Dergiler / Maden Tetkik ve Arama Dergisi / 2003 / Cilt: 126 - Sayı: 126

A DEBATE PELAGIC PALEOCENE SEQUENCE IN BIGA PENINSULA: BALLIKAYA (BALIKKAYA) FORMATION

Sayfa
43–48
Yayın Tarihi
2003-07-01
DOI
—
🏛️Bu makalenin bibliyografik verileri ve tam metin bağlantısı DergiPark üzerinden sağlanmıştır.
DergiPark Kaydı ↗
✨

Yapay Zeka Hızlı Bakış & Çıkarımlar

AI Insight
⚡ TL;DR(1 Cümlede Hızlı Çıkarım)

In this area, the limestone blocks are in Malm-Early Cretaceous age and the matrix to these blocks, however is rarely exposed and contains red, bordeaux, thin-bedded limestone which is Late Maastrichtian in age based on foraminferas identified as Globotruncanella havanensis (Voorwijk), Globotruncanella citae (Bolli), Abathomphalussp.

📌 3 Maddede Bu Makale

🎯
Amaç & Hipotez:An olistostromal unit, composed of andesite, basalt, sandstone and conglomerate, and limestone blocks within red-wine colored mudstone matrix is cropped out in surrounding areas of Balıkkaya hill, Havdan and Sansuvat villages 500 to the west of Biga township (Çanakkale).
📊
Temel Bulgular & Veri:The existence and age of this unit is under discussion as it is accepted in Thanetian-Danian (Paleocene) age based on foraminiferas found in mudstone and named as Ballıkaya formation.
💡
Sonuç & Katkı:In this area, the limestone blocks are in Malm-Early Cretaceous age and the matrix to these blocks, however is rarely exposed and contains red, bordeaux, thin-bedded limestone which is Late Maastrichtian in age based on foraminferas identified as Globotruncanella havanensis (Voorwijk), Globotruncanella citae (Bolli), Abathomphalussp.
🔬Tür:Laboratuvar & Saha Deneyi
📍Kapsam:Genişletilmiş Akademik Örneklem
⚙️Değişkenler:Alan Parametreleri

Abstract

An olistostromal unit, composed of andesite, basalt, sandstone and conglomerate, and limestone blocks within red-wine colored mudstone matrix is cropped out in surrounding areas of Balıkkaya hill, Havdan and Sansuvat villages 500 to the west of Biga township (Çanakkale). The existence and age of this unit is under discussion as it is accepted in Thanetian-Danian (Paleocene) age based on foraminiferas found in mudstone and named as Ballıkaya formation. In this area, the limestone blocks are in Malm-Early Cretaceous age and the matrix to these blocks, however is rarely exposed and contains red, bordeaux, thin-bedded limestone which is Late Maastrichtian in age based on foraminferas identified as Globotruncanella havanensis (Voorwijk), Globotruncanella citae (Bolli), Abathomphalussp.

🔖

Bu Makaleye Atıf Yap

ATABEY, E., ERDOĞAN, K. (2003). A DEBATE PELAGIC PALEOCENE SEQUENCE IN BIGA PENINSULA: BALLIKAYA (BALIKKAYA) FORMATION. Maden Tetkik ve Arama Dergisi, Cilt: 126 - Sayı: 126, 43–48. https://ajindex.com/articles/54181

📄 Tam Metin PDF Okuyucu

📄

PDF görüntüleyici hazırlanıyor...

Kaynakça (5)

  1. Altıner, D.; Koçyiğit, A.; Farinacci, A.; Nicosia, U. And Conti, M. A., 1991, Jurassic-Lower Cretaceous stratigraphy and paleogeograp- hic evolution of the southern part of North Western Ariatolia (Turkey), Geology and paleontology of Western Pontids, Jurassic- Early Cretaceous stratigraphy, tectonics and paleogeographic evolution: ed by (Anna Farinacci, Derek V. Ager, Umberto Nicosia, Geology Romana, S. 28, 13-80,
  2. Roma. Bingöl, E., Akyürek, B. and Korkmazer, B., 1975, Biga Yarımadasının jeolojisi ve Karakaya formas- yonunun bazı özellikleri, Cumhuriyet'in 50. Yılı Yerbilimleri Kongresi TebliğIeri, MTA Enstitüsü, Ankara, 70-77.
  3. Okay, I. A., 1988, Çan-Yenice-Biga arasının jeolojisi ve tektoniği, TPAO Arama Grubu Rap., No: 2544. Okay, I/A.; Siyako, M.; and Bürkan, K. A. 1990, Biga Yarımadasının Jeolojisi ve Tektonik Evrimi TPJDBult., C. 2/1, 83-121,
  4. Yıkılmaz, M. B. and Özkar-Öngen, I., 2002, Ballıkaya formasyonu: Biga Yarımadasında pelajik bir Paleosen istifi, Türkiye Stratigrafi Komitesi Çalıştayı, Trakya bölgesinin Litostratigrafi Adlamaları Özleri, s.6. Siyako, M., Burkan, K. A. and Okay, I. A., 1998, Biga ve Gelibolu Yarımadalarının Tersiyer Jeolojisi ve Hidrokarbon Olanakları, TPJD Bult., C. 1/3, 183-199.
  5. Yıkılmaz, M. B., Okay, I. A. and Özkar, I., 2002, Biga Yarımadasında pelajik bir Paleosen istifi, MTA Bull., 123-124, 21-26.