Search results for "trama"

showing 10 items of 100 documents

New evidence of mantle heterogeneity beneath the Hyblean Plateau (southeast Sicily, Italy) as inferred from noble gases and geochemistry of ultramafi…

2012

Abstract We analyzed major and trace elements, Sr and Nd isotopes in ultramafic xenoliths in Miocenic age Hyblean diatremes, along with noble gases of CO2-rich fluid inclusions hosted in the same products. The xenoliths consist of peridotites and pyroxenites, which are considered to be derived from the upper mantle. Although the mineral assemblage of peridotites and their whole-rock abundance of major elements (e.g., Al2O3 = 0.8–1.5 wt.%, TiO2 = 0.03–0.08 wt.%) suggest a residual character of the mantle, a moderate enrichment in some incompatible elements (e.g., LaN/YbN = 9–14) highlights the presence of cryptic metasomatic events. In this context a deep silicate liquid is considered the me…

XenolithsPeridotiteIncompatible elementHyblean PlateauGeochemistryGeologyFluid inclusionMantle (geology)Noble gaMetasomatismGeochemistry and PetrologyUltramafic rockNoble GasXenolithXenolithFluid inclusionsMantleMetasomatismMaficXenoliths; Mantle; Noble GasGeologyLithos
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Cambrian–Ordovician magmatism of the Ikh-Mongol Arc System exemplified by the Khantaishir Magmatic Complex (Lake Zone, south–central Mongolia)

2018

Abstract The Khantaishir Magmatic Complex (KMC) (south–central Mongolia) exposes a section of a magmatic system consisting of deep crustal, ultramafic cumulates (coarse-grained Amp gabbros and hornblendites; c. 0.35–0.5 GPa) to shallower crustal levels dominated by Amp–Bt tonalites ( c. 0.1–0.2 GPa). The magmatic rocks were emplaced during most of the Cambrian ( c. 538–495 Ma) and are mostly geochemically primitive (Mg# ~ 50), Na-rich and metaluminous. The (normal-) calc-alkaline signature and characteristic trace-element enrichment in hydrous-fluid mobile large-ion lithophile elements (LILE) relative to high-field strength elements (HFSE) suggest an origin within a magmatic arc. Multiple i…

[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsFractional crystallization (geology)010504 meteorology & atmospheric sciencesContinental crustPartial meltingGeochemistryGeology15. Life on land010502 geochemistry & geophysics01 natural sciencesUltramafic rockTonianArc systemIsland arcGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesZircon
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Participation and performance trends in multistage ultramarathons--the 'Marathon des Sables' 2003-2012

2012

International audience; BackgroundThe purpose of this study was to investigate participation and performance changes in the multistage ultramarathon 'Marathon des Sables' from 2003 to 2012.MethodsParticipation and performance trends in the four- or six-stage running event covering approximately 250 km were analyzed with special emphasis on the nationality and age of the athletes. The relations between gender, age, and nationality of finishers and performance were investigated using regression analyses and analysis of variance.ResultsBetween 2003 and 2012, a number of 7,275 athletes with 938 women (12.9%) and 6,337 men (87.1%) finished the Marathon des Sables. The finisher rate in both women…

[SDV.MHEP.PHY] Life Sciences [q-bio]/Human health and pathology/Tissues and Organs [q-bio.TO][ SDV.MHEP.PHY ] Life Sciences [q-bio]/Human health and pathology/Tissues and Organs [q-bio.TO][SDV.MHEP.PHY]Life Sciences [q-bio]/Human health and pathology/Tissues and Organs [q-bio.TO]Gender differenceNationalityUltramarathonPerformance trends
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Ca-rich carbonates associated with ultrabasic-ultramafic melts. Carbonatite or limestone xenoliths? A case study from the late Miocene Morron de Vill…

2016

The volcanic products of the late Miocene Morron de Villamayor volcano (Calatrava Volcanic Field, central Spain) are known for being one of the few outcrops of leucitites in the entire circum-Mediterranean area. These rocks are important because aragonite of mantle origin has been reported as inclusion in olivine macrocrysts. We use petrographic observations, mineral compositions, as well as oxygen and carbon isotope ratios coupled with experimental petrology to understand the origin of carbonate phase in these olivine-phyric rocks. Groundmass and macrocryst olivines range from δ18OVSMOW of +4.8‰, typical of mantle olivine values, to +7.4‰, indicating contamination by sedimentary carbonate.…

alkali basalts010504 meteorology & atmospheric sciencesGeochemistrySkarnMediterraneanengineering.material010502 geochemistry & geophysics01 natural sciencespetrologygeochemistry; petrology; carbonate; carbonatite; olivine; mantle; alkaline; Spain; Cenozoic; MagmatismPetrographychemistry.chemical_compoundcarbonateGeochemistry and PetrologyUltramafic rockolivineNeogene volcanism0105 earth and related environmental sciencesgeochemistryPeridotiteOlivineCenozoicAragoniteMagmatismcarbonatitechemistry13. Climate actionSpainCarbonatiteengineeringCarbonatealkalineGeologymantle
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Verschiedene Opioide beim kardiovaskul�ren Risikopatienten

1994

Efficient analgesia may be the major objective in the cardiovascular risk patient following myocardial infarction, acute occlusion of peripheral vessels, or dissection/perforation of major abdominal vessels. It was the purpose of the study to investigate the haemodynamic and respiratory side effects of eight different opioids in 57 circulatory risk patients prior to major vascular surgery. Methods. Patients were randomly allocated to eight groups, each receiving a different opioid within a clinical, equipotent dose range (buprenorphine, fentanyl, morphine, nalbuphine, pentazocine, pethidine, tramadol, alfentanil). A complete haemodynamic and blood gas status was obtained prior to as well as…

business.industryGeneral MedicineNalbuphineFentanylPethidineAnesthesiology and Pain Medicinemedicine.anatomical_structurePentazocineAnesthesiaVascular resistanceMedicineTramadolAlfentanilbusinessPulmonary wedge pressuremedicine.drugDer Anaesthesist
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FableAnimals from the ClassicalTradition in La Gran Conquista deUltramar

2021

espanolLa cronica titulada La Gran Conquista de Ultramar encierra una riqueza literaria mayor de lo que se esperaria para dicho genero. La presente contribucion examina algunos casos de insercion de elementos propios de la fabula de animales y de la narracion de corte antropologico, ambos dentro de la tradicion clasica. EnglishThe chronicle entitled La Gran Conquista de Ultramar brings up a much more rich literary samplethan expected because of its genre. Our contribution considers theinsertion ofelements taken from the animal fable and the anthropological narration, both within the Classical tradition.

cuento maravillosoLiteratura fantásticaAnimales literariosLiteraturafábulacuento popularAnimals Aspectes simbòlicsCrónicatradición clásicaGran conquista de Ultramar
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Single zircon ages for felsic to intermediate rocks from the Pietersburg and Giyani greenstone belts and bordering granitoid orthogneisses, northern …

2000

Abstract Previous models for the temporal evolution of greenstone belts and surrounding granitoid gneisses in the northern Kaapvaal Craton can be revised on the basis of new single zircon ages, obtained by conventional UPb dating and PbPb evaporation. In the Pietersburg greenstone belt, zircons from a metaquartz porphyry of the Ysterberg Formation yielded an age of 2949.7±0.2 Ma, while a granite intruding the greenstones, and deformed together with them, has an age of 2853 + 19/−18 Ma. These data show felsic volcanism in this belt to have been coeval with felsic volcanism in the Murchison belt farther east, and the date of ∼2853 Ma provides an older age limit for deformation in the region…

geographyFelsicgeography.geographical_feature_categoryGeochemistryGeologyGreenstone beltCratonBasement (geology)Ultramafic rockMaficPetrologyGeologyEarth-Surface ProcessesGneissZirconJournal of African Earth Sciences
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The Wadi Onib Mafic-Ultramafic Complex: A Neoproterozoic Supra-Subduction Zone Ophiolite in the Northern Red Sea Hills of the Sudan

2004

Publisher Summary The Wadi Onib mafic–ultramafic complex represents the best preserved, though tectonically dismembered, Neoproterozoic (Pan-African) ophiolite in the northern Red Sea Hills of the Sudan. Arabian–Nubian shield (ANS) is the northern continuation of the Mozambique belt and, together, they have been referred to as the East African Orogen (EAO). The Wadi Onib mafic—ultramafic complex constitutes one of the best preserved, though tectonically fragmented, ophiolitic sequence within the ANS and makes up the major part of the prominent, southwest to northeast oriented Onib–Sol Hamed suture. An improved understanding of the composition and history of this complex has important region…

geographyPillow lavageography.geographical_feature_categoryUltramafic rockFaciesGeochemistrySuture (geology)MaficMozambique BeltOphioliteGeologyWadi
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Characterization, provenance, and tectonic setting of Fig Tree greywackes from the Archaean Barberton Greenstone Belt, South Africa

1999

Abstract In this study, mineralogical and geochemical data, as well as Sr and Nd isotopic compositions of early Archaean greywackes from the Fig Tree Group are presented to provide further information about the evolution of the Barberton Greenstone Belt (BGB) of the Kaapvaal Craton, South Africa. The chemical data on the collected greywackes from the BGB suggest limited chemical modification of the source rocks. The Eu/Eu * anomaly is negative with an average value of 0.76 which is slightly higher than that of Eu-depleted crustal rocks (0.65). High Cr and Ni concentrations and a Cr/Ni ratio of about 1.6 indicate derivation from ultramafic sources without fractionation. Although rounded zirc…

geographyProvenancegeography.geographical_feature_categoryFelsicStratigraphyArcheanGeochemistryGeologyGreenstone beltCratonUltramafic rockIsland arcSiliciclasticGeologySedimentary Geology
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Xenoliths from the sub-volcanic lithosphere of Mt Taranaki, New Zealand

2010

Abstract Mount Taranaki is located 140 km west of the Taupo Volcanic Zone and represents the most westerly expression of subduction-related volcanism on the North Island of New Zealand. Taranaki is a predominantly high-K arc volcano but compositions range from basaltic andesite to andesite with minor dacite and basalt. The sub-volcanic basement under Taranaki is thought to comprise calc–alkaline plutonic and metamorphic rocks of the Median Batholith, overlain by a sequence of Cretaceous and Tertiary sediments. Taranaki lavas contain abundant xenoliths that represent samples of the upper to lower crust beneath the volcano. The xenolith suite has been initially organised into six groups based…

geographygeography.geographical_feature_categoryAndesiteGeochemistryTaranaki BasinVolcanic rockIgneous rockGeophysicsBasaltic andesiteGeochemistry and PetrologyBatholithUltramafic rockXenolithPetrologyGeologyJournal of Volcanology and Geothermal Research
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