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Chocolate clays of the Northern Caspian Sea Region: Distribution, structure, and origin

机译:北里海地区的巧克力黏土:分布,结构和成因

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The chocolate clays commonly comprise a part of the Lower Khvalynian sequence in the northern Caspian Lowland and in the Volga region. The mode of occurrence varies from continuous to patchy mosaic. All the clay deposits are confined to Pre-Khvalynian depressions of various origins. There are several sub-facies distinguishable within the chocolate clay facies: mono-clayey (typologic), stratified sandy-clayey and silty-clayey. Judging from specific features of lithology, geomorphic position, mode of occurrence, mollusc fauna composition, and radiocarbon dates, the chocolate clays represent a specific facies of the Lower Khvalynian sediments and cannot be considered as an individual stratigraphic unit. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:巧克力黏土通常在里海北部低地和伏尔加河地区包括下哈瓦利南层序的一部分。发生的模式从连续到斑驳的马赛克不等。所有的粘土沉积物都局限于各种起源的哈瓦林前凹陷。巧克力黏土相中有几个可区分的亚相:单黏土(典型),分层的沙质黏土和粉质黏土。从岩性,地貌位置,发生方式,软体动物区系组成和放射性碳年代等特定特征来判断,巧克力黏土代表了下哈瓦利尼亚沉积的特定相,不能被视为一个独立的地层单元。 (C)2015 Elsevier Ltd和INQUA。版权所有。

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