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PROVENANCE OF MARBLES FROM NAXOS BASED ON MICROSTRUCTURAL AND GEOCHEMICAL CHARACTERIZATION

机译:基于微结构和地球化学特征的纳克索斯州马鞭源

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摘要

A detailed quantitative microstructural study coupled with cathodoluminescence and geochemical analyses on marbles from Naxos demonstrates that the analysis of microstructures is the most sensitive method to define the origin of marbles within, and between, different regions. Microstructure examination can only be used as an accurate provenance tool if a correction for the second-phase content is considered. If second phases are not considered, a large spread of different microstructures occurs within sample sites, making a separation between neighbouring outcrops difficult or impossible. Moreover, this study shows that the origin of a marble is defined more precisely if the microstructural observations are coupled with cathodoluminescence data.
机译:对纳克索斯岛大理石进行的详细定量微观结构研究以及阴极发光和地球化学分析表明,对微观结构的分析是定义不同区域内和之间不同区域大理石起源的最灵敏方法。如果考虑对第二相含量进行校正,则微结构检查只能用作准确的出处工具。如果不考虑第二阶段,则在样品位点内会发生大量不同微观结构的扩散,从而使相邻露头之间的分离变得困难或不可能。此外,这项研究表明,如果将微观结构观察与阴极发光数据相结合,则可以更精确地定义大理石的起源。

著录项

  • 来源
    《Archaeometry》 |2010年第2期|p.209-228|共20页
  • 作者单位

    Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, CH-3012 Bern, Switzerland;

    Muséum d'histoire naturelle, route de Malagnou 1, CH-1208 Genève, Switzerland;

    Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, CH-3012 Bern, Switzerland;

    James Cook University, School of Earth and Environmental Sciences, Townsville, Australia;

    Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, CH-3012 Bern, Switzerland;

    IGME, 70 Messoghion Street, 115 27 Athens, Greece;

    Muséum d'histoire naturelle, route de Malagnou 1, CH-1208 Genève, Switzerland;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    MARBLE; CALCITE; NAXOS; GREECE; MICROSTRUCTURE; GRAIN SIZE; CATHODOLUMINESCENCE; ISOTOPE ANALYSIS; PROVENANCE; SECOND PHASE;

    机译:大理石;钙长石;纳克索斯;希腊;微观结构;粒度;阴极发光;同位素分析;物源;第二相;
  • 入库时间 2022-08-18 00:47:52

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