{"id":4440,"date":"2024-12-24T11:02:53","date_gmt":"2024-12-24T07:02:53","guid":{"rendered":"https:\/\/journal.geonatres.az\/?p=4440"},"modified":"2026-02-13T12:26:06","modified_gmt":"2026-02-13T08:26:06","slug":"serqi-azerbaycan-erazisinin-paleomuhitinin-erken-ve-orta-miosen-dovrunde-tekamulu-islamdag-kesilisi-uzre","status":"publish","type":"post","link":"https:\/\/journal.geonatres.az\/en\/serqi-azerbaycan-erazisinin-paleomuhitinin-erken-ve-orta-miosen-dovrunde-tekamulu-islamdag-kesilisi-uzre\/","title":{"rendered":"EVOLUTION OF PALEOENVIRONMENT OF EAST AZERBAIJAN IN THE EARLY AND MIDDLE MIOCENE ACCORDING TO ISLAMDAG SECTION"},"content":{"rendered":"

Y.N.Tahiyeva, R.A.Fataliyev, A.I.Aliyev<\/strong><\/p>\n

tagelena@rambler.ru, r.fataliyev@mail.ru<\/p>\n

DOI: 10.59423\/gnr.2024.32.69.007<\/a><\/p>\n

Annotation<\/strong>. Debris indicators, weathering indices, and palynomorph assemblages in a study of Early to Middle Miocene environmental conditions along the Islamdagh section in East Azerbaijan revealed early Miocene arid conditions, reduced weathering rates, and poorly oxygenated deep water basin sediments with above-average oceanic salinities. (above 40 o\/oo). In the middle of the Early Miocene, a transition to humid conditions and oxygenation of the water column was observed. Further long-term aridification into the flesh until the Middle Miocene occurred in a lacustrine or shelf environment of a less saline (30-18 o\/oo) and more oxygenated water basin, which made these marine deposits excellent source rocks compared to time-equivalent terrestrial deposits. Geochemical and palynological indicators suggest that, although the Cenozoic was a period of global cooling, East Azerbaijan at this time was characterized by a warm, moderately humid to arid climate.<\/p>\n

Keywords<\/strong>: Paratethys, Greater Caucasus, Miocene, section, sediments, clay minerals, climatic conditions, paleoenvironment.<\/p>\n

References<\/strong><\/p>\n

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    Accepted for publication<\/strong>: November 15, 2024.<\/p>\n

    Download article<\/strong><\/p>\n

    Y.N.Tahiyeva, R.A.Fataliyev, A.I.Aliyev<\/strong> \u2013 Evolut\u0131on of paleoenv\u0131ronment of East Azerbaijan in the early and middle miocene according to Islamdagh section. Geography and Natural Resources, \u21162 (22), 2024, pp. 40-46.<\/p>\n

     <\/p>\n","protected":false},"excerpt":{"rendered":"

    Y.N.Tahiyeva, R.A.Fataliyev, A.I.Aliyev tagelena@rambler.ru, r.fataliyev@mail.ru DOI: 10.59423\/gnr.2024.32.69.007 Annotation. Debris indicators, weathering indices, and palynomorph assemblages in a study of Early to Middle Miocene environmental conditions along the Islamdagh section in East Azerbaijan revealed early Miocene arid conditions, reduced weathering rates, and poorly oxygenated deep water basin sediments with above-average oceanic salinities. (above 40 o\/oo). In […]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[],"class_list":["post-4440","post","type-post","status-publish","format-standard","hentry","category-mqallr"],"blocksy_meta":[],"yoast_head":"\nEVOLUTION OF PALEOENVIRONMENT OF EAST AZERBAIJAN IN THE EARLY AND MIDDLE MIOCENE ACCORDING TO ISLAMDAG SECTION<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/journal.geonatres.az\/en\/serqi-azerbaycan-erazisinin-paleomuhitinin-erken-ve-orta-miosen-dovrunde-tekamulu-islamdag-kesilisi-uzre\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:locale:alternate\" content=\"az\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"EVOLUTION OF PALEOENVIRONMENT OF EAST AZERBAIJAN IN THE EARLY AND MIDDLE MIOCENE ACCORDING TO ISLAMDAG SECTION\" \/>\n<meta property=\"og:description\" content=\"Y.N.Tahiyeva, R.A.Fataliyev, A.I.Aliyev tagelena@rambler.ru, r.fataliyev@mail.ru DOI: 10.59423\/gnr.2024.32.69.007 Annotation. Debris indicators, weathering indices, and palynomorph assemblages in a study of Early to Middle Miocene environmental conditions along the Islamdagh section in East Azerbaijan revealed early Miocene arid conditions, reduced weathering rates, and poorly oxygenated deep water basin sediments with above-average oceanic salinities. (above 40 o\/oo). 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Debris indicators, weathering indices, and palynomorph assemblages in a study of Early to Middle Miocene environmental conditions along the Islamdagh section in East Azerbaijan revealed early Miocene arid conditions, reduced weathering rates, and poorly oxygenated deep water basin sediments with above-average oceanic salinities. (above 40 o\/oo). In […]","og_url":"https:\/\/journal.geonatres.az\/en\/serqi-azerbaycan-erazisinin-paleomuhitinin-erken-ve-orta-miosen-dovrunde-tekamulu-islamdag-kesilisi-uzre\/","og_site_name":"Geography and Natural Resources","article_published_time":"2024-12-24T07:02:53+00:00","article_modified_time":"2026-02-13T08:26:06+00:00","og_image":[{"width":1536,"height":1024,"url":"https:\/\/journal.geonatres.az\/wp-content\/uploads\/2026\/03\/ChatGPT-Image-27-\u043c\u0430\u0440.-2026-\u0433.-01_39_18.png","type":"image\/png"}],"author":"Sarkhan Jafarov","twitter_card":"summary_large_image","twitter_misc":{"Written by":"Sarkhan Jafarov","Est. reading time":"8 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