نتایج جستجو برای: leucosome

تعداد نتایج: 19  

جعفری, سیده راضیه, شهبازی, حسین, سپاهی, علی اصغر , موذن, محسن ,

In the Hamedan region, migmatitic rocks with various structures cropped out that stromatic structure is the most abundant. Index minerals of metapelites such as garnet (almandine), staurolite, andalusite, sillimanite, kyanite, fibrolite, cordierite, plagioclase (andesine) and spinel (hercynite) are present in these rocks. Garnet has occurred in all three parts of leucosome, paleosome, and melan...

برزوئی, کاظم , سپاهی, علی اصغر , موذن, محسن ,

Intrusion of the Alvand plutonic complex into the pelitic and sim-pelitic rocks of the Tuyserkan area has caused the development of a thermal aureole in the Sarabi area. The rocks within the aureole are thermally metamorphosed and formed different types of hornfelses. High-grade metamorphic rocks with chemically suitable compositions were melted adjacent to the contact due to the heat from the ...

Journal: :Journal of Metamorphic Geology 2021

The Kohistan island arc represents a >50 km thick and completely exposed Late Cretaceous–Eocene Neo-Tethyan sequence between the Indian Eurasian plates in western Himalaya. At base of Arc, Jijal Complex exposes continuous from ultramafic upper mantle rocks to mafic lower crust across Moho transition zone. In shallower section Complex, widespread garnet–clinopyroxene gabbros are uniform assembla...

Journal: :Precambrian Research 2021

• Mangodara forms a dome cored by tonalitic gneiss, mantled granodioritic gneiss. Gneiss-granitoids derive from partial melting of Birimian greenstones. Residual melt syntectonic gneiss genesis formed rare-metal pegmatites. We describe the geological context rare metal-bearing pegmatites district (South-West Burkina Faso, Paleoproterozoic West African Craton) and discuss their petrogenesis link...

2010
Michael Brown

The formation and differentiation of the continental crust occurs at convergent plate margins in accretionary and collisional orogenic belts where sufficient heat is generated to achieve high-grade metamorphism and anatexis. Volumetrically significant H2O-present melting requires an influx of aqueous fluid along zones of high-strain deformation or via fracture networks, or recycling of the flui...

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