BRIEF NOTE ON NEOGENE VOLCANISM in KEMALPAŞA–TORBALI BASIN (İZMİR)

Journal Title: Bulletin of the Mineral Research and Exploration - Year 2015, Vol 150, Issue

Abstract

This study was made in order to introduce Neogene volcanics the first time, which its presence has not been mentioned in previous investigations (Akdeniz et al., 1986; İnci, 1991; Kaya et al., 2007; Sözbilir et al., 2011), in Kemalpaşa–Torbalı basin corresponding to Torbalı section of the Akhisar Depression (Kaya, 1979; 1981) and to state their K/Ar ages.

Authors and Affiliations

Keywords

Related Articles

GEOCHEMICAL CHARACTERISTICS AND RARE-EARTH ELEMENT DISTRIBUTIONS OF KOZBUDAKLAR W-SKARN DEPOSIT (BURSA, WESTERN ANATOLIA)

The Kozbudaklar W-skarn deposit occurs along the contact between Eocene Topuk granitoid and Triassic İnönü marble in Tavşanlı Zone. In the study area, the endoskarn is represented by plagioclase-pyroxene and exoskarn zon...

Post-Glacial Terraces of The Marmara Sea and Water Exchange Periods

Semi enclosed Marmara Sea is a passage between the Aegean Sea (Northeastern Mediterranean Sea) and the Black Sea. The Marmara Sea is connected to the Black Sea and Aegean Sea through the İstanbul Strait (Bosphorus) and Ç...

A new species of Nummulites Lamarck (Nummulitidae, Foraminiferida) from Central Turkey

A new nummulitid species Nummulites sireli n. sp. is described from the middle Lutetian of the Çayraz section, North of Haymana, South of Ankara, Turkey. The new species is referred to the N. distans group, of which six...

WHEN DID THE PLATE TECTONICS BEGIN? THE INCEPTION OF PLATE TECTONICS BASED ON THE EXISTENCE OF KOMATIITES AND THEIR MgO VARIATIONS

The geoscientists have always wondered what evolutionary processes the Early Earth went through until it reached today. The beginning of the plate tectonics poses another matter of debate in these processes. Yet, the deb...

TRACE FOSSILS FROM DEEP SEA SEDIMENTS OF THE LATE EOCENE CEYLAN FORMATION, GELİBOLU PENINSULA (SW THRACE, TURKEY)

In this study, trace fossils of the Ceylan Formation (Late Eocene) in the area NW of Fındıklı village and on the coast of the Ece Bay the Gelibolu Peninsula are identified for the first time. They occur in gray siltstone...

Download PDF file
  • EP ID EP608222
  • DOI 10.19111/bmre.31304
  • Views 161
  • Downloads 0

How To Cite

(2015). BRIEF NOTE ON NEOGENE VOLCANISM in KEMALPAŞA–TORBALI BASIN (İZMİR). Bulletin of the Mineral Research and Exploration, 150(), 163-168. https://europub.co.uk/articles/-A-608222