Peridotitelcsh:Mineralogylcsh:QE351-399.2lamproites010504 meteorology & atmospheric sciencesLithologyultrapotassicTrace elementGeochemistryGeologyUltrapotassic igneous rocksengineering.material010502 geochemistry & geophysicsGeotechnical Engineering and Engineering Geology01 natural sciencesK-enrichmentMantle (geology)MagmatismengineeringPhlogopiteSedimentary rockhigh-pressure experimentssubduction zonesGeology0105 earth and related environmental sciencesMinerals
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Polarity-reversal subduction zone initiation triggered by buoyant plateau obstruction

2022

Abstract Oceanic lithosphere worldwide is younger than ca. 200 Myr, suggesting that it must have been globally recycled by the recurrent formation of new subduction zones since the existence of subduction on Earth. However, postulated subduction zone initiation processes remain difficult to explain in many cases, and the specific geodynamic conditions under which these might occur are still largely unknown. We here use numerical models driven by the internal force balance of a subduction system to better understand the (geo)dynamics governing (intra-oceanic) polarity-reversal subduction zone initiation. This initiation mode assumes that the birth of a new subduction zone could be triggered …

Polarity reversalgeographyPlateaugeography.geographical_feature_categorySubductionnumerical modellingpolarity-reversalNumerical modelsinternal force balanceGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyLithosphereoceanic plateausubduction zone initiationEarth and Planetary Sciences (miscellaneous)Internal forcesPetrologysubduction zonesGeologyEarth and Planetary Science Letters
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Subduction-related structures and geodinamic evolution of SE Sicily-Calabria offshore

2008

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicasubduction zones oceanic structures
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