Post-collisional H-type granitoid magmatism in Central Anatolia and time-space relation with Fe-oxide mineralization
Küçük Resim Yok
Tarih
2003
Dergi Başlığı
Dergi ISSN
Cilt Başlığı
Yayıncı
MILLPRESS SCIENCE PUBLISHERS
Erişim Hakkı
info:eu-repo/semantics/closedAccess
Özet
The distribution, in both space and time, of the mineral deposits of the Central Anatolia reveals some interesting and enigmatic features of mineralization in a collision related setting. Central Anatolia is a polymetallic metallogenic province hosting mineral deposits of various size and type. Present study concerns with the formation and distribution of the Fe-oxide mineralization in terms of granite metallogeny, and reveals the genetic coexistence of H-type post-collisional granitoid magmatisin and Fe-oxide mineralization.
Açıklama
7th Biennial SGA Meeting -- AUG 24-28, 2003 -- Athens, GREECE
Anahtar Kelimeler
Central Anatolia, Fe-oxide, Cu-Au, Fe-oxide-Cu-Au, post-collisional H-type magmatism
Kaynak
MINERAL EXPLORATION AND SUSTAINABLE DEVELOPMENT, VOLS 1 AND 2
WoS Q Değeri
N/A
