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Evaporite karst of the lower Pecos region最新文献

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Pre-conference field trip three: Carlsbad Cavern from Washington Ranch to Whites City, Walnut Canyon, scenic view of Delaware Basin, and Carlsbad Caverns 会前实地考察三:卡尔斯巴德洞穴从华盛顿牧场到白城,核桃峡谷,特拉华盆地的风景,和卡尔斯巴德洞穴
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.15
Issam Bou Jaode
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引用次数: 0
First-Day road log: From Washington Ranch to State Line Castile Gypsum Roadcut, Rader Debris Flow, Brushy Canyon Submarine Channel Sand, Salt Basin, Capitan Reef Overlook, Chosa Draw Evaporite Karst Features, and Parks Ranch Cave 第一天的道路日志:从华盛顿牧场到州线卡斯提尔石膏路堑,雷德泥石流,灌木峡谷海底通道砂,盐盆地,Capitan礁俯瞰,Chosa Draw蒸发岩喀斯特特征,和公园牧场洞穴
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.27
L. Land
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引用次数: 0
The ancestral Rocky Mountain orogeny and evolution of the Permian Basin 祖先落基山的造山运动与二叠纪盆地的演化
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.68
K. Rudolph
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引用次数: 0
Sulfuric acid speleogenesis at the new section level of Carlsbad Cavern roughly 6 Ma 约6 Ma卡尔斯巴德溶洞新剖面水平的硫酸造洞作用
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.76
V. Polyak, P. Provencio, Bill Mcintosh
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引用次数: 0
Pre-conference field trip two: Cornudas Mountains 会前实地考察之二:科努达斯山脉
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.7
Evan J. Owen, Virginia L. McLemore
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引用次数: 1
Quaternary Age Of The Gatu�a Formation at Livingston Ridge 利文斯顿岭加图亚组的第四纪时代
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.103
Snir Attia, M. Heizler, J. Ricci
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引用次数: 0
The Guadalupian series and the Permian timescale 瓜达鲁普系和二叠纪的时间尺度
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.82
S. Lucas
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引用次数: 0
A north-flowing precursor to the Pecos River in the Gatu�a formation of southeastern New Mexico and Texas 佩科斯河:新墨西哥州东南部和德克萨斯州加图河构造中佩科斯河向北流动的前体
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.89
S. Cather, M. Heizler
Axial-fluvial deposits in the Gatuña Formation of southeastern New Mexico have been recognized for decades. Contrary to existing models, 725 paleocurrent measurements presented here indicate this axial river flowed north, with mean values for individual localities ranging from northwest to north-northeast. Axial sediments were deposited by a regional braided paleoriver within evolving solution-subsidence basins near the modern, south-flowing Pecos River. These dissolution features preserved Gatuña deposits from paleo-landscape positions possibly hundreds of meters above the modern Pecos Valley. Most of the fluvial sedimentary fill within major solution-subsidence features is likely Miocene–Pleistocene, whereas the thin alluvial and eolian Gatuña on the margins of the modern Pecos Valley may be largely Pleistocene. Northward paleoflow (and its subsequent reversal) in southeastern New Mexico resulted largely from epeirogenic warping of the Llano Estacado region since the Oligocene. 90
新墨西哥州东南部Gatuña组的轴向河流沉积已经被发现了几十年。与现有模型相反,本文提供的725个古水流测量结果表明,这条轴向河流向北流动,其平均值从西北到东北偏北不等。轴向沉积物由区域性辫状古河流沉积于现代南流佩科斯河附近不断演化的溶蚀沉降盆地内。这些溶解特征保存了Gatuña沉积物,这些沉积物来自古地貌位置,可能比现在的佩科斯山谷高数百米。主要溶蚀沉降特征内的河流沉积填充物大部分可能是中新世-更新世,而现代佩科斯谷边缘的薄冲积和风成Gatuña可能主要是更新世。新墨西哥州东南部向北的古流动(及其随后的逆转)主要是由渐新世以来Llano Estacado地区的造陆翘曲造成的
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引用次数: 0
Pre-conference field trip one: Guadalupe Peak Trail, Guadalupe Mountains National Park 会前实地考察一:瓜达卢佩峰步道,瓜达卢佩山国家公园
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.2
L. Land
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引用次数: 0
Third-Day Road Log: From Washington Ranch to the Seven Rivers Embayment and Bottomless Lakes State Park 第三天的道路日志:从华盛顿牧场到七河海湾和无底湖州立公园
Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.53
L. Land
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引用次数: 0
期刊
Evaporite karst of the lower Pecos region
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