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Exploring Extreme and Unusual Geology in the Stable Midcontinent: Field Excursions for the 2019 GSA South-Central, North-Central, and Rocky Mountain Sections Joint Meeting最新文献

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Trails west and the Civil War in the Kansas City, Missouri/Kansas, region 小径西部和内战在堪萨斯城,密苏里州/堪萨斯地区
J. Aber, S. E. Aber
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引用次数: 0
Windows into the Cretaceous mantle of the North American midcontinent—Kimberlites of Riley County, Kansas 北美中大陆白垩纪地幔的窗口——堪萨斯州莱利县的金伯利岩
P. Kempton, K. Rogers, M. Brueseke
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引用次数: 1
The science and industry of the Permian Hutchinson Salt 二叠纪哈钦森盐业的科学与工业
M. Schulmeister, A. S. Andeskie, K. Benison
The 120-m-thick Hutchinson Salt Member of the Permian Wellington Formation of central Kansas supports multiple industries. Composed of bedded halite, gypsum/anhydrite, and minor siliciclastic mudstone, it was deposited by shallow saline waters in a warm, dry climate. Underground salt mines access the purest horizon, producing salt that is distributed through the United States and Canada. The vast space left by mining supports a prosperous commercial storage enterprise and a popular underground tourist attraction. Vertical solution-mined caverns host the nation’s primary midcontinent liquid petroleum gas storage industry. This fi eld trip will explore the origin and use of the Hutchinson Salt in core samples and subsurface outcrops while meeting in an underground salt cavern, and above ground at a solution-mined storage cavern. Schulmeister, M.K., Andeskie, A.S., and Benison, K.C., 2019, The science and industry of the Permian Hutchinson Salt, in Schulmeister, M.K., and Aber, J.S., eds., Exploring Extreme and Unusual Geology in the Stable Midcontinent: Field Excursions for the 2019 GSA South-Central, North-Central, and Rocky Mountain Sections Joint Meeting: Geological Society of America Field Guide 52, p. 25–35, https://doi.org/10.1130/2019.0052(02). © 2019 The Geological Society of America. All rights reserved. For permission to copy, contact editing@geosociety.org. INTRODUCTION The Hutchinson Salt, underlying an area of ~96,000 km (37,000 mi) mainly in central and south-central Kansas, is considered a saline giant (Walters, 1978; Fig. 1). It attains a thickness of up to 122 m in Kansas and is composed of ~60%–80% halite (Kulstad, 1959; Walters, 1978). Although this bedded halite deposit is one of the Earth’s most famous salt deposits, it has been the subject of limited study. In particular, its depositional environment and the brines’ chemistry have not been clearly established. In addition to its scientifi c relevance, the deposit has a rich and evolving history as an economic resource. This fi eld guide focuses on the Hutchinson Salt in the Hutchinson, Kansas, area. The objectives of this fi eld trip and guide are to provide an overview of the Hutchinson Salt’s industrial uses, as well as to describe the past and current studies about its sedimentology, diagenesis, and depositional environment. The History of Salt Mining in Central Kansas The use of salt marshes and springs by Native Americans and early travelers is reported in central Kansas prior to the arrival of European settlers (Sawin and Buchanan, 2002). Natural salt licks that formed from evaporated shallow pools attracted bison, deer, antelope, and elk. In turn, early hunters would use the salt to preserve meat. In 1875, rock salt was discovered in Hutchinson by local entrepreneurs, who attempted to pump the brine to a regional processing plant, evaporate it, and sell the salt to U.S. markets (Vincent, 1915). The brine was not pure enough to evaporate for use as table salt, however, a
堪萨斯州中部二叠纪惠灵顿地层的120米厚的Hutchinson盐层支撑着多个行业。它由层状盐岩、石膏/硬石膏和少量的硅屑泥岩组成,在温暖干燥的气候下由浅水咸水沉积而成。地下盐矿进入最纯净的地平线,生产的盐分布在美国和加拿大。采矿留下的广阔空间支撑着一个繁荣的商业存储企业和一个受欢迎的地下旅游景点。垂直溶液开采洞穴承载着美国大陆中部主要的液化石油气储存行业。这次实地考察将探索哈钦森盐在岩心样品和地下露头中的起源和用途,同时在地下盐洞和地面上的溶液开采储存洞中相遇。Schulmeister, m.k., Andeskie, a.s.和Benison, k.c., 2019,《二叠纪哈钦森盐的科学和工业》,Schulmeister, m.k.和Aber, j.s.编。,在稳定的中部大陆探索极端和不寻常的地质:2019年GSA中南部,中北部和落基山脉部分联合会议的实地考察:美国地质学会野外指南52,p. 25-35, https://doi.org/10.1130/2019.0052(02)。©2019美国地质学会。版权所有。请联系editing@geosociety.org获取复制权限。哈钦森盐田位于堪萨斯州中部和中南部,面积约96,000公里(37,000英里),被认为是一个巨大的盐田(Walters, 1978;图1)。它在堪萨斯州的厚度可达122米,由~ 60%-80%的盐岩组成(Kulstad, 1959;沃尔特斯,1978)。虽然这个层状盐岩矿床是地球上最著名的盐矿床之一,但它一直是有限的研究对象。特别是其沉积环境和卤水的化学性质尚未明确。除了其科学意义外,该矿床作为一种经济资源有着丰富而不断发展的历史。本野外指南重点介绍堪萨斯州哈钦森地区的哈钦森盐场。这次实地考察和指南的目的是概述哈钦森盐的工业用途,以及描述过去和现在关于其沉积学、成岩作用和沉积环境的研究。据报道,在欧洲定居者到来之前,美国原住民和早期旅行者在堪萨斯中部使用盐沼和盐泉(Sawin and Buchanan, 2002)。由蒸发的浅水池形成的天然盐渍吸引了野牛、鹿、羚羊和麋鹿。反过来,早期的猎人会用盐来保存肉。1875年,当地企业家在哈钦森发现了岩盐,他们试图将盐水泵入地区加工厂,将其蒸发,并将盐出售给美国市场(Vincent, 1915)。然而,卤水不够纯净,不能蒸发成食盐,他们的努力失败了。1887年,一位房地产开发商在他在南哈钦森购买的土地上钻探石油。他的测试井显示出盐而不是碳氢化合物。溶液采矿盐厂立即在里昂、金曼和堪萨斯州的卡诺波利斯发展起来。岩盐的地下开采始于1923年,当时凯里·舒尔迈斯特等人。盐矿(现为哈钦森盐矿)成立。盐矿开采对哈钦森市的历史和经济活力做出了重大贡献。上午的实地考察停留突出了哈钦森盐矿中盐矿的地质起源,以及它的采矿历史和作为地下储存设施和博物馆的额外用途。哈钦森盐的不渗透、不反应性、退火性能和抗压强度与混凝土相似,因此非常适合储存液化石油气(LPG)。在压力下,盐表现出可塑性,导致裂缝或压力自愈。盐岩形成一种不透水的层,不会泄漏或允许外来液体进入。自20世纪50年代以来,用于生产盐水的溶液采矿工艺已被用于在Hutchinson盐段下部创建液化碳氢化合物的储存洞穴。尽管碳氢化合物在美国其他地方也储存在洞穴中,但堪萨斯州的洞穴比其他任何州都多。2013年,堪萨斯州共有9个活跃的液化石油气储存设施,运营着382个活跃的储藏库,总储藏量约为7300万桶(Kansas Department of Health and Environment, 2013)。哈钦森地区巨大的储存能力和中央配送中心使该地区成为全国几个大型液化石油气传输中心之一。
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引用次数: 1
Geology of the Flint Hills, Kansas: Sea-level and climate changes in the Permian 堪萨斯州弗林特山的地质:二叠纪的海平面和气候变化
K. Goldberg, K. Miller
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引用次数: 1
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Exploring Extreme and Unusual Geology in the Stable Midcontinent: Field Excursions for the 2019 GSA South-Central, North-Central, and Rocky Mountain Sections Joint Meeting
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