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  • 1
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    3D Grazing Collision of Two Black Holes (2001)
    In:  EPIC3Physical review letters, 87, 271103 p.
    Details
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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    PAPER (OA)
  • 2
    Electronic Resource
    Electronic Resource
    Thermodynamic Properties of N-Propyl Alcohol. (1963)
    s.l. : American Chemical Society
    Journal of chemical & engineering data 8 (1963), S. 560-564 
    Details
    ISSN: 1520-5134
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/je60019a025
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  • 3
    Electronic Resource
    Electronic Resource
    Modification of the VICKSI beam profile monitor system for application at low beam intensities
    Amsterdam : Elsevier
    Nuclear Instruments and Methods in Physics Research Section A: 268 (1988), S. 503-505 
    Details
    ISSN: 0168-9002
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0168-9002(88)90567-0
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  • 4
    Electronic Resource
    Electronic Resource
    Physik des erdkorpers - SCHICK, R. und G. SCHNEIDER (1973): Eine Einfuhrung fur Naturwissenschaftler und Ingenieure. 267 S., 127 Abb., 14 Tab. Stuttgart: Ferdinand Enke Verlag. DM 59,-.
    Amsterdam : Elsevier
    Geoforum 15 (1973), S. 72 
    Details
    ISSN: 0016-7185
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geography
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0016-7185(73)90056-0
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  • 5
    Electronic Resource
    Electronic Resource
    Jurassic age of metamorphism at the base of the Brezovica peridotite (Yugoslavia)
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 39 (1978), S. 291-297 
    Details
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0012-821X(78)90205-4
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  • 6
    Electronic Resource
    Electronic Resource
    Crystal-chemical relations of iron in natural Mg-carpholites: a spectroscopic study (1996)
    Springer
    Physics and chemistry of minerals 23 (1996), S. 237-238 
    Details
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00207755
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  • 7
    Electronic Resource
    Electronic Resource
    Crystal chemistry of Fe-Mg-carpholites (1979)
    Springer
    Contributions to mineralogy and petrology 70 (1979), S. 41-47 
    Details
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A chemical and X-ray investigation of the Fe-Mg-carpholites of Crete/Greece reveals a large variation in their Fe2+/(Fe2++Mg) ratios (0.68 to 0.05). The lattice constants a and b depend linearly on this parameter, and the magnitude of the effect is comparable to that encountered in pyroxenes. The similar behaviour of the lattice dimensions of both these minerals is explained by comparing their structures and pointing out the salient crystal chemical similarities.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00371870
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  • 8
    Electronic Resource
    Electronic Resource
    Magmatic and metamorphic evolution of metagabbros in the Münchberg Massif, N.E. Bavaria (1991)
    Springer
    Contributions to mineralogy and petrology 107 (1991), S. 112-123 
    Details
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The central gneiss complex of the Münchberg Massif consists of the Liegendserie at the base and the Hangendserie at the top. Metagabbros are found in the Liegendserie; eclogites occur in the Hangendserie. New isotope data revive the discussion whether a genetic relationship exists between metagabbros and eclogites in the Münchberg Massif. It is possible to relate the two types of rocks to the same protoliths by variable degrees of crustal contamination and magmatic accumulation. Therefore, a common magmatic origin may be assumed. Both the metagabbros and the eclogites were affected by amphibolite-facies metamorphism. The amphibolitization of the metagabbros was a prograde metamorphic event. Increasing temperature is indicated by inverse zonation of recrystallized plagioclase and increasing Mg/Fe ratios in garnet from core to rim. Geothermobarometry yields a temperature of 600°C and a pressure of about 11 kbar for the peak of metamorphism. In contrast, the eclogites underwent a first high-pressure stage at a minimum pressure of 14 kbar and a temperature estimated at 600°C and were subsequently overprinted under amphibolite-facies conditions at 10 kbar/700°C. A common magmatic origin of metagabbros (Liegendserie) and eclogites (Hangendserie) of the Münchberg Massif can no longer be discarded. However, the converging P-T-t paths reflect a different geodynamic evolution of the Liegendserie and the Hangendserie after magmatism and before amphibolite-facies metamorphism.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00311189
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  • 9
    Electronic Resource
    Electronic Resource
    Rb–Sr and K–Ar mineral data of the KTB and the surrounding area and their bearing on the tectonothermal evolution of the metamorphic basement rocks (1997)
    Springer
    Geologische Rundschau 86 (1997), S. S251 
    Details
    ISSN: 0016-7835
    Keywords: Key words Bohemian Massif ; KTB ; K ; Ar and Rb ; Sr mineral dating ; Middle to post-Variscan tectonothermal evolution
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  K–Ar and Rb–Sr age determinations on muscovites and biotites and K–Ar age determinations on amphiboles are presented for leucocratic gneisses, amphibolites and (meta-)igneous rocks from the Zone of Erbendorf Vohenstrauss (ZEV) and the KTB boreholes located in the northeastern ZEV and leucocratic gneisses from the Erbendorf Greenschist zone (EGZ). The investigations were carried out to contribute to the knowledge of the tectonothermal evolution of the area and to the response of the isotope systems to retrograde processes including recent elevated in- situ temperatures in the boreholes. A memory of an early Ordovician igneous event is given by Rb–Sr ages of 480±5–475±5 Ma obtained on very coarse-grained relic igneous muscovites of metapegmatites from the ZEV. This memory is missing in micas from peg matoids of the drill site. Coarse-grained muscovites of gneisses from ZEV and EGZ surface outcrops and of gneisses and pegmatoids from the boreholes yielded maximum K–Ar ages of 377±3–371±3 Ma related to the end of the Devonian regional metamorphism in both units. Consistent K–Ar and Rb–Sr apparent ages of some muscovites from surface outcrops point to a fast cooling of the metamorphic rocks due to rapid tectonic uplift. The lack of a depth-related gradient in model ages of coarse-grained KTB muscovites is explained by post-Variscan stacking processes. For minerals from intermediate to greater depths of the KTB, a strong age dependence on grain size and disturbances of the isotope systems due to various late- to post-Variscan retrograde processes can be demonstrated. A strong decrease in K–Ar model ages with increasing depth as obtained for biotites from the deepest section of the HB borehole probably indicates time-integrated response of the isotope system to elevated in situ temperatures.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/PL00014658
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  • 10
    Electronic Resource
    Electronic Resource
    Oberkretazisches Kristallin an der Basis von Ophiolithen der Südägäis: Charakterisierung der Metamorphose-Fazies (1984)
    Springer
    Mineralogy and petrology 33 (1984), S. 263-286 
    Details
    ISSN: 1438-1168
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Summary Late Cretaceous metamorphites, investigated in a profile near Lendas/Asterousia Mountains (southern coast of Crete), consist of the following lithological units (from the base to the top): massive ortho-amphibolites, which may contain diopside besides plagioclase and magnesiohornblende; cordierite-garnet-sillimanite-biotite gneisses; calc-silicate rocks and marbles with salitic pyroxene, pargasite, magnesio-homblende, cummingtonite, grossular-andradite garnet, wollastonite, and scapolite. Meta-ultramafics with anthophyllite, tremolite, olivine, and orthopyroxene are intercalated with the calc-silicate series. The mineral parageneses in the four classic bulk rock compositions — basic, pelitic, siliceous-calcareous, and ultrabasic — afford an opportunity to characterize the metamorphic facies in detail. From these parageneses, and from the Mg/Fe2+ ratios of coexisting cordierite and garnet, temperatures between 650 and 700°C and pressures between 4 and 6 kbar have been estimated for the conditions of metamorphism.
    Notes: Zusammenfassung Zur Charakterisierung der Metamorphose-Fazies des oberkretazischen Kristallins wurde ein Profil bei Lendas im Asterousia-Gebirge an der Südküste Kretas gewählt. Der Kristallin-Komplex besteht dort — vom Liegenden zum Hangenden — aus massigen Ortho-Amphiboliten, die neben Plagioklas und Magnesiohornblende Diopsid enthalten können, aus Cordierit-Granat-Sillimanit-Biotit-Gneisen sowie aus einer kalksilikatischen Serie mit salitischem Pyroxen, Pargasit, Magnesiohornblende, Cummingtonit, Granat der Grossular-Andradit-Reihe, Wollastonit und Skapolith. In die kalksilikatische Serie sind Anthophyllit, Tremolit, Olivin und Orthopyroxen führende Meta-Ultrabasite eingeschaltet. Die Mineralparagenesen in den vier klassischen Stoffbeständen — basaltisch, pelitisch, kieselig-kalkig, ultrabasisch — ermöglichen eine detaillierte Charakterisierung der Metamorphose-Fazies. An Hand dieser Paragenesen und der Mg/Fe2+-Verhältnisse in Cordierit und Granat wurden für die Metamorphose Temperaturen zwischen 650 und 700°C und Drucke zwischen 4 und 6 kbar abgeschätzt.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01082673
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