Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Erdal Koşun"'
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 122, Iss 122, Pp 1-21 (2000)
Bu çalışmaya konu olan glokonili sedimanlar, Devrek-Zonguldak ve Kastamonu civarında farklı yaş ve fasiyes özelliğinde depoianmışlardır.Batı Karadeniz bölgesi Alt Kretase islifindeki glo koni. dış şelfde aşmalı deniz düzeyi koşull
Externí odkaz:
https://doaj.org/article/726e58a3a1984630a1c64d2bb70f69b7
Autor:
Erdal KOŞUN, Attila ÇİNER
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 125, Iss 125, Pp 58-59 (2002)
Sivas Miyosen havzası birimlerinin zaman ve mekân içerisindeki ortamsal ve sedimanter özellikleri ile çökel evrimlerini belirlemek amacı ile Zara güneyinde yapılan detay çalışmalar sonucunda Erken Miyosen yaşlı Ağılkaya formasyonunun
Externí odkaz:
https://doaj.org/article/9c4a4c72b746488694b891f0011a870d
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 130, Iss 130, Pp 19-19 (2005)
Tufa terimi; düşük Mg- karbonatlı, soğuk tatlı suların oluşturduğu, biyolojik ve/ veya fiziko-kimyasal süreçler tarafından çökeltileri, makro ve mikro ölçekte bitki, hayvan kalıntısı ve bakteri (özellikle siyanobakteri) içeren,
Externí odkaz:
https://doaj.org/article/4ad9abcae9d240bab48f3486192b84af
Autor:
Aymon Baud, Richard J. Twitchett, Sylvain Richoz, Rainer Brandner, Tayebeh Mohtat, Joachim Reitner, Katrin Heindel, Erdal Koşun, Vanessa Julie Roden, Jörn Peckmann, Daniel Birgel, Leopold Krystyn, William J. Foster
Publikováno v:
Gondwana Research. 61:187-202
After the latest Permian mass extinction event, microbial mats filled the ecological niche previously occupied by metazoan reefs, resulting in widespread microbialites. This study focuses on the lipid biomarker (molecular fossil) and invertebrate fos
Autor:
Susanne Gier, Jörn Peckmann, Wolfgang Bach, Bernhard Grasemann, Christa Schleper, Jennifer Zwicker, Daniel Smrzka, Sylvain Richoz, Simon K.-M. R. Rittmann, Erdal Koşun, Daniel Birgel
Publikováno v:
Chemical Geology. 483:567-580
Serpentinite-hosted ecosystems are potential sites where life may first have evolved on Earth. Serpentinization reactions produce strongly reducing and highly alkaline fluids that are typified by high concentrations of molecular hydrogen (H2) and met
Publikováno v:
World Geomorphological Landscapes ISBN: 9783030035136
Tufa formation is a very common feature in the geological record of the Antalya region where it covers an area of 630 km2 and is up to 280 m thick. The oldest date obtained from this tufa deposit is >600 ka, and the youngest one is modern. Characteri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a60cf631ed5e5867b4b6fb2afd272dfa
https://doi.org/10.1007/978-3-030-03515-0_7
https://doi.org/10.1007/978-3-030-03515-0_7
Publikováno v:
Journal of Archaeological Science. 123:105255
Speleothems are recognized as sensitive recorders of climatic fluctuations in the past and provide precisely dated and highly resolved environmental records. However, their potential as an archaeological archive is not fully acknowledged yet. Here we
Publikováno v:
Volume: 58, Issue: 2 85-102
Türkiye Jeoloji Bülteni
Türkiye Jeoloji Bülteni
Konyaaltı ve Lara plajları Antalya ilinin merkezi sınırları içerisinde ve Antalya Körfezi’nin sırasıylakuzeybatı ve kuzeydoğu kesimlerinde yer almaktadırlar. Bu çalışmada aynı hidrodinamik koşullar altındagörünen bu iki plajın,
Autor:
Jörn Peckmann, William J. Foster, Rainer Brandner, Tayebeh Mohtat, Richard J. Twitchett, Sylvain Richoz, Daniel Birgel, Katrin Heindel, Aymon Baud, Erdal Koşun, Joachim Reitner, Leopold Krystyn
Publikováno v:
Geological Society of America Abstracts with Programs.
Facies characteristics and depositional environments of Quaternary tufa deposits, Antalya, SW Turkey
Autor:
Erdal Koşun
Publikováno v:
Carbonates and Evaporites. 27:269-289
This study describes the facies characteristics and the origin of widespread tufa deposits in Antalya Quaternary Basin in southwestern Turkey. The tufa formation covers an area of 630 km2 and is up to 280 m thick. Its generation is related to three m