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• W2001079105 abstract "Research Article| January 01, 1999 Structural Domains and Their Potential Impact on Recharge to Intermontane-Basin Aquifers GREGORY C. OHLMACHER GREGORY C. OHLMACHER Kansas Geological Survey, University of Kansas, 1930 Constant Avenue, Lawrence, KS 66047-3726 Search for other works by this author on: GSW Google Scholar Author and Article Information GREGORY C. OHLMACHER Kansas Geological Survey, University of Kansas, 1930 Constant Avenue, Lawrence, KS 66047-3726 Publisher: Association of Environmental & Engineering Geologists First Online: 02 Mar 2017 Online Issn: 1558-9161 Print Issn: 1078-7275 © Association of Engineering Geologists 1999 Environmental & Engineering Geoscience (1999) V (1): 61–71. https://doi.org/10.2113/gseegeosci.V.1.61 Article history First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation GREGORY C. OHLMACHER; Structural Domains and Their Potential Impact on Recharge to Intermontane-Basin Aquifers. Environmental & Engineering Geoscience 1999;; V (1): 61–71. doi: https://doi.org/10.2113/gseegeosci.V.1.61 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyEnvironmental & Engineering Geoscience Search Advanced Search Abstract Variations in the structures exposed in structural domains associated with faults can affect the amount of ground-water recharge to fractured rock aquifers supplying intermontane-basin aquifers. In the southwestern Franklin Mountains, El Paso, Texas, an outcrop of the Ordovician Scenic Drive Formation exposes a group of structures including faults, joints, and folds associated with a left-lateral fault striking N74°E and dipping 81°NW. Slip along this fault has produced a structural domain with extensional structures (normal faults and joints) and a domain with contractional structures (folds and joints). These extensional and contractional domains occur on opposite sides of the fault.Properties of fractures within the different structural domains can influence ground-water recharge and migration. For example, the domain with extensional structures contains nearly vertical joints that extend from the soil-bedrock interface to normal faults and along which precipitation can infiltrate. Since the left-lateral fault is approximately normal to the trend of the Franklin Mountains, this fault may be a conduit for ground-water flow from the mountains to the basin. The domain with contractional structures is limited in extent, and the fractures in this domain are poorly connected. Therefore, surface infiltration in this domain is reduced, and may not contribute as much to ground-water migration. Structural domains that are analogous to this outcrop and cover larger areas can be found throughout the Franklin Mountains. Understanding the variations between structural domains can aid in siting water-supply wells and determining contaminant transport in fractured rock. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2001079105 title "Structural Domains and Their Potential Impact on Recharge to Intermontane-Basin Aquifers" @default.
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