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首页> 外文期刊>Applied clay science >Clay supply for Aguada ordinary vessels from Piedras Blancas (4th to 12th centuries AC), Ambato Valley (Argentina)
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Clay supply for Aguada ordinary vessels from Piedras Blancas (4th to 12th centuries AC), Ambato Valley (Argentina)

机译:从阿根廷安巴托山谷的皮德拉斯·布兰卡斯(公元4至12世纪)为阿瓜达普通船提供粘土

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摘要

The provenance of the raw materials used to produce ordinary ceramic vessel of the Aguada Culture (4th to 12th c. AC) from the Ambato Valley (Catamarca, Argentina) has been evaluated. Since there are no commercial clay deposits in the area, local clayish sources were selected as possible candidates. Samples were collected from Precambrian to Low Paleozoic metapelites, clays from fault gouges derived from crystalline basement rocks, epiclastic rocks and Quaternary loessic sediments that filled the valley and crop out close to the archaeological sites. The pottery sherds were found at Piedras Blancas highly hierarchical site. Mineralogical and geochemical studies were conducted by XRD and FE-SEM-EDS on both the pot sherds and the possible source materials. The latter were also preliminary evaluated on basic physical and technological properties; test specimens were heated at different temperatures (800, 900 and 1000 degrees C) to study their thermal behavior and their mineralogical and textural transformations. The physical properties of the metapelites, the clay gouges and the loessic sediments suggest that they are suitable for ceramic production. The epiclastic rocks are mostly bentonitic and could have been used as additives to improve the plasticity and other properties of other clay materials. The mineralogy of the sherds is quite homogeneous with no significant differences between technological classes E and D; most of them bear either phlogopite, hornblende and/or hypersthene and high temperature phases (diopside, spinel, mullite and cristobalite) also found in some clays under natural conditions or after firing at 1000 degrees C. Commonly used provenance geochemical ratios are relatively similar in all pottery samples and in the selected source rocks and comparable with typical UCC. Hence, according to those values, all samples are related to each other and indistinguishable except for one sample (B30) highly enriched in REE. Nearly all raw materials and ceramics are either enriched in Cs, Bi, Sb or in any of these elements. The trend of using local materials for the pottery is suggested by the mineralogy and the geochemistry. (C) 2016 Elsevier B.V. All rights reserved.
机译:已评估了用于从Ambato谷(阿根廷卡塔马卡)生产普通瓜陶文化(公元前4到12世纪)的陶瓷容器的原料来源。由于该地区没有商业黏土矿床,因此选择了当地黏土资源作为可能的候选地。样品采集自前寒武纪到低古生代的变质岩,断层泥中的粘土,这些断层泥是从形成于山谷中的结晶基底岩,表生碎屑岩和第四纪黄土沉积物衍生出来的,并靠近考古现场。在彼德拉斯·布兰卡斯(Piedras Blancas)的高等级遗址中发现了陶器棚。 XRD和FE-SEM-EDS分别对盆架和可能的原料进行了矿物学和地球化学研究。还对后者的基本物理和技术特性进行了初步评估;在不同的温度(800、900和1000摄氏度)下加热试样,以研究其热行为以及矿物学和组织学转变。变质岩,粘土凿和黄土沉积物的物理性质表明它们适用于陶瓷生产。表生碎屑岩大多为膨润土,可以用作添加剂来改善其他粘土材料的可塑性和其他性能。麦片的矿物学是相当均匀的,在技术等级E和D之间没有显着差异。它们中的大多数都具有金云母,角闪石和/或超菱形,高温相(透辉石,尖晶石,莫来石和方石英)也存在于某些粘土中,它们是在自然条件下或在1000摄氏度下煅烧后发现的。所有陶器样品以及选定的烃源岩中的样品,都可以与典型的UCC相提并论。因此,根据这些值,除了一个样品(B30)的稀土元素高度富集之外,所有样品都是相互关联且无法区分的。几乎所有原材料和陶瓷都富含Cs,Bi,Sb或这些元素中的任何一种。矿物学和地球化学表明了将当地材料用于陶器的趋势。 (C)2016 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Applied clay science》 |2016年第10期|158-174|共17页
  • 作者单位

    IFEG CONICET, Medina Allende S-N,Cdad Univ, Cordoba, Argentina;

    Univ Nacl Cordoba, Fac Filosofia & Humanidades, Museo Antropol, IDACOR CONICET, Ave Hipolito Irigoyen 174, RA-5000 Cordoba, Argentina;

    Univ Stavanger, Dept Petr Engn, N-4036 Stavanger, Norway;

    Univ Nacl Cordoba, Fac Filosofia & Humanidades, Museo Antropol, IDACOR CONICET, Ave Hipolito Irigoyen 174, RA-5000 Cordoba, Argentina;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Aguada Ambato Culture; Ordinary ceramic; Mineralogy; Geochemistry; Provenance;

    机译:Aguada Ambato文化;普通陶瓷;矿物学;地球化学;物产;

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