Evolution of the Variscan orogenic plutonic magmatism: the Greater Caucasus
نویسندگان
چکیده
منابع مشابه
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[1] The current structure of the South Armorican Domain in the French Variscan Belt, provides an excellent record of the late orogenic evolution, as documented by the complex interactions between extensional structures and partial melting. In the Golfe du Morbihan, the South Brittany Migmatite Belt (SBMB), tectonically overlain by non‐melted metamorphic units, was studied by combined structural...
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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...
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ژورنال
عنوان ژورنال: Journal of Nepal Geological Society
سال: 2011
ISSN: 2676-1378,0259-1316
DOI: 10.3126/jngs.v43i0.24514