{"id":15,"date":"2019-03-16T11:03:36","date_gmt":"2019-03-16T11:03:36","guid":{"rendered":"http:\/\/journal.geonatres.az\/?p=15"},"modified":"2019-07-23T22:55:21","modified_gmt":"2019-07-23T18:55:21","slug":"meqale-1","status":"publish","type":"post","link":"https:\/\/journal.geonatres.az\/en\/meqale-1\/","title":{"rendered":"CLAY MINERALS OF THE PRODUCTIVE SERIES (SURAKHANY SUITE) AND ITS PALAEOCLIMATIC SIGNIFICANCE"},"content":{"rendered":"<p style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\"><strong>Y.N.Taghiyeva, Z.N.Javadzade, E.A.Abdullayev<\/strong><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\"><strong>Abstract.\u00a0<\/strong>The clay minerals can be significant indicator of pa\u00adlaeoclimate. Only detrital clay minerals without any diagenetic alternation may be used in reconstruction pa\u00adlaeoweathering which is controlled by climate. The re\u00adsults showed that the sediments of Surakhany Suite (Up\u00adper Division of the productive Series) is characterised by high amount of illite. It indicates that palaeoclimate was arid in source area, which was the Russian Platform. However high amount of smectite in interval 1-2.1 m suggest relatively humid climate in the Russian Platform for the time.<\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\"><strong>REFERENCES<\/strong><\/span><\/p>\n<ol>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">A\u011fayev, A.A., \u00c7\u00f6km\u0259 procesl\u0259rin geokimyas\u0131. Adil o\u011flu, Baku. 136 s.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">\u0410\u043b\u0438\u0435\u0432\u0430 \u042d.\u0413., \u0410\u043b\u0438\u0435\u0432 \u0427.C., \u0413\u0443\u0441\u0435\u0439\u043d\u043e\u0432 \u0414.\u0410., \u0411\u0430\u00ad\u0431\u0430\u0435\u0432 \u0428.\u0410., \u041c\u0430\u043c\u0435\u0434\u043e\u0432 \u0420. M. 2008. \u0423\u0441\u043b\u043e\u0432\u0438\u044f \u0441\u0435\u0434\u0438\u00ad\u043c\u0435\u043d\u00ad\u0442\u0430\u00ad\u0446\u0438\u0438 \u043e\u0442\u043b\u043e\u0436\u0435\u043d\u0438\u0439 \u043d\u0438\u0436\u043d\u0435\u0433\u043e \u043e\u0442\u0434\u0435\u043b\u0430 \u043f\u0440\u043e\u0434\u0443\u043a\u0442\u0438\u0432\u043d\u043e\u0439 \u0442\u043e\u043b\u00ad\u0449\u0438 \u0438 \u0438\u0445 \u0435\u0441\u0442\u0435\u0441\u0442\u0432\u0435\u043d\u043d\u0430\u044f \u0440\u0430\u0434\u0438\u043e\u0430\u043a\u0442\u0438\u0432\u043d\u043e\u0441\u0442\u044c. \u0421\u0442\u0440\u0430\u0442\u0438\u00ad\u0433\u0440\u0430\u00ad\u0444\u0438\u044f \u0438 \u0441\u0435\u0434\u0438\u043c\u0435\u043d\u0442\u043e\u043b\u043e\u0433\u0438\u044f \u043d\u0435\u0444\u0442\u0435\u0433\u0430\u0437\u043e\u043d\u043e\u0441\u043d\u044b\u0445 \u0431\u0430\u0441\u0441\u0435\u0439\u043d\u043e\u0432, \u2116 2, \u0441. 91-110.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Abdullayev, E and Leroy, S. A.G. 2016. Leroy Provenance of clay minerals in the sediments from the Pliocene Productive Series, western South Caspian Basin. Marine and Petroleum Geology 73, 2016, p. 517-527.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Biscaye, P.E., Distinction between kaolinite and chlorite in recent sediments by X-ray diffraction. American Mineralogist 49, 1964, 1281\u20131289.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Biscaye, P.E., 1965. Mineralogy and sedimen\u00adtation of recent deep sea clay in the Atlantic Ocean and adjacent seas and oceans. Geological Society of Ame\u00adrica, Bulletin, 76, 803\u2013832.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Chamley, H., 1989. Clay sedimentology. Springer-Verlag, Berlin, Heidelberg, New York, 623 p.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Esquevin, J., 1969. Influence of chemical com\u00adposition of the clay on the crystallinity. Bulletin des Centres de Recherches de Pau-Societe Nationale des Petroles d\u2019 Aquitaine 3, p. 147-154.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Fagel, N., 2007 Clay minerals, deep circulation and climate. Development in Marine Geology 1, p. 139-176.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Forte, A.M., Cowgill, E., 2013. Late Cenozoic baselevel variations of the Caspian Sea: A review of its history and proposed driving mechanisms. Palaeo\u00adge\u00adography, Palaeoclimatology, Palaeoecology 386, p. 392-407.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Franke, D., Ehrmann, W., 2010. Neogene clay mineral assemblages in the AND-2A drill core (Mc Murdo Sound, Antarctica) and their implications for en\u00advironmental change. Palaeogeography, Palaeocli\u00adma\u00adto\u00adlogy, Palaeoecology 286, p. 55-65.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Gradusov, B.P., 1974. A tentative study of clay mineral distribution in soils of the world. Geoderma 12, p. 49-55.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Hinds, D.J., Aliyeva, E., Allen, M.B., Davies, C.E., Kroonenberg, S.B., Simmons, M.D., Vincent, S.J., 2004. Sedimentation in a discharge dominated fluvial-lacustrine system: the Neogene Productive Series of the South Caspian Basin, Azerbaijan. Marine and Petroleum Geology 21, p. 613\u2013638.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Meyers, P.A., Lallier-Verges, E., 1999. La\u00adcus\u00adtrine sedimentary organic matter records of Late Qua\u00adter\u00adnary paleoclimates. Journal of Paleolimnology 21, p. 345\u2013372.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Pettijohn, F.J., Potter, P.E., Siever, R., 1987. Sand and sandstone. Springer, Berlin. 552 p.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Singer, A., 1984. The paleoclimatic in\u00adter\u00adpre\u00adta\u00adtion of clay minerals in sediment a review. Earth-Sci\u00adence Reviews 21, p. 251-293.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Singer, A., 1980. The paleoclimatic inter\u00adpreta\u00adtion of clay minerals in soils and weathering profiles. Earth-Science Reviews 15, p. 303-326.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Thiry, M., 2000. Palaeoclimatic interpretation of clay minerals in marine deposits: an outlook from the continental origin. Earth-Science Reviews. 49, p. 201-221.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Tyson, R.V., Sedimentary organic matter. Chapman and Hall, Oxford, 1995, 615 p.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Vincent, S.J., Davies, C.E., Richards, K., Ali\u00adyeva, E., 2010. Contrasting Pliocene fluvial depositional systems within the rapidly subsiding South Caspian Ba\u00adsin; a case study of the Palaeo-Volga and Palaeo-Kura river systems in the Surakhany Suite, Upper Productive Series, onshore Azerbaijan. Marine and Petroleum Ge\u00adology 27, p. 2079-2106.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Wang, X., Zhang, Y., Chen, R., 2010. Distribu\u00adtion and partitioning of polycyclic aromatic hydro\u00adcar\u00adbons (PAHs) in different size fractions in sediment from Boston Harbor, United States. Marine Pollution Bulletin 42, p. 1113-1149.<\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">Weaver, C.E., 1989. Clays, Muds, and Shales. Elsevier, Amsterdam, 818 p.<\/span><\/li>\n<\/ol>\n<p><a href=\"http:\/\/journal.geonatres.az\/wp-content\/uploads\/2019\/03\/\u0415.\u041d.\u0422\u0430\u0433\u0438\u0435\u0432\u0430-2018.pdf\"><strong>Download the article<\/strong><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Y.N.Taghiyeva, Z.N.Javadzade, E.A.Abdullayev Abstract.\u00a0The clay minerals can be significant indicator of pa\u00adlaeoclimate. Only detrital clay minerals without any diagenetic alternation may be used in reconstruction pa\u00adlaeoweathering which is controlled by climate. The re\u00adsults showed that the sediments of Surakhany Suite (Up\u00adper Division of the productive Series) is characterised by high amount of illite. It indicates [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2],"tags":[],"class_list":["post-15","post","type-post","status-publish","format-standard","hentry","category-article"],"blocksy_meta":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>CLAY MINERALS OF THE PRODUCTIVE SERIES (SURAKHANY SUITE) AND ITS PALAEOCLIMATIC SIGNIFICANCE<\/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\/meqale-1\/\" \/>\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=\"CLAY MINERALS OF THE PRODUCTIVE SERIES (SURAKHANY SUITE) AND ITS PALAEOCLIMATIC SIGNIFICANCE\" \/>\n<meta property=\"og:description\" content=\"Y.N.Taghiyeva, Z.N.Javadzade, E.A.Abdullayev Abstract.\u00a0The clay minerals can be significant indicator of pa\u00adlaeoclimate. 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