Search results for "NEI"

showing 10 items of 2245 documents

CCDC 262732: Experimental Crystal Structure Determination

2005

Related Article: C.Faulmann, S.Dorbes, B.G.de Bonneval, G.Molnar, A.Bousseksou, C.J.Gomez-Garcia, E.Coronado, L.Valade|2005|Eur.J.Inorg.Chem.||3261|doi:10.1002/ejic.200500125

(4-azaheptamethylene-17-bis(salicylideneiminate))-(1-(pyridine-4-yl)-2-(N-methylpyrrol-2-yl)ethene)-iron(iii) bis(13-dithiole-2-thione-45-dithiolato)-nickelSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 262731: Experimental Crystal Structure Determination

2005

Related Article: C.Faulmann, S.Dorbes, B.G.de Bonneval, G.Molnar, A.Bousseksou, C.J.Gomez-Garcia, E.Coronado, L.Valade|2005|Eur.J.Inorg.Chem.||3261|doi:10.1002/ejic.200500125

(4-azaheptamethylene-17-bis(salicylideneiminate))-(1-(pyridine-4-yl)-2-(N-methylpyrrol-2-yl)ethene)-iron(iii) bis(13-dithiole-2-thione-45-dithiolato)-nickelSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 262734: Experimental Crystal Structure Determination

2005

Related Article: C.Faulmann, S.Dorbes, B.G.de Bonneval, G.Molnar, A.Bousseksou, C.J.Gomez-Garcia, E.Coronado, L.Valade|2005|Eur.J.Inorg.Chem.||3261|doi:10.1002/ejic.200500125

(4-azaheptamethylene-17-bis(salicylideneiminate))-(1-(pyridine-4-yl)-2-(N-methylpyrrol-2-yl)ethene)-iron(iii) bis(13-dithiole-2-thione-45-dithiolato)-nickelSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 262730: Experimental Crystal Structure Determination

2005

Related Article: C.Faulmann, S.Dorbes, B.G.de Bonneval, G.Molnar, A.Bousseksou, C.J.Gomez-Garcia, E.Coronado, L.Valade|2005|Eur.J.Inorg.Chem.||3261|doi:10.1002/ejic.200500125

(4-azaheptamethylene-17-bis(salicylideneiminate))-(1-(pyridine-4-yl)-2-(N-methylpyrrol-2-yl)ethene)-iron(iii) bis(13-dithiole-2-thione-45-dithiolato)-nickelSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 645212: Experimental Crystal Structure Determination

2009

Related Article: D.Mal, R.Sen, C.Adhikary, Y.Miyashita, K.-I.Okamoto, A.Bhattacharjee, P.Gutlich, S.Koner|2008|J.Coord.Chem.|61|3486|doi:10.1080/00958970802072773

(mu~2~-Dicyanamide)-bis(1-(N-salicylideneimino)-2-(NN-dimethylamino)ethane)-di-copper(ii) perchlorateSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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SARS-CoV-2 vaccine response and rate of breakthrough infection in patients with hematological disorders

2022

Abstract Background The clinical efficacy of SARS-CoV-2 vaccines according to antibody response in immunosuppressed patients such as hematological patients has not yet been established. Patients and methods A prospective multicenter registry-based cohort study conducted from December 2020 to December 2021 by the Spanish transplant and cell therapy group was used to analyze the relationship of antibody response at 3–6 weeks after full vaccination (2 doses) with breakthrough SARS-CoV-2 infection in 1394 patients with hematological disorders. Results At a median follow-up of 165 days after complete immunization, 37 out of 1394 (2.6%) developed breakthrough SARS-CoV-2 infection at median of 77 …

*Pfizer-BioNTech BNT162b2Cancer ResearchCOVID-19 Vaccines*Hematological malignanciesAutologous stem cell transplantationAntibodies ViralBreakthrough SARS-CoV-2 infectionModerna mRNA-1273Cohort StudiesHematological malignancies*Moderna mRNA-1273Correlates of protection*VaccineHumansProspective StudiesVacunacióPfizer-BioNTech BNT162b2Molecular BiologyBNT162 Vaccine*Immunocompromised patients*Correlates of protectionSARS-CoV-2VaccinationHematologic diseasesCOVID-19Hematology*Breakthrough SARS-CoV-2 infectionHematologic DiseasesSARS-CoV-2 vaccinesAllogeneic stem cell transplantationVirusOncologyMalalties hematològiquesImmunocompromised patients*SARS-CoV-2 vaccines*Autologous stem cell transplantation*COVID-19Vaccine*Allogeneic stem cell transplantationJournal of Hematology & Oncology
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Barrier inhomogeneity in vertical Schottky diodes on free standing gallium nitride

2019

Abstract In this paper, the electrical behavior of a Ni/Au Schottky barrier on free standing GaN has been studied employing a variety of techniques and correlated with the material and interface quality. The temperature dependence of the ideality factor (n) and of the Schottky barrier height (ΦB) revealed a spatial inhomogeneity of the barrier. This behavior has been described by means of the Tung's model on inhomogeneous Schottky barriers. The origin of the barrier inhomogeneity can be likely associated to the surface quality of the GaN epilayer or to microstructure of the Ni/GaN interface.

010302 applied physicsMaterials scienceCondensed matter physicsMechanical EngineeringSchottky barrierSchottky diodeGallium nitride02 engineering and technology021001 nanoscience & nanotechnologyCondensed Matter PhysicsMicrostructure01 natural sciencesFree standing GaNchemistry.chemical_compoundQuality (physics)chemistryMechanics of MaterialsNi/GaN interface0103 physical sciencesGeneral Materials ScienceBarrier spatial inhomogeneity0210 nano-technologySchottky barrier
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Subduction or sagduction? Ambiguity in constraining the origin of ultramafic–mafic bodies in the Archean crust of NW Scotland

2016

Abstract The Lewisian Complex of NW Scotland is a fragment of the North Atlantic Craton. It comprises mostly Archean tonalite–trondhjemite–granodiorite (TTG) orthogneisses that were variably metamorphosed and reworked in the late Neoarchean to Paleoproterozoic. Within the granulite facies central region of the mainland Lewisian Complex, discontinuous belts composed of ultramafic–mafic rocks and structurally overlying garnet–biotite gneiss (brown gneiss) are spatially associated with steeply-inclined amphibolite facies shear zones that have been interpreted as terrane boundaries. Interpretation of the primary chemical composition of these rocks is complicated by partial melting and melt loss…

010504 meteorology & atmospheric sciencesArcheanGeochemistryMetamorphismGeology010502 geochemistry & geophysicsGranulite01 natural sciencesLewisian complexGeochemistry and PetrologyUltramafic rockPetrologyProtolithGeologyMetamorphic facies0105 earth and related environmental sciencesGneissPrecambrian Research
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Effects of natural radiation damage on back-scattered electron images of single crystals of minerals

2006

Generally, it has been assumed that signal intensity variations in back-scattered electron (BSE) images of minerals are mainly controlled by chemical heterogeneity. This is especially true for images of single crystals, where effects of different crystal orientations with respect to the incident beam on the observed BSE are excluded. In contrast, we show that local variations of the structural state within single-crystals (i.e., degree of lattice order or lattice imperfectness) may also have dramatic effects on the back-scattering of electrons. As an example, we present BSE images of single-crystals of natural zircon, ZrSiO 4 , whose intensity patterns are predominantly controlled by struct…

010504 meteorology & atmospheric sciencesCondensed matter physicsChemistryMineralogyElectron010502 geochemistry & geophysics01 natural sciencesStructural heterogeneityCrystalGeophysicsGeochemistry and PetrologyRadiation damageIncident beamSignal intensity0105 earth and related environmental sciencesZirconChemical heterogeneityAmerican Mineralogist
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Kinematics, deformation partitioning and late Variscan magmatism in the Agly massif, Eastern Pyrenees, France

2020

International audience; In order to constrain the finite deformation pattern of the Variscan basement of the Agly massif, a detailed structural analysis over the whole Agly massif was performed. Our investigation combined geological mapping, reappraisal of published and unpublished data completed with our own structural work. Results are provided in the form of new tectonic maps and series of regional cross-sections through the Agly massif. At variance from previous studies, we identified three deformation fabrics named D1, D2 and D3. The D1 deformation is only relictual and characterized by a broadly northwest-southeast striking and eastward dipping foliation without any clear mineral and …

010504 meteorology & atmospheric sciencesCrustal thinningPlutonGneiss domeMetamorphism[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesTranspressionLineationPetrologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesVariscan orogengeographygeography.geographical_feature_categorylcsh:QE1-996.5GeologyMassifPlutonismAgly Massiflcsh:GeologySinistral and dextral[SDU]Sciences of the Universe [physics]eastern pyreneesShear zoneGeology
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