Kayseri civarında incelemeler yapan E. CHAPUT (I), G. BARTSCH ( 2 ) ve F. BAYKAL (3 ) bölgedeki Neojon arazisinin, umumiyetle göl menşeli kalker ve marnlardan, lav ve tüflerden, birde konglomera ve grelerden müteşekkil olduğunu göstermişlerdir.
Maden Tetkik Arama Entitüsü
Les formations néogènes des environs de Kayseri ont été observées par de nombreux auteurs qui ont voyagé dans cette région. Parmi eux E. CHAPUT (1), F BARTSH (2) et F. BAYKAL (3) surtout, les ont fait connaitre; d’après leurs observations le terrain Néogène est formé de laves et de tufs volcaniques, de calcaires et de marnes lacustres, de conglomérats et de sables.
Primary Language | Turkish |
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Subjects | General Geology, Mineralogy- Petrography, Geological Sciences and Engineering (Other), Physical Geography and Environmental Geology, Palaeontology, Geology (Other) |
Journal Section | Makaleler - Articles |
Authors | |
Publication Date | January 31, 1951 |
Submission Date | December 20, 1950 |
Acceptance Date | January 24, 1951 |
Published in Issue | Year 1951 Volume: 3 Issue: 1 |
Instructions for Authors: http://www.jmo.org.tr/yayinlar/tjb_yazim_kurallari.php
Ethical Statement and Copyrighy Form: https://www.jmo.org.tr/yayinlar/tjb_telif_etik_formlar.php