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Denticles on Chain Silicate Grain Surfaces and Their Utility as Indicators of Weathering Conditions on Earth and Mars

机译:硅酸盐链状颗粒表面的齿状体及其作为地球和火星风化状况指标的效用

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摘要

Denticulated margins (also known in older literature as "sawtooth," "cockscomb," or "hacksaw" terminations) are a common feature of pyroxenes and amphiboles, visible in optical and electron microscopes. Denticles are remnants of undissolved material that formerly constituted the walls between elongate etch pits, the characteristic aqueous-dissolution form of chain-silicate minerals. Denticles occur widely in terrestrial near-surface materials that have experienced low-temperature aqueous alteration, including chemically weathered regoliths, soils in a variety of climatic and geomorphic settings, sediments, and sedimentary rocks. Ranges of dissolution forms and dimensions (commonly tens of microns in length) are identical on both pyroxenes and amphiboles in these materials.
机译:锯齿状边缘(在较早的文献中也称为“锯齿”,“ ” cockscomb”或“钢锯”端接)是辉石和闪石的常见特征,在光学和可见电子 显微镜。细粒是未溶解物质的残留物,以前构成细长蚀刻坑之间的壁,是链状硅酸盐矿物的特征性水溶形式。在经历了低温水蚀变化的地面近地物质中,广泛存在着细小颗粒,其中包括化学风化的碎石,各种气候下的土壤。sups 和地貌设置,沉积物和沉积物 岩石。在这些材料中,辉石和 amphiboles的溶解形式和尺寸范围(通常 长度为数十微米)是相同的。

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    《Journal of Sedimentary Research》 |2010年第9期|00000771-00000780|共10页
  • 作者单位

    Department of Geological Sciences, Michigan State University, East Lansing, Michigan 48824-1115, U.S.A.velbel@msu.edu;

    Department of Geological Sciences, Michigan State University, East Lansing, Michigan 48824-1115, U.S.A.Department of Lithospheric Research, University of Vienna, Althanstrasse 14, 1090 Vienna, Austria;

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