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Study of heterogeneous fabric and texture within a quartz-feldspar mylonite using the photometric method

机译:用光度法研究石英长石my石中的异质织物和质地

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摘要

In a quartz-feldspar mylonite specimen from the Darling fault zone, Western Australia, the quartz c-axis fabrics were analyzed using a combination of the conventional universal-stage methods and the photometric method of determining fabric variations. Previously existing techniques for gauging fabric homogeneity proved laborious; therefore, detailed analysis was performed using the photometric approach. The results were considered in relation to grain morphological characteristics, and three types of quartz grains were recognized. Domains of each of these types of grains exhibited different c-axis fabrics. Spatial distribution of fabric parameters determined from the photometric data revealed the degree and nature of fabric heterogeneity. It is suggested that these variations in fabric are the result of variable strain produced by the action of a uniform stress on a layered material in which alternate layers have different rheological properties related to the proportion of quartz and feldspar.
机译:在澳大利亚西部达令断层 地带的石英长石镍铁矿标本中,采用常规通用阶段方法的组合对石英c轴织物进行了分析。 > 和确定织物变化的光度法。 先前用于测量织物均匀性的技术证明很费力;因此,使用光度法进行了详细的分析 。将结果与晶粒形态特征相关,认为是 ,并识别出三种 类型的石英晶粒。这些 类型的每种晶粒的畴都表现出不同的c轴结构。由光度法测定的织物参数的空间 分布表明织物异质性的程度和性质。 建议织物中的这些变化是由均匀应力作用在层状材料上产生的可变应变的结果 ,在该层状材料中,交替层的流变特性与比例有关石英和 长石。

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  • 来源
    《GSA Bulletin》 |1978年第9期|1359-1372|共14页
  • 作者

    GRAHAM P. PRICE;

  • 作者单位

    Commonwealth Scientific and Industrial Research Organization, Division of Applied Geomechanics, Syndal, Victoria, Australia;

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  • 正文语种 eng
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