Evaporite karst features and processes at Nash Draw, Eddy County, New Mexico

D. W. Powers, R. Beauheim, R. Holt, D. Hughes
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引用次数: 4

Abstract

—Nash Draw, about 30 km east of Carlsbad, NM, is a karst valley developed on Upper Permian evaporite rocks of the Rustler and Salado Formations. Early studies found sodium chloride brine along the draw axis above halite of the Salado Formation, with the brine flowing toward and into the Pecos River. The draw was interpreted as the consequence of erosion, solution, and fill. Later studies report solution of sulfate units of the Rustler, yielding more complicated surficial structures. More drillhole logs are now available, showing that the eastern margin of Nash Draw (Livingston Ridge) overlies the position where the elevation of upper Salado halite changes, as deos the thickness across the upper Salado and the elevation of overlying units. These elevation changes reflect dissolution of Salado halite. Depressions along Livingston Ridge result from subsidence that has caused recent regrading of arroyos. At Laguna Grande de la Sal, elevations of the top of Salado halite indicate a depression under the lake, and lower halite south of the lake is associated with elongate valley-like depressions as well as rounded basins. The movement of brine at depth may be directed along this surface. Surface karst features in the southeastern arm of Nash Draw develop on and within sulfate beds of the Rustler Formation and surficial gypsite. Collapse sinks and coalescing collapse in small karst valleys appear to show some evolutionary trends based on period since erosion exposed sulfate beds. Vertical-walled collapse sinks without fill are young, while karst valleys are older. These features are developed along stratigraphic trends. Some of the recharge in this sulfate-dominated environment discharges year-round in local springs, indicating fluid storage within the system. Alluvium in sinks and karst valleys are proposed as part of the storage system. FIGURE 1. General location map of Nash Draw with identified features. Numbers refer to brine lakes informally named Laguna Uno (1) through Cinco (5). The Waste Isolation Pilot Plant (WIPP) site outline does not include the entire WIPP area. The area shown in Figure 3 is outlined here. 254 POWERS, BEAUHEIM, HOLT, AND HUGHES
新墨西哥州埃迪县纳什图的蒸发岩岩溶特征和过程
纳什图位于新罕布什尔州卡尔斯巴德以东约30公里处,是一个喀斯特山谷,发育在Rustler和Salado地层的上二叠世蒸发岩上。早期的研究发现,氯化钠卤水沿着萨拉多地层盐岩上方的拉轴,流向佩科斯河。这一现象被解释为侵蚀、溶解和填充的结果。后来的研究报告了Rustler的硫酸盐单位溶液,产生了更复杂的表面结构。更多的钻孔测井资料显示,Nash Draw (Livingston Ridge)的东部边缘覆盖了Salado上部岩盐岩海拔变化的位置,以及Salado上部岩盐岩的厚度和上覆单元的海拔变化。这些海拔变化反映了萨拉多岩盐的溶解作用。利文斯顿山脊沿线的洼地是由最近造成阿罗约斯退坡的沉降造成的。在拉古纳格兰德萨尔湖,萨拉多岩盐岩顶部的高度表明湖下有一个凹陷,而湖南部的下部岩盐岩则与细长的山谷状凹陷以及圆形盆地有关。盐水在深部的运动可能沿着这个表面进行。纳什拉东南支的地表岩溶特征发育在拉斯特勒组的硫酸盐层和表面石膏层上和内部。小喀斯特山谷塌陷汇和聚结塌陷在侵蚀暴露硫酸盐层的时间上表现出一定的演化趋势。无填充物的垂壁塌陷汇较年轻,而岩溶谷较老。这些特征是沿地层走向发育的。在这个以硫酸盐为主的环境中,一些补给在当地的泉水中全年排放,表明系统内存在流体储存。汇和喀斯特山谷的冲积层被认为是蓄水系统的一部分。图1所示。纳什绘制的大致位置地图,带有已识别的特征。数字指的是非正式命名为Laguna Uno(1)至Cinco(5)的盐水湖。废物隔离试验工厂(WIPP)的场地大纲不包括整个WIPP区域。图3中显示的区域在这里进行了概述。254名鲍尔,博海姆,霍尔特和休斯
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