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Decoupling of high-pressure H2 production from serpentinization and magnetite in subduction zones
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Erosion of heterogeneous rock drives diversification of Appalachian fishes
Science, 2023The high levels of biodiversity supported by mountains suggest a possible link between geologic processes and biological evolution. Freshwater biodiversity is high not only in tectonically active settings but also in tectonically quiescent montane ...
M. Stokes +11 more
semanticscholar +1 more source
Contributions to Mineralogy and Petrology, 1978
The distribution of U has been studied in two metamorphic rock-series with a gradient of regional metamorphism. One series ranges from the lowest greenschist to amphibolite facies and the other one shows increasing metamorphic grade from amphibolite to granulite facies.
Dostal, Jaroslav, Capedri, Silvio
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The distribution of U has been studied in two metamorphic rock-series with a gradient of regional metamorphism. One series ranges from the lowest greenschist to amphibolite facies and the other one shows increasing metamorphic grade from amphibolite to granulite facies.
Dostal, Jaroslav, Capedri, Silvio
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The metamorphic and magmatic record of collisional orogens
Nature Reviews Earth & Environment, 2021Owen M Weller +2 more
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2014
Metamorphic rocks are product of transformation or solid-state recrystallization of existing (protolith) igneous, sedimentary, and metamorphic rocks, due to change in physical and chemical conditions, principally temperature, pressure and introduction of chemically active fluids and gases. Metamorphism alters the mineral composition including formation
S.K. Haldar, Josip TiĊĦljar
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Metamorphic rocks are product of transformation or solid-state recrystallization of existing (protolith) igneous, sedimentary, and metamorphic rocks, due to change in physical and chemical conditions, principally temperature, pressure and introduction of chemically active fluids and gases. Metamorphism alters the mineral composition including formation
S.K. Haldar, Josip TiĊĦljar
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1994
Metamorphic mafic rocks (e.g., mafic schist or greenschist and mafic gneiss, amphibolite) are derived from mafic igneous rocks, mainly basalts and andesites, and of lesser importance, gabbro and mafic diorite (Chap. 2). Metamorphic assemblages in mafic rocks are particularly useful in defining the intensity of metamorphism within the metamorphic facies
Martin Frey, Kurt Bucher
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Metamorphic mafic rocks (e.g., mafic schist or greenschist and mafic gneiss, amphibolite) are derived from mafic igneous rocks, mainly basalts and andesites, and of lesser importance, gabbro and mafic diorite (Chap. 2). Metamorphic assemblages in mafic rocks are particularly useful in defining the intensity of metamorphism within the metamorphic facies
Martin Frey, Kurt Bucher
openaire +2 more sources