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The Neoproterozoic Noonday Formation, Death Valley region, California: Reply

机译:加利福尼亚死亡谷地区新元古代正午组:回复

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摘要

Because our paper was focused on the stratigraphy of the Noonday Formation and the upper part of the underlying Wildrose Diamictite of the Kingston Peak Formation, we did not dwell on the structural geology, beyond presentation of geologic maps and photographs of our measured sections, and description of structural complexities, where appropriate, in our detailed stratigraphic sections in the GSA Data Repository.1 All metamorphic tectonites, as a definitional matter, are metamorphic rocks, but it is not the case that all metamorphic rocks are tectonites, or that they everywhere absorb large amounts of penetrative strain. We welcome this opportunity to summarize previous work bearing on this issue in Neoproterozoic strata exposed in the central and northern Panamint Range, and present additional photodocumentation demonstrating that our measured stratigraphic sections are structurally intact.
机译:因为我们的论文集中于正午组的地层和金斯敦峰组的底层野玫瑰铁矾的上部,所以除了介绍地质图和实测断面的照片以及描述外,我们没有详细介绍结构地质GSA数据存储库中详细的地层部分中,对结构复杂性进行了分析。1作为定义,所有变质构造岩都是变质岩,但并非所有变质岩都是构造岩,也不是到处都吸收大量的穿透力。我们欢迎有此机会总结在Panamint山脉中部和北部暴露的新元古代地层中有关此问题的先前工作,并提供其他照片记录,证明我们测得的地层剖面在结构上是完整的。

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  • 来源
    《GSA Bulletin》 |2013年第2期|p.252-255|共4页
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    1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA 2Department of Earth Sciences, University of St. Andrews, St. Andrews, KY16 9AL, Scotland/UK 3Scottish Universities Environmental Research Centre, East Kilbride, G75 0QF, Scotland/UK;

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