首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >The dynamics and interaction of compaction bands in Valley of Fire State Park, Nevada (USA): Implications for their growth, evolution, and geostatistical property
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The dynamics and interaction of compaction bands in Valley of Fire State Park, Nevada (USA): Implications for their growth, evolution, and geostatistical property

机译:内华达州火谷州立公园的压实带的动力学和相互作用(美国):对压实带的生长,演化和地统计性质的影响

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摘要

Geometry, geostatistics and microstructures of two sets of high-angle compaction bands within Aztec Sandstone are investigated for the purpose of characterizing their dimensions, distributions, and growth dynamics. Both sets generally terminate at the dune boundaries. The first set of compaction bands is longer than the second set, which is thought to be controlled by the depositional architecture. The macroscopic thickness of single compaction bands varies from zero at their tips to maximum values, 3 to 10 mm commonly within the central parts. The compaction bands often cluster into zones, the thickness of which increases by addition of a new band subparallel to the previously formed bands. The average thickness of a given zone does not change significantly except for a limited number of places along their lengths and a high thickness/distance gradient at their ends. The high thickness anomalies in the thickness distribution plots along the zones correspond to local complexities such as eye structures, steps, and intersections of converging or diverging bands and may reach to about 35 cm. Microstructural analysis of single compaction bands highlights the presence of two typical portions, a thin portion and a thick portion. The thin portion of the band contains pockets of tightly packed grains surrounded by large pores in the band. The thick portion is characterized by an almost homogeneously distributed compaction throughout the band. The thin portions are found close to the tips, whereas the thick portions occur primarily in the central parts of the bands. Two other characteristics of both single bands and zones of bands in high resolution images are that their thicknesses appear to be smaller and that their lateral boundaries are unexpectedly rough with respect to their appearance in outcrops and hand samples, the latter of which may play an important role in their lateral growth. (C) 2015 Elsevier B.V. All rights reserved.
机译:研究了阿兹台克砂岩中两组高角度压实带的几何,地统计学和微结构,以表征其尺寸,分布和生长动力学。两组通常都在沙丘边界处终止。第一组压实带长于第二组压实带,第二组被认为是由沉积结构控制的。单个压实带的宏观厚度从尖端的零变化到最大值,通常在中心部分为3至10 mm。压实带常常聚集成区域,其厚度通过增加与先前形成的带平行的新带而增加。给定区域的平均厚度不会发生很大变化,除了沿其长度的位置数量有限并且其端部的厚度/距离梯度较高。沿这些区域的厚度分布图中的高厚度异常对应于局部复杂性,例如眼睛结构,台阶和会聚或发散带的交点,并且可能达到约35 cm。单个压实带的微观结构分析突出显示了两个典型部分的存在,即薄部分和厚部分。条带的较薄部分包含由条带中的大孔围绕的紧密堆积的颗粒袋。厚的部分的特征在于在整个带中几乎均匀分布的压紧。发现较薄的部分靠近尖端,而较厚的部分主要出现在带的中央部分。高分辨率图像中单条带和条带区域的两个其他特征是,它们的厚度似乎较小,并且相对于露头和手工样品的外观而言,其横向边界出乎意料地粗糙,后者可能起重要作用在其横向生长中的作用。 (C)2015 Elsevier B.V.保留所有权利。

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