首页> 外文会议>Trilateral Meeting on Clays >FIRST APPROACH TO THE CLAY MINERALOGY OF THE KAOLIN-RICH SEDIMENTARY DEPOSITS FROM THE WEALD FACIES IN THE IBERIAN RANGE (NE SPAIN)
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FIRST APPROACH TO THE CLAY MINERALOGY OF THE KAOLIN-RICH SEDIMENTARY DEPOSITS FROM THE WEALD FACIES IN THE IBERIAN RANGE (NE SPAIN)

机译:首先是伊比利亚人范围(NE西班牙)的WEALD相片中富有的高岭土沉积沉积物粘土矿物质

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The aim of this study is to characterize the clay mineral associations from the clayey sedimentary deposits of the Lower Cretaceous (Weald facies) in Maestrazgo basin (Teruel, NE Spain). These deposits, that are rich in kaolin minerals, are actively mined by the ceramic industry (sanitaryware). The studied rocks (ciaystones, siltstones and sandstones) constitute the Camarillas Formation (Barremian) and correspond to a fluvial environment. Most of these materials display red colors although there are also greenish and grey levels. The formation represents a fluvial system of multiple low sinuosity channels, evolving towards the top to a delta plain, with tidal influence (Diaz-Molina & Yebenes, 1987). A systematic sampling (45 samples) has been performed in two sections in the Maestrazgo basin: in an open pit nowadays mined close to Galve (Calve section) and in other outcrop at 50 km (Miravete section).
机译:本研究的目的是将粘土矿物协会从Maestrazgo盆地(Teruel,Ne Spain)的下白垩纪(WEALD相机)的粘土沉积物沉积物沉积物沉积物。这些富含高岭土的沉积物,由陶瓷工业(卫生洁具)主动开采。学习的岩石(Ciaystones,Siltstones和砂岩)构成了Camarillas的形成(Barremian),对应于河流环境。这些材料中的大多数显示红颜色,尽管还有绿色和灰度水平。该形成代表多个低态度通道的河流系统,以潮汐影响(Diaz-molina和Yeebenes,1987)而发展为迄今为止趋向于δ平原。系统采样(45个样本)已经在Maestrazgo盆地的两部分中进行:在现在的露天坑中,靠近Galve(Calve Section)和50公里的其他露头(Miravete截面)。

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