Уважаемые коллеги, доброго времени суток! Представляем вам турецкое научное издание Turkish Journal of Earth Sciences. Журнал имеет третий квартиль, его SJR за 2020 г. равен 0,356, пятилетний импакт-фактор - 1,435, печатный ISSN - 1300-0985, электронный - 1303-619X, предметная область - Науки о Земле. Вот так выглядит обложка:
Редактором является Орхан Татар, контактные данные - orhantatar@cumhuriyet.edu.tr, orhantatar@gmail.com, earth@tubitak.gov.tr.
Журнал издается в электронном виде 6 раз в год Советом по научным и технологическим исследованиям Турции (TÜBİTAK). Это международный англоязычный журнал для публикации значительных оригинальных недавних исследований по широкому спектру тем в науках о Земле, таких как геология, структурная геология, тектоника, седиментология, геохимия, геохронология, палеонтология, магматическая и метаморфическая петрология, минералогия. , биостратиграфия, геофизика, геоморфология, палеоэкология и океанография, месторождения полезных ископаемых. Участие открыто для исследователей со всего мира.
Адрес издания - https://journals.tubitak.gov.tr/earth/index.htm;jsessionid=DF87A4F5C60D2E112A9CF16804F466B5#
Пример статьи, название - The multidisciplinary approaches on facies developments and depositional systems of the Bahçecik travertines, Gümüşhane, NE-Turkey. Заголовок (Abstract) - The Bahçecik travertines, located in Gümüşhane (NE-Turkey) have been investigated for the first time using a multidisciplinary approach, which included sedimentological (lithofacies, depositional system), petrographic, radiometric 230Th dating, geochemical analysis (stable isotopes), palynomorphs and geophysics (GPR). A carbonate build-up, 12 m thick, was formed with some interruptions, through the middle Pleistocene period. For this study, two travertine sections (F and D) were extensively used to figure out palaeoenvironmental and palaeoclimatic proxies. The main precipitation cycles, separated by palaeosol levels, have been described and interpreted from a sedimentological perspective. The carbonate deposits consist of shrubs, crystalline crust, reed, laminated (micritic), pisoids, oncoids, calcite thin rafts and coated gas bubbles, lithoclasts, and palaeosol levels. The sedimentological fieldwork and petrographic analysis show that the Bahçecik travertines formed in depression depositional and slope depositional systems. Moreover, the first 230Th ages, stable isotopic results and palynofloral data in this study, prove that the Bahçecik travertines might have been affected by climatic and tectonic interruptions. According to dating results, the travertine occurrences began to precipitate during the 353 ka and continued into the 263 ka. Based on the palynological data, an abundance of herbaceous plants species was recorded in the warming period of climate. The thickness ranges from 2 to 12 m of the Bahçecik travertines. This precise thickness and also the presence of two different travertine formations, separated by a palaeosol erosional surface, were recorded by the ground penetrating radar (GPR) geophysical method. Key words: Travertine, depositional system, radiometric dating, stable isotopes, middle Pleistocene, Gümüşhane