Provenance of clay minerals in the sediments from the Pliocene Productive Series, western South Caspian Basin

被引:24
作者
Abdullayev, Elshan [1 ]
Leroy, Suzanne A. G. [2 ]
机构
[1] Univ Leipzig, Inst Geophys & Geol, Talstr 35, D-04103 Leipzig, Germany
[2] Brunel Univ London, Environm Sci, Kingston Lane, Uxbridge UB8 3PH, Middx, England
关键词
Clay minerals; Provenance; South Caspian sea; PALEOCLIMATIC INTERPRETATION; AZERBAIJAN; SEA; SOILS;
D O I
10.1016/j.marpetgeo.2016.03.002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The research work presents clay mineral composition in the sediment of the Pliocene Productive Series from western South Caspian Basin and identify potential source areas for the different research regions. The Productive Series is a main reservoir unit in the South Caspian Basin and divided into a lower division and an upper division. The clay mineral assemblages document coinciding changes in provenance. At the time of the deposition of the Lower Division, the Russian Platform was a potential source area for the Absheron Peninsula and drained by Palaeo-Volga River. However, at the time deposition of the Upper Division three different sediment source could be identified for the three research areas: Absheron Peninsula the Russian Platform was drained by the Palaeo-Volga; South Absheron Offshore Zone the Greater Caucasus was drained by the Palaeo Samur River; Baku Archipelago - the Lesser Caucasus was drained by the Palaeo-Kura River. (C) 2016 The Authors. Published by Elsevier Ltd.
引用
收藏
页码:517 / 527
页数:11
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