Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Yeşim Yücel-Öztürk"'
The Late Miocene igneous rocks of the Bodrum magmatic complex (SW Anatolia, Turkey), are composed of small monzonitic intrusions and trachyandesite-trachydacite volcanic rocks. The Kadıkalesi monzonite (KM) forms a small stock (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b8b734f9465a90601ee69984368838b0
https://avesis.deu.edu.tr/publication/details/737dd6e3-d95c-4d8a-8ad9-fe20956f0c0a/oai
https://avesis.deu.edu.tr/publication/details/737dd6e3-d95c-4d8a-8ad9-fe20956f0c0a/oai
Autor:
Yeşim Yücel-Öztürk
The O and H isotopic ratios of borates, clay minerals, and volcanic rocks from the Kırka basin (south of Eskişehir, W Anatolia) have been analysed in order to better constrain the conditions that led to precipitation of the borates. The δ18Owr val
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::359071a61d1b0d8313ee3d7c4d176ecf
https://avesis.deu.edu.tr/publication/details/c5e7b289-4718-4fc3-95b4-e2eac0ec22e2/oai
https://avesis.deu.edu.tr/publication/details/c5e7b289-4718-4fc3-95b4-e2eac0ec22e2/oai
Autor:
Yeşim YÜCEL ÖZTÜRK, Cüneyt AKAL
Publikováno v:
Türkiye Jeoloji Bülteni / Geological Bulletin of Turkey.
Spherulitic structures are classically defined as concentrically zoned crystal clusters that form in igneous systems (especially in alkaline igneous rocks), and usually occur as different mineral layers or shells. The volcano-sedimentary series obser
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c749b6bb9a90eb2d5492c13f80c3d9cd
https://doi.org/10.25288/tjb.1084686
https://doi.org/10.25288/tjb.1084686
Publikováno v:
International Geology Review. 63:1719-1736
The formation of large, economic borate deposits requires a boron-rich source, the means of transporting and concentrating the boron in a restricted environment, and mechanisms for the preservation of the deposit. There are several Miocene basins in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cfc61f31afa4e121a1dd50beb262c7c4
https://doi.org/10.1080/00206814.2020.1793422
https://doi.org/10.1080/00206814.2020.1793422
Publikováno v:
Lithos (0024-4937) (Elsevier Science Bv), 2015-03, Vol. 218, P. 22-36
In the western central portion of Anatolia lies the Menderes Massif - a large metamorphic crystalline complex made of Neoproterozoic to Precambrian basement rocks overlain by Palaeozoic to early Tertiary metasedimentary rocks, and with a multistage m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6fe32f6c40990efc79d9f6ffb587b58b
https://doi.org/10.1016/j.lithos.2015.01.009
https://doi.org/10.1016/j.lithos.2015.01.009
Autor:
Yeşim Yücel-Öztürk
The oxygen and strontium isotope compositions of Cenozoic granitoids cropping out in the Izmir-Ankara-Erzincan suture zone help constrain the petrological evolution of magmatism in northwest Anatolia. The magmatism was mostly widespread between late
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0b8d25816164adf02f4360e659b732ad
https://avesis.deu.edu.tr/publication/details/e34c737e-fee8-48d7-ae98-7820375b79e1/oai
https://avesis.deu.edu.tr/publication/details/e34c737e-fee8-48d7-ae98-7820375b79e1/oai