Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Kürşad ASAN"'
Autor:
Hüseyin Kurt, Kürşad Asan
Publikováno v:
Pamukkale University Journal of Engineering Sciences, Vol 26, Iss 3, Pp 524-534 (2020)
Orta Pontidlerde, Sinop-Samsun çevresinde Geç Kretase-Eosen yaşlı volkanik kayaçlar belirgin yüzlekler vermektedir. Geç Kretase volkanitleri, kuzeyde Sinop yakın civarında Hamsaros Volkanitleri, güneyde ise Alaçam-Dikmen-Durağan çevreler
Externí odkaz:
https://doaj.org/article/2f827ecf1b4b40b8ac01b3aca837b197
Autor:
Kürşad Asan
Publikováno v:
Geosciences, Vol 10, Iss 9, p 348 (2020)
This study presented whole-rock elemental and Sr-Nd isotope geochemistry data with the purpose to decipher the origin and evolution of the Miocene Elmadağ Volcanic Complex, Central Anatolia (Ankara, Turkey). Volcanic products spanned in composition
Externí odkaz:
https://doaj.org/article/70b3f70b64984bbab63483d160de48c7
Publikováno v:
Pamukkale University Journal of Engineering Sciences, Vol 15, Iss 2, Pp 253-262 (2009)
Pasinler (Erzurum) kuzeyinde Üst Miyosen-Pliyosen yaşlı volkanik kayaçlar yüzeylemektedir. Bu volkanitler bazaltik andezit, andezit, dasit, riyolit türü lav ve riyolitik piroklastiklerden oluşmaktadır. Kayaçlarda porfirik, mikrolitik porfir
Externí odkaz:
https://doaj.org/article/5d6425d27aee4d5984191169b5210251
Publikováno v:
Pamukkale University Journal of Engineering Sciences, Vol 15, Iss 2, Pp 253-262 (2009)
In the north of Pasinler (Erzurum), Upper Miocene-Pliocene volcanic rocks crop out. These volcanites are composed of basaltic andesite, andesite, dacite, rhyolite lavas and rhyolitic pyroclastics. The rocks show porphyritic, microlitic porphyritic, h
Externí odkaz:
https://doaj.org/article/0c142477bccf47479f63d18e5538b5c9
Publikováno v:
Pamukkale University Journal of Engineering Sciences, Vol 15, Iss 2, Pp 253-262 (2009)
Pasinler (Erzurum) kuzeyinde Üst Miyosen-Pliyosen yaşlı volkanik kayaçlar yüzeylemektedir. Bu volkanitler bazaltik andezit, andezit, dasit, riyolit türü lav ve riyolitik piroklastiklerden oluşmaktadır. Kayaçlarda porfirik, mikrolitik porfir
Externí odkaz:
https://doaj.org/article/055d200ae84547fca736ec19f09b7b78
Publikováno v:
Pamukkale University Journal of Engineering Sciences, Vol 12, Iss 2, Pp 249-258 (2006)
Biyotit granitoidler başlıca kuvars, biyotit, plajiyoklas, K-feldispat, muskovit nadiren amfibol içerirler. Tali bileşen olarak apatit, zirkon, allanit ve ikincil olarak klorit ve serisit içerirler. Anklavlar başlıca plajiyoklas, amfibol, ojit
Externí odkaz:
https://doaj.org/article/1475a3ff3b35416aa91f64983be16c7b
Publikováno v:
Pamukkale University Journal of Engineering Sciences, Vol 12, Iss 2, Pp 249-258 (2006)
Biotite granitoid contain mainly quartz, biotite, plagioclase, K-feldspar, muscovite as main phases with minor amphiboles, and apatite, zircon, allanite and chlorite and serisite as accessory components. In contrast, enclaves are composed mainly of p
Externí odkaz:
https://doaj.org/article/81962c2aa3064f8f869afa1e28aaa283
TEPEKENT (KONYA-ORTA ANADOLU) YÖRESİNDEKİ VOLKANİK KAYALARIN PETROGRAFİSİ, JEOKİMYASI VE PETROLOJİSİ
Publikováno v:
Konya Journal of Engineering Sciences. :1002-1018
Bu çalışmada, Tepekent yöresi (Konya-Orta Anadolu) yüzeyleyen Miyosen yaşlı riyolitik, dasitik ve bazaltik lav akıntıları ve bunların piroklastiklerinin petrografisi, mineralojisi, jeokimyası ve petrolojisi incelenmiştir. İncelenen kaya
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f72ce465d24051fb1811b701bcde191f
https://doi.org/10.36306/konjes.1165649
https://doi.org/10.36306/konjes.1165649
Autor:
Mesut Gündüz, Kürşad Asan
Publikováno v:
Mineralogical Magazine. 87:1-9
Igneous rock forming minerals carry valuable information from the deep earth that is not directly accessible at the surface. Each mineral represents the physico-chemical conditions at which various magmatic processes have occured over a wide range of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::649504d3c403af28d6b37e5eb2b3093d
https://doi.org/10.1180/mgm.2022.113
https://doi.org/10.1180/mgm.2022.113
