澳大利亚风化玻璃上的斑驳和斑纹多样性--斑驳工艺和产品之窗

V. &. C. Semeniuk
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引用次数: 0

摘要

玻璃风化的结果是形成超薄的铜绿岩,这种铜绿岩呈现出多种结构、微结构和微岩层,记录了其(地质)成因和成岩过程。澳大利亚铜绿泥的扫描电子显微镜显示,铜绿泥有简单层状、复杂层状、胶体状、微碎屑状、斑驳状和凝块状,并伴有微观结构和层状二氧化硅或层状二氧化硅与方解石之间的微观岩性。这些层内特征被称为 "斑纹"。此外,还有干燥裂缝、凹槽和灰尘外渗。这些结构、微观结构和微观岩性以透镜状、片状和铜绿岩内部块状排列。铜绿斑结构和微观岩性以及斑岩的多样性可用于确定铜绿斑和斑岩的历史。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Diversity of Patina and Patinelles on Weathered Glass in Australia –Windows into Processes and Products In Patination
Weathering of glass results in an ultra-thin patina that exhibits a multitude of structures, micro-structures, and microlithologies that record its (geological) paragenesis and diagenesis. Scanning electron microscopy of patina from Australia shows it to be simply laminated, complexly laminated, colloform, to micro-brecciated, to mottled and clotted, with microunconformities, and micro-lithologies of laminated silica, or inter-laminated silica and calcite. These intra-patina features are termed ‘patinelles’. There are also desiccation cracks, vughs, and exogenic infiltrations of dust. This range of structures, micro-structures, and micro-lithologies are arrayed as lenses, sheets and as intra-patina masses. The diversity of patina structures and micro-lithologies, and patinelles can be used to determine the history of patina and patinelles.
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