We'd like to understand how you use our websites in order to improve them. Register your interest. Clinopyroxene and orthopyroxene megacrysts with lamellar intergrowths of pyroxenes and garnet rarely survive in pyroxenite layers from the exposed spinel-lherzolite massifs because of the emplacement history into the crust. Textural and chemical data suggest that the present pyroxenite parageneses resulted from subsolidus recrystallization of magmatic assemblages composed of Al-rich orthopyroxene and clinopyroxene with minor spinel. The primary Al-rich ortho-and clinopyroxenes behaved differently on cooling. In a first stage, orthopyroxene exsolved concomitant Al-rich clinopyroxene and garnet, whereas clinopyroxene exsolved only Al-rich orthopyroxene.
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ISBN 13: 9789056991241
Kodra, K. Gjata, F. Bakalli; Les principales etapes de l'evolution paleogeographique et geodynamique des Albanides internes au cours du Mesozoique. Shibboleth Sign In.
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User Name. Remember Me. Exploration of Mars has revealed the presence of large outflow channels which have been interpreted as the products of catastrophic flood events during which a large quantity of water was released Read More Mars had a global magnetic field much earlier and much later in the planet's history than scientists have previously known.
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