نتایج جستجو برای: migmatite

تعداد نتایج: 114  

Journal: :Bulletin De La Societe Geologique De France 2021

The Montagne Noire located in the southern part of French Massif Central represents northern South-Variscan Foreland. It is subdivided into three parts. granite-migmatite Axial Zone dome surrounded by non- or weakly metamorphosed Paleozoic sedimentary series. Both and flanks are deformed km-scale, south to southeast facing recumbent folds thrusts sheets. Raman Spectroscopy Carbonaceous Material...

Bayat, Sima, Didar, Pejvak, Jahangiri, Ahmad, Siahcheshm, Kamal,

The Malayer-Boroujerd-Shazand district (approximately 70 km long) is located in the Sanandaj-Sirjan zone with NW-SE trending, and consist mainly of hornfels, schist, phyllite, migmatite, granite and granodiorite which contain numerous pegmatite and aplitic dykes. Among these rocks, granodiorite, hornfels and schist are main host rocks for quartz, feldspar, muscovite and tourmaline bearing pegma...

Masoudi, , Tondkar, ,

Biotite is a common rock-forming mineral and accepts a variety of elements in its structure. The valuable information of crystallization conditions of the biotite mineral obtain on natural biotite composition. The biotite mineral is one of the main mineral phases of pelitic rocks which are formed in a wide range of geological conditions. In this research, microscopic mineralogy, Raman spectrosc...

2007
Michel Faure

The Variscan French Massif Central experienced two successive stages of extension from Middle Carboniferous to Early Permian. In the northern Massif Central, the first stage began in the late Visean, immediately after nappe stacking, and is well recorded by NamurianWestphalian synkinematic plutonism. The Middle Carboniferous leucogranites widespread in the NW Massif Central (Limousin and Sioule...

2012
T. E. JOHNSON H. R. ROLLINSON

The central region of the mainland Lewisian gneiss complex of NW Scotland is a granulite-facies migmatite terrane.With the exception of ultramafic and rare calc-silicate rocks, all other lithologies partially melted during Neoarchaean, ultrahigh-temperature (Badcallian) metamorphism. The clearest evidence is preserved within large layered mafic^ultramafic bodies that exhibit macroscopic feature...

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