- Communications Faculty of Sciences University Ankara Series C Biology
- Vol: 08 (1990)
- GEOLOGY AND GEOCHEMİSTRY OF THE KARADAĞ VOLCANİC succession, POLİOCENE - QUATERNARY, CENTRAL 2INATOL...
GEOLOGY AND GEOCHEMİSTRY OF THE KARADAĞ VOLCANİC succession, POLİOCENE - QUATERNARY, CENTRAL 2INATOLIA, TURKEY
Authors : Şükrü Koç
Pages : 0-0
Doi:10.1501/Commuc_0000000110
View : 4 | Download : 3
Publication Date : 1990-01-01
Article Type : Research
Abstract :The Karadağ volcanic succession of Pliocene and Oualernaiy represents typical Continen tal volcanisms of central Anatolia. It consists of nıainîy lava flows and pyroclastic depositş. Overall, they Avere produced by magmato-phreatic e.Kplosions in four periods throiıgh the plioce ne and Çuaternay times. The product of each period can be easiîy distinguished by vvcathering surfaces and localiy erodcd surfaces. Petrographical and geochemical analysis show that they are mostly andcsitic and dacitic roeks, originated from partial rnelting of Continental crust.Keywords : GEOLOGY, GEOCHEMİSTRY, POLİOCENE - QUATERNARY