Zobrazeno 1 - 3
of 3
pro vyhledávání: '"glokonitli kumtaşı"'
Autor:
A. Müjdat Özkan
Publikováno v:
Pamukkale University Journal of Engineering Sciences, Vol 8, Iss 3, Pp 357-364 (2002)
İnceleme alanında yer alan Üst Paleosen - Orta Eosen yaşlı Halkapınar formasyonu, sığ ve derin denizel ortamda oluşmuştur. Formasyonun litolojilerini orta-kalın tabakalanmalı konglomera, ince - kalın tabakalanmalı kumtaşı, ince - çok
Externí odkaz:
https://doaj.org/article/a472b76008c4429984ef5adedd8fac54
Autor:
A. Müjdat Özkan
Publikováno v:
Pamukkale University Journal of Engineering Sciences, Vol 8, Iss 3, Pp 357-364 (2002)
In the study area, Upper Paleocene - Middle Eocene aged Halkapınar formation, was formed in a shallow and deep marine environment. The lithologies of this formation are medium - thick bedded conglomerate, thin - thick bedded sandstone, thin - very t
Externí odkaz:
https://doaj.org/article/de61af7aa5e84514a1a04a5f2439bb02
Autor:
ÖZKAN, A. Müjdat
Publikováno v:
Volume: 8, Issue: 3 357-364
Pamukkale Üniversitesi Mühendislik Bilimleri Dergisi
Pamukkale Üniversitesi Mühendislik Bilimleri Dergisi
In the study area, Upper Paleocene - Middle Eocene aged Halkapınar formation, was formed in a shallow and deep marine environment. The lithologies of this formation are medium - thick bedded conglomerate, thin - thick bedded sandstone, thin - very t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=tubitakulakb::a23726a3274261376fb0712c708d224b
https://dergipark.org.tr/tr/pub/pajes/issue/20534/218765
https://dergipark.org.tr/tr/pub/pajes/issue/20534/218765
