Search results for "Mantle"

showing 10 items of 322 documents

Evidence of Two-Component Iblean-Like Mantle From 2001-2006 Igneous Products of Mount Etna

2008

Mount Etna Melt inclusions Mantle source
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EVIDENCES OF ENRICHED MANTLE (EM-2) SOURCE CONTRIBUTION TO ETNEAN MAGMAS: A COMPREHENSIVE STUDY ON FLUID AND MELT INCLUSIONS OF 2001-2006 ERUPTIONS

2009

Mt. Etna Fluid inclusions noble gases melt inclusions mantle sources
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Geodynamic inversion to constrain the non-linear rheology of the lithosphere

2015

A common method to determine the strength of the lithosphere is through estimating its effective elastic thickness from the coherence between gravity and topography. This method assumes a priori that the lithosphere is a thin elastic plate floating on a viscous mantle. Whereas this seems to work well with oceanic plates, it has given controversial results in continental collision zones. Usually, continental collisions zones are well-studied areas for which additional geophysical datasets such as receiver functions and seismic tomography exist that constrain the geometry of the lithosphere and often show that it is rather complex. Yet, lithospheric geometry by itself is insufficient to under…

Nonlinear systemGeophysicsRheologyContinental collisionGeochemistry and PetrologyOceanic crustLithosphereSeismic tomographyGeophysicsGeologyMantle (geology)Physics::GeophysicsCoherence (physics)Geophysical Journal International
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Two tissue-specific loci for octopine dehydrogenase in Tapes Decussatus (Bivalvia, Veneridae)

1992

Abstract 1. 1. Octopine dehydrogenase catalyses the reductive condensation of pyruvate and arginine to produce octopine in mollusc tissues. 2. 2. In all Bivalvia species studied to date, a single polymorphic locus, anodally migrating, was demonstrated. 3. 3. We studied, by starch gel electrophoresis, octopine isozymes in Tapes decussatus tissues. 4. 4. A polymorphic anodal form is present in adductor muscle, foot muscle, mantle and gill. 5. 5. A hepatopancreas-specific form, cathodally migrating, is also evident.

OctopinebiologyPhysiologyD-octopine dehydrogenaseDehydrogenaseVeneridaeGeneral MedicineBivalviabiology.organism_classificationBiochemistryIsozymechemistry.chemical_compoundStarch gel electrophoresisBiochemistrychemistryBotanyMantle (mollusc)Molecular BiologyComparative Biochemistry and Physiology Part B: Comparative Biochemistry
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Dehydration of melt inclusions in olivine and implications for the origin of silica-undersaturated island-arc melts

2019

Highlights • New experiments with melt inclusions in olivine at 1200 °C and 300 MPa. • Coupled behavior H2O and SiO2 in inclusions during re-hydration and dehydration. • SiO2 mobility results from formation/destruction of metal vacant olivine. • SiO2-undersaturated arc melt inclusions may originate by dehydration. • New method to assess initial H2O in dehydrated inclusions. Abstract Primary subduction-related magmas build up modern continental crust and counterbalance massive recycling of crustal material into the deep mantle occurring at this tectonic setting. Melt inclusions in Mg-rich olivine are believed to be the best probes of primary subduction-related melts. However, unexpectedly, m…

Olivine010504 meteorology & atmospheric sciencesContinental crustCrustengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)law.inventionGeophysics13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologylawEarth and Planetary Sciences (miscellaneous)engineeringIsland arcCrystallization10. No inequalityPetrologyDissolutionGeology0105 earth and related environmental sciencesMelt inclusionsEarth and Planetary Science Letters
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Melting and dynamic metasomatism of mixed harzburgite + glimmerite mantle source: Implications for the genesis of orogenic potassic magmas

2017

Abstract Tectonically young, orogenic settings are commonly the sites of post-collisional silica-rich ultrapotassic magmas with extreme K2O-contents of up to 9 wt% and K2O/Na2O > 2. Many experimental studies investigating the generation of these melts have concentrated on melting of homogenous phlogopite bearing peridotites, whereas geochemical signatures indicate the involvement of at least two types of source rocks: ultra-depleted and K and trace elements-enriched ones. We report the results of melting experiments at 1–2 GPa of mixed glimmerite and harzburgite, in which these rock types make up two halves each capsule. Melting begins in the glimmerite, and its metasomatic effects on the h…

Olivine010504 meteorology & atmospheric sciencesGeochemistryGeologyengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)Source rockGeochemistry and PetrologyengineeringRock typesPhlogopiteMetasomatismGeology0105 earth and related environmental sciencesChemical Geology
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Modification of the subcontinental mantle beneath East Serbia: Evidence from orthopyroxene-rich xenoliths

2007

Orthopyroxene-rich olivine websterite xenoliths (OWB2) in Palaeogene basanites in East Serbia are mostly composed of tabular low-Al2O3 orthopyroxene (> 70 vol.%, Mg# 85–87) containing tiny Cr spinel inclusions. Orthopyroxene shows a slightly U-shaped primitive mantle-normalized trace element pattern with strong peaks at U and Pb, similar to that of orthopyroxene from normal regional peridotitic mantle. In between the orthopyroxenes are interstitial spaces composed of partially altered olivine (Mg# 85–87), clinopyroxene, Ti-rich spinel, Mg-bearing calcite, K-feldspar, apatite, ilmenite and relicts of a hydrous mineral. Clinopyroxene appears as selvages around orthopyroxene and as coarser euh…

Olivine010504 meteorology & atmospheric sciencesbiologyGeochemistryGeologyengineering.material010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesMantle (geology)Geochemistry and PetrologyWebsteriteengineeringXenolithMetasomatismMaficGeologyLileIlmenite0105 earth and related environmental sciencesLithos
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Detection of a Ca-rich lithology in the Earth's deep (>300 km) convecting mantle

2005

Earth's deep convecting upper mantle is believed to represent a rather homogenous geochemical reservoir of spinel or garnet lherzolite with primitive major element and moderately depleted trace element composition. Only where subduction occurs is this homogeneity disrupted by a suite of rocks ranging from eclogites/garnet pyroxenites (former oceanic crust) to residual harzburgites. In addition to these well documented peridotitic and metabasaltic rocks we have now discovered the presence of a chemically distinct reservoir in the deep convecting upper mantle. In situ structural analyses (micro X-ray diffraction and micro Raman spectroscopy) and three-dimensional trace element mapping (confoc…

OlivineSubductionTrace elementGeochemistryPyroxeneengineering.materialMantle (geology)GeophysicsSpace and Planetary ScienceGeochemistry and PetrologyLithosphereOceanic crustEarth and Planetary Sciences (miscellaneous)engineeringEclogiteGeologyEarth and Planetary Science Letters
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Relationship of Mediterranean type lamproites to large shoshonite volcanoes, Miocene of Lesbos, NE Aegean Sea

2014

Abstract Shoshonites, which are high-K trachyandesitic rocks, are found in many orogenic belts and are commonly of post-collisional origin. The petrogenesis of shoshonites has been widely debated. Small lava flows and dykes of lamproite and related lamproitic rocks of early Miocene age in Lesbos are coeval with voluminous shoshonite volcanoes. Their distinctive petrology and isotope geochemistry provide an exceptional opportunity to assess the petrogenetic relationship between lamproites and shoshonites. The lamproitic rocks contain phenocrysts of forsteritic olivine (as high as Fo93) and clinopyroxene, both with inclusions of chrome spinel (Cr# ~ 0.9 or ~ 0.6) and carbonate melt inclusions…

OlivinebiologyPartial meltingGeochemistryGeologyengineering.materialbiology.organism_classificationMantle (geology)Geochemistry and PetrologyIsotope geochemistryengineeringPhenocrystLileGeologyMelt inclusionsPetrogenesis
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Health-related quality of life data from a phase 3, international, randomized, open-label, multicenter study in patients with previously treated mant…

2017

Mantle cell lymphoma (MCL) is a rare, aggressive, incurable B-cell malignancy. Ibrutinib has been shown to be highly active for patients with relapsed/refractory (R/R) MCL. The RAY trial (MCL3001) was a phase 3, randomized, open-label, multicenter study that compared ibrutinib with temsirolimus in patients with R/R MCL. Active disease is frequently associated with impaired functional status and reduced well-being. Therefore, the current study employed two patient-reported outcome instruments, the Functional Assessment of Cancer Therapy-Lymphoma (FACT-Lym) and the EQ-5D-5L, to assess symptoms, well-being, health status, and health-related quality of life of patients on treatment within the R…

OncologyAdultMaleCancer Researchmedicine.medical_specialtyLymphoma Mantle-CellMalignancy03 medical and health scienceschemistry.chemical_compound0302 clinical medicineRefractoryQuality of lifePiperidinesInternal medicineAntineoplastic Combined Chemotherapy ProtocolsmedicineHumans030212 general & internal medicineDisease burdenAgedNeoplasm StagingAged 80 and overSirolimusbusiness.industryAdenineCancerHematologyMiddle Agedmedicine.diseaseTemsirolimusSurgeryPyrimidinesTreatment OutcomeOncologychemistryDrug Resistance Neoplasm030220 oncology & carcinogenesisIbrutinibRetreatmentQuality of LifePyrazolesMantle cell lymphomaFemalebusinessmedicine.drug
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