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Geothermobarometry in metasediments of the southern Grossvenediger area (Tauern Window, Austria)
Journal of Metamorphic Geology, 1990Metasediments in the southern Grossvenediger area (Tauern Window, Austria) were studied along a cross‐section through rocks of increasing metamorphic grade from the margin of the Tauern Window in the south to the base of the Upper Schieferhülle, including the Eclogite Zone, in the north.In the southern part of the cross‐section there is no evidence for
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Novel use of borosilicates in geothermobarometry
Mitteilungen der Österreichischen Mineralogischen GesellschaftTerrestrial planets (like Venus, Earth, Mars) are planets, which are composed preliminary of silicates or metals. All terrestrial planets may have the same basic type of structure; such as a metallic core (mostly iron), with a surrounding silicate mantle. More than 90 % of the Earth’s crust is composed of silicates.
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Geothermobarometry on anatectic melts – a high-pressure Variscan migmatite from northeast Sardinia
International Geology Review, 2013Hans-Joachim Massonne, Gabriele Cruciani
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