Dergiler / Maden Tetkik ve Arama Dergisi / 1985 / Cilt: 103 - Sayı: 104

MIDDLE MIOCENE BIOSTRATIGRAPHY

Sayfa
55–55
Yayın Tarihi
1985-08-01
DOI
—
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⚡ TL;DR(1 Cümlede Hızlı Çıkarım)

The fossil association and property of the sediments are also indicated that the environment is pelagic.

📌 3 Maddede Bu Makale

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Amaç & Hipotez:In this study, 21 planktonic Foraminifera species determined in the Middle Miocene sequence at the Karaisalı region of Adana.
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Temel Bulgular & Veri:In addition to above mentioned planktonic Foraminifera, 13 Nannoplankton species are determined in the same samples.
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Sonuç & Katkı:The fossil association and property of the sediments are also indicated that the environment is pelagic.
🔬Tür:Araştırma Makalesi
📍Kapsam:Genişletilmiş Akademik Örneklem
⚙️Değişkenler:Alan Parametreleri

Abstract

In this study, 21 planktonic Foraminifera species determined in the Middle Miocene sequence at the Karaisalı region of Adana. The following biozones in Langhian-Serravalian ages are distinguished: ? Globorotalia fohsi lobata zone, Globorotalia fohsi fohsi zone, Globorotalia fohsi peripheroronda zone. In addition to above mentioned planktonic Foraminifera, 13 Nannoplankton species are determined in the same samples. The result of this study has been compared with other studies which have been done in Trinidad, New Zeland, Libya, SW Africa and Nord Carrebean Sea and similar results are obtained. The fossil association and property of the sediments are also indicated that the environment is pelagic.

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Bu Makaleye Atıf Yap

NAZİK, A., TOKER, V. (1985). MIDDLE MIOCENE BIOSTRATIGRAPHY. Maden Tetkik ve Arama Dergisi, Cilt: 103 - Sayı: 104, 55–55. https://ajindex.com/articles/54414

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Kaynakça (10)

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