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Using geologic structures to constrain constitutive laws not accessible in the laboratory

机译:利用地质结构来限制实验室无法访问的本构规定

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In this essay, we explore a central problem of structural geology today, and in the foreseeable future, which is the determination of constitutive laws governing rock deformation to produce geologic structures. Although laboratory experiments provide much needed data and insights about constitutive laws, these experiments cannot cover the range of conditions and compositions relevant to the formation of geologic structures. We advocate that structural geologists address this limitation by interpreting natural experiments, documented with field and microstructural data, using continuum mechanical models that enable the deduction of constitutive laws. To put this procedure into a historical context, we review the founding of structural geology by James Hutton in the late 18th century, and the seminal contributions to continuum mechanics from Newton to Cauchy that provide the tools to model geologic structures. The procedure is illustrated with two examples drawn from recent and ongoing field investigations of crustal and mantle lithologies. We conclude by pointing to future research opportunities that will engage structural geologists in the pursuit of constitutive laws during the 21st century.
机译:在本文中,我们今天探索了结构地质的核心问题,在可预见的未来,这是对管理地质结构产生地质结构的本构规定的确定。尽管实验室实验提供了大量需要的数据和关于本构规则的见解,但这些实验不能涵盖与地质结构形成相关的条件和组合物。我们倡导结构地质学家通过解释具有现场和微观结构数据的自然实验来解决这种限制,使用连续的机械模型,使得构成术法扣除。为了将此程序纳入历史背景下,我们在18世纪后期的詹姆斯·赫顿审查了结构地质的创立,以及从牛顿到Cauchy的连续力学的开创性贡献,为模型地质结构提供了工具。该程序用来自地壳和地幔岩性的最近和持续的场地调查的两个例子说明。我们通过指出未来的研究机会,将在21世纪追求构成性地质学家的未来研究机会。

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