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Genesis and mineral transformations in Lower Cretaceous karst bauxites (NE Spain): climatic influence and superimposed processes

机译:下白垩统喀斯特铝土矿的成因和矿物转化(西班牙东北):气候影响和叠加过程

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Four outcrops of Lower Cretaceous (Barremian) karst bauxites located in Teruel (NE Spain) were analysed to determine their mineral associations and genesis related to climatic palaeoweathering events and late superimposed kaolinization processes. The materials comprise metric-sized pisolitic blocks embedded in a clay-rich red groundmass. Fourteen samples were examined by X-ray diffraction, optical microscopy, scanning and transmission electron microscopy and the major elements were analysed by inductively-coupled plasma mass spectroscopy (ICPMS). The samples are composed of kaolinite, gibbsite, goethite, and hematite as the main phases, with diaspore, boehmite, anatase, and rutile as accessory minerals. The results show a complex sequence of mineralogical and geochemical processes that transformed the parent rock into the current bauxite materials. The clay-rich groundmass constitutes the lateritic parent material of the pisolitic bauxites. In the parent material authigenic kaolinite (e.g. vermicular kaolinite and kaolinite between cleavage sheets of pre-existing mica) has been observed; Fe oxides formed subsequent to kaolinite. In the pisolitic bauxites, mineralogical and textural evidence indicates that bauxitization took place at the expense of previous kaolinite, with gibbsite post-dating the other Al hydroxides. The pisolitic bauxites also show a more homogeneous chemical composition and a relative Ti, Al and Zr enrichment. The data are consistent with an intense palaeoweathering event during the Lower Cretaceous (Barremian) under tropical climatic conditions (warm and humid). Several stages probably took place during the bauxitization process, suggesting variations in water saturation conditions. Subsequent karst reactivation stages and related collapses were responsible for the present lithostructure of the deposits and allowed late kaolinization not related to climate to take place. Copyright (c) 2014 John Wiley & Sons, Ltd.
机译:分析了位于特鲁埃尔(西班牙东北部)的下白垩统(巴雷米亚)喀斯特铝土矿的四个露头,以确定它们与气候古风化事件和后期叠加高岭土化过程有关的矿物关联和成因。这些材料包括嵌入富含粘土的红色地面中的公制尺寸的蛇行岩块。通过X射线衍射,光学显微镜,扫描和透射电子显微镜检查了14个样品,并通过电感耦合等离子体质谱法(ICPMS)分析了主要元素。样品由高岭石,三水铝铁矿,针铁矿和赤铁矿为主要相,并以水辉石,勃姆石,锐钛矿和金红石为辅助矿物。结果表明,复杂的矿物学和地球化学过程序列将母体岩石转变为当前的铝土矿材料。富含粘土的地基构成了弧形铝土矿的红土母体材料。在母体材料中观察到了自生高岭石(例如蠕虫状高岭石和已存在的云母分裂片之间的高岭石);铁氧化物在高岭石之后形成。在毛硅酸铝土矿中,矿物学和组织学证据表明,铝土矿化是以先前的高岭石为代价而发生的,而三水铝石则是在其他氢氧化铝之后进行的。柱状铝土矿还显示出更均匀的化学组成和相对丰富的Ti,Al和Zr。该数据与热带气候条件(温暖和潮湿)下白垩纪(巴雷姆期)强烈的古风化事件一致。在铝土化过程中可能发生了几个阶段,表明水饱和度条件有所不同。随后的岩溶活化阶段和相关的塌陷是造成沉积物目前岩石结构的原因,并使得与气候无关的后期高岭土化发生了。版权所有(c)2014 John Wiley&Sons,Ltd.

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