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Mineralogy, geochemistry and physical properties of bentonites from the Western Thrace Region and the islands of Samos and Chios, East Aegean, Greece

机译:西色雷斯地区以及希腊东爱琴海的萨摩斯岛和希俄斯岛的膨润土的矿物学,地球化学和物理性质

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摘要

Greece is a major bentonite producer, with Milos Island being one of the largest bentonite mining centres in the world. In addition to the bentonite deposits which are well known, various other occurrences exist in the islands of Chios and Samos, Eastern Aegean and in some areas of Thrace, in NE Greece. These bentonites are associated with volcanic activity and their age ranges from Lower Oligocene in Thrace, to Lower-Middle Miocene in Chios and to Upper Miocene in Samos. Although some of these materials have been utilized since ancient times (e.g. the Samian Earth), these bentonites have been mined only at a local scale. In this study the first data on the mineralogical and geochemical characteristics of these bentonites are presented.
机译:希腊是主要的膨润土生产国,米洛斯岛是世界上最大的膨润土开采中心之一。除了众所周知的膨润土矿床外,在希腊东北部的希俄斯和萨摩斯岛,东爱琴海和色雷斯的某些地区还存在其他各种矿床。这些膨润土与火山活动有关,其年龄范围从色雷斯的下渐新世,希俄斯的中下中新世和萨摩斯的上中新世。尽管这些材料中的一些自古以来就已被利用(例如萨满地球),但这些膨润土仅在当地规模开采。在这项研究中,提供了有关这些膨润土的矿物学和地球化学特征的第一批数据。

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