Evaporite karst of the lower Pecos region最新文献

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Field trip and road log references 实地考察和道路日志参考
Evaporite karst of the lower Pecos region Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.64
Lewis Land, Issam Bou Jaode, Peter Hutchinson, K. Zeigler, Anne C. Jakle, Brittney Van Der Werff
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引用次数: 0
Second-day road log: From Washington Ranch to Rattlesnake Spring and Black River, Carlsbad Spring and Carlsbad Flume, and Gypsum Caves of the Seven Rivers Hills 第二天的道路日志:从华盛顿牧场到响尾蛇泉和黑河,卡尔斯巴德泉和卡尔斯巴德Flume,以及七河山的石膏洞
Evaporite karst of the lower Pecos region Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.41
L. Land
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引用次数: 0
Salt dissolution in the Salado formation (Upper Permian) and land subsidence south of Imperial, Pecos County, West Texas 西德克萨斯州佩科斯县帝国南部萨拉多地层(上二叠纪)的盐溶解和地面沉降
Evaporite karst of the lower Pecos region Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.112
Kenneth Johnson
{"title":"Salt dissolution in the Salado formation (Upper Permian) and land subsidence south of Imperial, Pecos County, West Texas","authors":"Kenneth Johnson","doi":"10.56577/ffc-73.112","DOIUrl":"https://doi.org/10.56577/ffc-73.112","url":null,"abstract":"","PeriodicalId":106599,"journal":{"name":"Evaporite karst of the lower Pecos region","volume":"15 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122396010","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Latest Eocene 40Ar/39Ar Age from the Yeso Hills Dikes, Eddy County, New Mexico 新墨西哥州Eddy县Yeso Hills Dikes地区始新世40Ar/39Ar年龄
Evaporite karst of the lower Pecos region Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.122
Snir Attia, J. Ricci
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引用次数: 0
Critical Mineral Resources in the Cornudas Mountains, Otero County, New Mexico. 新墨西哥州奥特罗县科尼达斯山脉的重要矿产资源。
Evaporite karst of the lower Pecos region Pub Date : 1900-01-01 DOI: 10.56577/ffc-73.132
V. McLemore, N. Iverson, Mason Woodard, Snir Attia, Evan J. Owen
{"title":"Critical Mineral Resources in the Cornudas Mountains, Otero County, New Mexico.","authors":"V. McLemore, N. Iverson, Mason Woodard, Snir Attia, Evan J. Owen","doi":"10.56577/ffc-73.132","DOIUrl":"https://doi.org/10.56577/ffc-73.132","url":null,"abstract":"Reexamination of the mineral resources in the Cornudas Mountains is warranted in light of today’s economic importance of critical minerals that are essential in most of our electronic devices. The Cornudas Mountains form the northern Trans-Pecos alkaline magmatic province in the southern part of the North American Cordilleran alkaline-igneous belt. New mapping, petrography, 40Ar/39Ar geochronology, and geochemical analyses have provided a better understanding of the emplacement of the intrusions and associated mineral deposits in the area. The igneous rocks in the Cornudas Mountains were emplaced into Permian and Cretaceous sedimentary rocks in two pulses at 37.14–34.5 and 32.48–26.95 Ma, just prior to or during the early phases of Rio Grande Rift extension, and consist of (1) larger nepheline syenite–syenite laccoliths and plugs, (2) phonolite plugs, sills, and dikes, (3) smaller syenite plugs and dikes, and (4) volcanic breccia dikes. New U.S. Geological Survey geophysical data indicate that some of the larger intrusions extend into the subsurface as pipelike geometries, with additional buried intrusions potentially at depth that could be additional exploration targets. The focus of exploration for critical minerals in the Cornudas Mountains is for rare earth elements (REE), niobium (Nb), and zirconium (Zr) that are found within (1) the basal unit (PEnsp2) of the Wind Mountain nepheline syenite laccolith, (2) syenite-phonolite and volcanic breccia dikes and plugs, and (3) skarns and carbonate-replacement deposits in Chess Draw and Wind Mountain areas. Some samples contain as much as 3110 ppm total REE. REE could be leached from a mineral concentrate of REE-bearing minerals (eudialyte, zircon, monazite, bastnäsite, calciocatapleiite, vitusite, roumaite, xenotime). Pyrochlore (Nb), eudialyte (Zr), and zircon (Zr) are also found with the REE-bearing minerals and have potential for economic recovery. Another potential mineral resource is nepheline syenite for use as ceramics, glass, or other industrial use. 132 New Mexico Geological Society Guidebook, 73rd Fall Field Conference, 2023, p. 132–141, https://doi.org/10.56577/FFC-73.132","PeriodicalId":106599,"journal":{"name":"Evaporite karst of the lower Pecos region","volume":"36 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"116820427","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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