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首页> 外文期刊>Geological Society of America Bulletin >The Neoproterozoic Noonday Formation, Death Valley region, California: Reply
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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 photodocumen-tation demonstrating that our measured strati-graphic sections are structurally intact.
机译:因为我们的论文集中在Noonday组的地层和金斯敦峰组的底层Wildrose菱铁矿的上部,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山脉中部和北部裸露的新元古代地层中有关此问题的先前工作,并提出其他光电子学证据,证明我们测得的地层剖面在结构上是完整的。

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