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  • 11
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Journal of Physics and Chemistry of Solids 43 (1982), S. 1103-1109 
    ISSN: 0022-3697
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 12
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The 1981 French–Chinese expedition to Tibet focused on the Lhasa block, extending earlier coverage 400 km north of the Tsangpo suture. The Lhasa block stood between 10 and 15° N latitude over most of the Upper Cretaceous and Eocene and, if Gondwanian in origin, had detached from Gondwana ...
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  • 13
    ISSN: 1432-0819
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract There are two rifts zones in the Republic of Djibuti: the active Asal rift (birthplace of the Ardoukôba basaltic volcano in 1978) and the poorly known Manda-Inakir rift described here. The most recent volcanic event in the Manda-Inakir rift was the formation of the Kammourta basaltic cone, probably in 1928, accompanied by strong seismic activity. This historic eruption and related tectonic features show that the Manda-Inakir rift, like Asal, is presently active. The Kammourta basalt, of transitional alkaline type, belongs to the Manda-Inakir differentiated series, which ranges from basalt to rhyolite. In contrast, volcanic rocks of the Asal rift are entirely transitional tholeiitic basalt. The differences in magmatic affinity and tectonics between these two rift zones reflect the more advanced evolution of rifting in the Asal zone than in Manda-Inakir.
    Type of Medium: Electronic Resource
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  • 14
    ISSN: 1600-5759
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 15
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Cenozoic andesitic volcanism of Logudoro and Bosano correspond to three successive eruptive cycles composed of high alumina basalts, andesites (predominant), dacites, and, more sparsely, rhyolites. All these rocks belong to the calc-alkali serie. In the two first series, a progressive chemical evolution is shown from the saturated and oversaturated basaltic rocks to the dacites. In basaltic rocks, the variation of chemical composition may be related to the segregation of mafic minerals; the segregation of plagioclase appears in andesites. On the other hand, each andesitic serie has distinct evolutive chemical properties. All rocks of this calc-alkali association are relatively enriched in potassium. In Sardinia, the contents of this element increase Northward and suggest a deepening of a Benioff zone in the same direction. Moreover, the Logudoro region is caracterised by irregular distribution of potassium, with very local enrichment, particularly in andesites. These enrichments may be related to a crustal contamination.
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  • 16
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 68 (1978), S. 89-98 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Cenozoic calc-alkaline ignimbrites and related lavas from N.W. Sardinia (Italy), which are closely associated with andesites, have dacitic to rhyolitic composition. The ignimbritic rocks underwent fractional crystallization dominated by plagioclase. The model calculations for REE, Ba, Sr, and Rb are consistent with the generation of ignimbritic magmas by partial melting of tonalitic rocks. P-T estimates for the crystallization of ignimbrites, which give temperatures in the range of 910 °–1070 ° C and P $$P - T - X_{CO_2 }$$ about 5 kb, imply a local increase of temperature in the crust, which is probably related to the ascending andesitic magma. The variations of trace elements indicate that associated andesitic rocks were contaminated by ignimbritic magma.
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  • 17
    ISSN: 1432-0819
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Some recent calc-alkaline andesites and dacites from southern and central Martinique contain basic xenoliths belonging to two main petrographic types: The most frequent one has a hyalodoleritic texture (« H type ») with hornblende + plagioclase + Fe-Ti oxides, set in an abundant glassy and vacuolar groundmass. The other one exhibits a typical porphyritic basaltic texture (« B type ») and mineralogy (olivine + plagioclase + orthopyroxene + clinopyroxene + Fe-Ti oxides and scarce, or absent hornblende). Gradual textural and mineralogical transitions occur between these two types (« I type ») with the progressive development of hornblende at the expense of olivine and pyroxenes. Mineralogical and chemical studies show no primary compositional correlations between the basaltic xenoliths and their host lavas, thus demonstrating that the former are not cognate inclusions; they are remnants of basaltic liquids intruded into andesitic to dacitic magma chambers. This interpretation is strengthened by the typical calc-alkaline basaltic composition of the xenoliths, whatever their petrographic type (« H », « I » or « B »). The intrusion of partly liquid, hot basaltic magma into colder water-saturated andesitic to dacitic bodies leads to drastic changes in physical conditions. The two components; the basaltic xenoliths are quenched and homogeneized with their host lavas with respect to To;fO2 andpH2O conditions. « H type » xenoliths represent original mostly liquid basalts in which such physical changes lead to the formation of hornblende and the development of a vacuolar and hyalodoleritic texture. The temperature increase of the acid magma depends on the amount of the intruding basalt and on the thermal contrast between the two components. The textural diversity which characterizes the xenoliths reflects the cooling rate of the basaltic fragments and/or their position relative to the basaltic bodies (chilled margins or inner, more crystallized, portions). In addition to physical equilibration (T, fO2) between the magmas, mixing involves: mechanical transfer of phenocrysts from one component to another, in both directions; volatile transfer to the basaltic xenoliths, with chemical exchanges. It is here demonstrated that a short period of time (some ten hours to a few days) separates the mixing event from the eruption, outlining the importance of magma mixing in the triggering of eruption. The common occurrence of basaltic xenoliths (generally of « H » type) in calc-alkaline lavas is emphasized, showing that this mechanism is of first importance in calc-alkaline magma petrogenesis.
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  • 18
    ISSN: 1434-6036
    Keywords: PACS. 71.30.+h Metal-insulator transitions and other electronic transitions - 75.30.Kz Magnetic phase boundaries (including magnetic transitions metamagnetion, etc.) - 75.30.Fv Spin density waves
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract: In order to understand the magnetic field-induced restoration of a highly conductive state in , static (SQUID) and dynamic (ESR and AFR) magnetization measurements were performed on polycrystalline samples and single crystals, respectively. In addition, cantilever and resistivity measurements under steady fields were performed. While the metal-insulator transition curve of the ( ) phase diagram exhibits a first order character, a “spin-flop” transition line divides the insulating state when the magnetic field is applied along the easy axis of magnetization. The effects of a RKKY-type indirect exchange and of applied magnetic field are described within the framework of a generalized Kondo lattice, namely two chains of localised spins coupled through the itinerant spins of the 2D sheets of BETS. The calculations, which can incorporate intramolecular electron correlations within a mean field theory, are in qualitative agreement with the field induced transition from the antiferromagnetic insulating ground state to a canted one, i.e. a not fully oriented paramagnetic, but metallic state.
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  • 19
    ISSN: 1434-6036
    Keywords: PACS. 76.30.-v Electron paramagnetic resonance and relaxation - 61.50.Ks Crystallographic aspects of phase transformations; pressure effects - 75.50.Ee Antiferromagnetics
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract: Electrocrystallization of CH2Cl2 solutions of Cp2Mo(dmit), dmit2- = 2-thioxo-1,3-dithiole-4,5-dithiolate, in the presence of n-Bu4NX (X- = PF 6 - , AsF 6 - , SbF 6 - ) affords the corresponding 1:1 cation radical salts [Cp2Mo(dmit) ][X-]. The three isostructural salts crystallize in the orthorhombic system, space group Cmcm. In the three salts, a second-order transition at a temperature T1, identified by EPR measurements and low-temperature X-ray Weissenberg photographs reveals also a splitting of some principal reflections and the twinned character of the crystals, whose room temperature structure may also be described in the monoclinic P21/m space group. The second order monoclinic triclinic transition is associated with the apparition of a superlattice characterized by the critical wave vector when expressed in the monoclinic system. A second transition at a lower temperature T2, of first order character, is observed only in the PF 6 - salt. This triclinic triclinic transition leads to a novel superlattice of wave vector while the superlattice is conserved down to 10 K in the AsF 6 - and SbF 6 - salts. Finally, a third transition to an antiferromagnetic ground state is observed for the three salts and investigated by static susceptibility measurements and Antiferromagnetic Resonance (AFMR) experiments. The detailed analysis of the AFMR rotation patterns confirms the twinned nature and the low temperature triclinic symmetry of the crystals as well as the peculiar behaviour of the PF 6 - salt, when compared with the two other members of these novel series.
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  • 20
    ISSN: 1434-6036
    Keywords: PACS. 76.30.-v Electron paramagnetic resonance and relaxation - 61.50.Ks Crystallographic aspects of phase transformations - 75.50.Ee Antiferromagnetics
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract: The physical properties of paramagnetic Mo(V) organometallic radical cation salts, , are investigated through the study of two series of solid solutions incorporating two kinds of anions ( or ). The combination of EPR and X-ray diffraction is used to specify the nature of the structural phase transitions which occur in the paramagnetic phase and to determine the corresponding ( T , x ) phase diagrams. Finally, antiferromagnetic resonance is studied to probe the low temperature antiferromagnetic ground state. In the last part of the paper, the observed complex phase diagram is analyzed by considering a compressible model with at least two independent modes of compression. We conclude that the larger compressibilities are associated with the smaller anions.
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