Relevant bibliographies by topics / Geology – Texas – Bexar County

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Geology – Texas – Bexar County'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Geology – Texas – Bexar County"

1

Golab, James A., Jon J. Smith, Allan K. Clark, and Charles D. Blome. "Effects of Thalassinoides ichnofabrics on the petrophysical properties of the Lower Cretaceous Lower Glen Rose Limestone, Middle Trinity Aquifer, Northern Bexar County, Texas." Sedimentary Geology 351 (April 2017): 1–10. http://dx.doi.org/10.1016/j.sedgeo.2017.02.001.

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Lukowski, Paul D. "Archaeological Investigations at 41BX1, Bexar County, Texas." Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State 1987, no. 1 (1988): Article 5. http://dx.doi.org/10.21112/ita.1988.1.5.

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Young, Wayne C. "Archaeological Testing of Site 41BX679 Bexar County, Texas." Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State 1985, no. 1 (1985): Article 22. http://dx.doi.org/10.21112/ita.1985.1.22.

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Figueroa, Antonia. "Archaeological Survey of the Paloma Subdivision, Bexar County, Texas." Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State 2009, no. 1 (2009): Article 4. http://dx.doi.org/10.21112/ita.2009.1.4.

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McGraw, A. Joachim. "Archaeological Investigations at Eisenhower Park, Northern Bexar County, Texas." Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State 1986, no. 1 (1986): Article 2. http://dx.doi.org/10.21112/ita.1986.1.2.

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Turner, David D. "Excavations at San Juan Capistrano, 41BX5, Bexar County, Texas." Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State 1987, no. 1 (1988): Article 1. http://dx.doi.org/10.21112/ita.1988.1.1.

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Boyd, T. "Assessing immunization registry data completeness in Bexar County, Texas." American Journal of Preventive Medicine 22, no. 3 (2002): 184–87. http://dx.doi.org/10.1016/s0749-3797(01)00427-5.

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Snavely, Ralph. "An Archaeological Survey of Converse City Park, Bexar County, Texas." Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State 1986, no. 1 (1986): Article 1. http://dx.doi.org/10.21112/ita.1986.1.1.

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Tennis, Cynthia L., and Robert J. Hard. "Archaeological Survey of Upper Leon Creek Terraces, Bexar County, Texas." Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State 1995, no. 1 (1995): Article 5. http://dx.doi.org/10.21112/ita.1995.1.5.

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Nickels, David L., David W. Pease, and C. Britt Bousman. "Archaeological Survey of Lackland Air Force Base, Bexar County, Texas." Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State 1997, no. 1 (1997): Article 16. http://dx.doi.org/10.21112/ita.1997.1.16.

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Dissertations / Theses on the topic "Geology – Texas – Bexar County"

1

Veni, George. "Effects of Urbanization on the Quantity and Quality of Storm Water Runoff Recharging Through Caves into the Edwards Aquifer, Bexar County, Texas." TopSCHOLAR®, 1985. http://digitalcommons.wku.edu/theses/1842.

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Eighty-nine caves and sinkholes were investigated in the Edwards Aquifer recharge zone in Bexar County, Texas. The study examined their hydrogeologic and topographic origins and distribution, relationships to major fracture traces, quantity of recharge into the aquifer and degree of sensitivity towards degradation of the aquifer’s water quality. Groundwater traces were attempted to determine aquifer flow routes, time of groundwater travel, groundwater volume within conduits, and the aquifer’s capacity for dilution and dispersion of recharged contaminants. Trends in water quality were examined to quantify the volume and variety of contaminants recharged into the aquifer and to determine the effects of urbanization upon the Edwards Aquifer. The Edwards recharge zone was hydrogeologically assessed to rate the sensitivity of its areas. Socio-political impacts on recharge zone development were also examined. Based on the results of the above outlined research method, the conclusions of this investigation are that caves and sinkholes contribute substantial recharge into the Edwards Aquifer, rapidly transmit that recharge to the aquifer and are sensitive sites for potential contamination. The entire recharge zone was determined to be very sensitive to contamination. No significant differences were found between areas within the recharge zone to scale their degree of sensitivity. Major conduit flow networks were found to exist within the aquifer and their groundwater flow paths could be traced. Urban development of the Edwards recharge zone was shown to decrease the volume of recharge and degrade the aquifer’s water quality. No significant detrimental effects on the aquifer were observed. The volume of diminished recharge and the concentration of recharged contaminants that were necessary to produce significant adverse effects on the aquifer were not determined due to lack of precipitation during the study period and inconclusive groundwater tracings. It was recommended that further development of the recharge zone be suspended until the effects of urbanization are quantified.
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Dada, Olamide. "Reservoir Characterization of the Spraberry Formation, Borden County, West Texas." Thesis, University of Louisiana at Lafayette, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1557545.

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<p> The Spraberry Formation is a Leonardian age submarine fan deposit restricted to the Midland Basin. The formation consists of very fine-grained sandstone, medium to coarse grain size siltstones, organic shales and carbonate mudstones. These rocks show variability in sedimentary structures and bedding types varied from thinly laminated to convolute laminations. Bioturbations were present in some samples and soft sediment deformation, such as water escape features, sediment loading and flame structures. </p><p> The Spraberry Formation is a naturally fractured reservoir with low porosity and low matrix permeability. Porosity measured varied from 2% in rocks with poor reservoir quality such as the argillaceous siltstone and mudstone while good reservoir rocks had an average porosity of 9%. Seven lithofacies were identified based on sedimentary structures, grain size and rock fabrics. Petrographic analysis showed four porosity types: (1) intragraular porosity; (2) dissolution porosity; (3) fracture porosity and (4) intergranular porosity. Fractured porosity was only observed in the argillaceous siltstone lithofacies. </p><p> The prominent diagenetic influences on the Spraberry Formation are: quartz cementation, quartz overgrowth, illtization of smectite, feldspar dissolution, clay precipitation, carbonate cementation, formation of framboidal pyrite and fracture formation. These diagenetic features were observed using scanning electron microscope (SEM) and in thin sections. Generally, petrophysical properties, such as porosity and permeability, vary gradually from reservoir rocks to non-reservoir rock. Observed trends where: 1) increasing organic and argillaceous content with decreasing porosity and 2) increasing carbonate sediments and calcite cements with decreasing porosity. Mineralogical analysis from FTIR showed an abundance of quartz and calcite, while illite is the prominent clay mineral observed in all samples.</p>
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Mason, James Bryan. "Analysis of site structure and post-depositional disturbance at two Early Holocene components, Richard Beene site (41BX831), Bexar County, Texas." Thesis, Texas A&M University, 2003. http://hdl.handle.net/1969/584.

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Edds, Donald Dean. "Structural geology of Black Butte area, Northwest Eagle Mountains, Hudspeth County, Texas." Kansas State University, 1987. http://hdl.handle.net/2097/18556.

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Lomago, Brendan Michael. "Subsurface Framework and Fault Timing in the Missourian Granite Wash Interval, Stiles Ranch and Mills Ranch Fields, Wheeler County, Texas." Thesis, Mississippi State University, 2019. http://pqdtopen.proquest.com/#viewpdf?dispub=10979211.

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<p> The recent and rapid growth of horizontal drilling in the Anadarko basin necessitates newer studies to characterize reservoir and source rock quality in the region. Most oil production in the basin comes from the Granite Wash reservoirs, which are composed of stacked tight sandstones and conglomerates that range from Virgillian (305&ndash;299 Ma) to Atokan (311&ndash;309.4 Ma) in age. By utilizing geophysical well logging data available in raster format, the Granite Wash reservoirs and their respective marine flooding surfaces were stratigraphically mapped across the regional fault systems. Additionally, well log trends were calibrated with coincident core data to minimize uncertainty regarding facies variability and lateral continuity of these intervals. In this thesis, inferred lithofacies were grouped into medium submarine fan lobe, distal fan lobe, and offshore facies (the interpreted depositional environments). By creating isopach and net sand maps in Petra, faulting in the Missourian was determined to have occurred syndepositionally at the fifth order scale of stratigraphic hierarchy.</p><p>
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Arteaga, Veronica Hernandez. "The relationship between vertical teaming in science and student achievement as reported in the academic excellence indicator system (AEIS) at selected public schools in Bexar County, Texas." Texas A&M University, 2008. http://hdl.handle.net/1969.1/86019.

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The purpose of this study was to examine the relationship between vertical teaming in science and student achievement. This study compared student achievement of campuses implementing vertical teaming with schools that do not practice vertical teaming. In addition, this study explored the relationship between selected demographic variables and vertical teaming using Grade 5 Science TAKS results in the Academic Excellence Indicator System (AEIS). Campus demographic variables such as economically disadvantaged, minority students, English language learners, student mobility, and experienced teachers were researched. A call-out yielded 168 responses. With the exclusion of the 12 campuses, a total of 156 participating campuses from 18 traditional school districts remained. Campuses employing vertical teaming were self-identified on the basis of having implemented the process for two or more years. The gain in percent mastered for Science TAKS scores from 2004 to 2007 was used as the Science TAKS score variable. Results indicated that there was no significant difference in student achievement in science for campuses practicing vertical teaming and campuses that did not. The twoway ANOVA was used to measure the relationship between the independent variables (vertical teaming and campus demographic variables) on the dependent variable (student achievement on Science TAKS). The results suggested that campuses having low percentages of economically disadvantaged students statistically gained more on the Science TAKS than campuses that have high percentages of economically disadvantaged students irrespective of vertical teaming practices. In addition, campuses that have low percentages of minority students statistically gained more on the Science TAKS than campuses that have high percentages of minority students despite vertical teaming participation. Recommendations include districts, state, and federal agencies providing campuses with a high percent of economically disadvantaged students with more resources and more flexibility in using those resources. Recommendations for further study included a replication of the study that takes into account the degree of implementation of vertical teaming.
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Triyana, Yanyan. "Characterization of Rodessa Formation Reservoir (Lower Cretaceous) in Van Field, Van Zandt County, Texas." Texas A&M University, 2003. http://hdl.handle.net/1969/62.

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Boudreaux, Elisabeth L. "A Lithologic and Petrologic Reanalysis of a Lithic-Rich Tuff Within the Sierra Quemada Structure, Big Bend National Park, Brewster County, Texas." Thesis, University of Louisiana at Lafayette, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1553887.

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<p>The origin of the Mule Ear Spring Tuff (Tmet) member of the Chisos Formation of the Big Bend Group in Big Bend National Park (BBNP) (Maxwell et al., 1967) and its relationship to Sierra Quemada (SQ) is debated (a caldera versus a ring dike complex without associated collapse), as well as how the exact age of the Tmet relates to volcanic material present in and around the SQ structure. The main objectives were to identify main types of clasts present within the lithic-rich tuff and to determine the relative age of the lithic-rich tuff within SQ in order to help identify the type of structure and the type of activity&mdash;caldera with collapse or simply a ring dike. </p><p> Detailed lithologic and petrologic descriptions of hand samples and thin sections were performed to determine relationships of the clasts within the lithic-rich tuff to units outside of SQ. The identification and comparison of the samples produced a relative age of approximately 30.3 Ma to 33.7 Ma for the activity within SQ, which is comparable to published ages of Tmet. </p><p> Measurements of the clasts, along with the apparent thickness of the lithic-rich tuff, were compared with studies done on lithic-rich accumulations within modern and ancient calderas. The concentration and sizes of the clasts within the lithic-rich tuff from SQ are comparable to, or larger than, calderas with similar diameters to the SQ structure. The results are compatible with the formation of a typical resurgent caldera. The lack of lithic fragments younger than Tmet within the tuff is compatible with the age of Tmet. Therefore, the age of activity and formation of SQ occurred approximately 34 Ma. </p>
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Maxey, George F. "Geology as a Georegional Influence on Quercus Fagaceae Distribution in Denton and Coke Counties of Central and North Central Texas and Choctaw County of Southeastern Oklahoma, Using GIS as an Analytical Tool." Thesis, University of North Texas, 2007. https://digital.library.unt.edu/ark:/67531/metadc5144/.

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This study elucidates the underlying relationships for the distribution of oak landcover on bedrock and soil orders in two counties in Texas and one in Oklahoma. ESRI's ArcGis and ArcMap was used to create surface maps for Denton and Coke Counties, Texas and Choctaw County, Oklahoma. Attribute tables generated in GIS were exported into a spreadsheet software program and frequency tables were created for every formation and soil order in the tri-county research area. The results were both a visual and numeric distribution of oaks in the transition area between the eastern hardwood forests and the Great Plains. Oak distributions are changing on this transition area of the South Central Plains. The sandy Woodbine and Antlers formations traditionally associated with the largest oak distribution are carrying oak coverage of approximately 31-32% in Choctaw and Denton Counties. The calcareous Blackland and Grand Prairies are traditionally associated with treeless grasslands, but are now carrying oak and other tree landcover up to 18.9%. Human intervention, including the establishment of artificial, political and social boundaries, urbanization, farming and fire control have altered the natural distribution of oaks and other landcover of this unique georegion.
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Ryu, Changsu. "Sequence stratigraphic controls of hydrocarbon reservoir architecture case study of Late Permian (Guadalupian) Queen Formation, Means Field, Andrews County, Texas /." Texas A&M University, 2002. http://hdl.handle.net/1969/530.

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Books on the topic "Geology – Texas – Bexar County"

1

Weston, Jason D. Archaeological survey and geoarchaeological investigations at 41BX1271, Walker Ranch Park, Bexar County, Texas. Center for Archaeological Research, The University of Texas at San Antonio, 2003.

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Clark, Allan K. Geologic framework and hydrogeologic features of the Glen Rose Limestone, Camp Bullis training site, Bexar County, Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 2003.

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Loftus, Carrie. Bexar County, Texas, selected cemeteries (early burials). F.T. Ingmire, 1985.

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Alley, Jacobina. Bexar County, Texas voter registration, 1865 & 1867-1869. San Antonio Genealogical & Historical Society, 2006.

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Figueroa, Antonia. Archaeological investigations and construction monitoring at the Bexar County Justice Center Expansion Project, San Antonio, Bexar County, Texas. Center for Archaeological Research, University of Texas at San Antonio, 2011.

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Nickels, David L. Archaeological survey of Lackland Air Force Base, Bexar County, Texas. Center for Archaeological Research, The University of Texas at San Antonio, 1997.

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Clark, Amy R. Vulnerability of ground water to contamination, northern Bexar County, Texas. U.S. Dept. of the Interior, U.S. Geological Survey, 2003.

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Tennis, Cynthia L. Archaeological survey of upper Leon Creek terraces, Bexar County, Texas. Center for Archaeological Research, The University of Texas at San Antonio, 1995.

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Nickels, David L. Test excavations at the Culebra Creek site, 41BX126, Bexar County, Texas. Center for Archaeological Research, University of Texas at San Antonio, 1998.

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Figueroa, Antonia. Archaeological survey of the proposed Medina River Park, Bexar County, Texas. Center for Archaeological Research, University of Texas at San Antonio, 2004.

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Book chapters on the topic "Geology – Texas – Bexar County"

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Martinez, Matthew J. "School District Formation as an Explanation for Spatial and Temporal Dimensions of Concentrated Poverty in Bexar County, Texas." In The Springer Series on Demographic Methods and Population Analysis. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-26492-5_14.

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Winzinger, R., J. L. Brink, K. S. Patel, C. B. Davenport, Y. R. Patel, and G. C. Thakur. "Design of a Major CO2 Flood—North Ward Estes Field, Ward County, Texas." In The Integration of Geology, Geophysics, Petrophysics and Petroleum Engineering in Reservoir Delineation, Description and Management. American Association of Petroleum Geologists, 1991. http://dx.doi.org/10.1306/sp535c35.

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Conference papers on the topic "Geology – Texas – Bexar County"

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Poling, Katrina M., Harshad Vijay Kulkarni, Keisuke Ikehata, and Saugata Datta. "BRACKISH GROUNDWATER IN BEXAR COUNTY TEXAS: SUITABILITY FOR REVERSE OSMOSIS (RO) DESALINATION." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358000.

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Steuer, A., M. Deszcz-Pan, and B. D. Smith. "Resolution of Hydrostratigraphic Parameters from Inversions of HEM Measurements, Northern Bexar County, Texas." In Near Surface 2007 - 13th EAGE European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609.20146685.

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D. Shah, Sachin, Jason D. Payne, Bruce D. Smith, and Allan K. Clark. "An Integrated Geophysical And Hydrogeological Investigation Of The Cibolo Canyon Development Area, Northeastern Bexar County, Texas." In 21st EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609-pdb.177.96.

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D. Payne, Jason, Bruce D. Smith, and Allan K. Clark. "Hydrogeophysical Surveys Of The Trinity And Edwards Aquifers At Camp Bullis, Northern Bexar County, Texas, 2006." In 23rd EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609-pdb.175.sageep055.

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Payne, Jason D., Bruce D. Smith, and Allan K. Clark. "Hydrogeophysical Surveys of the Trinity and Edwards Aquifers at Camp Bullis, Northern Bexar County, Texas, 2006." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2010. Environment and Engineering Geophysical Society, 2010. http://dx.doi.org/10.4133/1.3445471.

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Shah, Sachin D., Jason D. Payne, Bruce D. Smith, and Allan K. Clark. "An Integrated Geophysical and Hydrogeological Investigation of the Cibolo Canyon Development Area, Northeastern Bexar County, Texas." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2008. Environment and Engineering Geophysical Society, 2008. http://dx.doi.org/10.4133/1.2963332.

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Smith, David V., Bruce Smith, Maria Deszcz-Pan, Marcus Gary, and Allan Clark. "REPROCESSING AND INTERPRETATION OF HELICOPTER ELECTROMAGNETIC DATA OVER THE EDWARDS AND TRINITY AQUIFER INTERFACE IN NORTHERN BEXAR COUNTY, TEXAS." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2013. Environment and Engineering Geophysical Society, 2013. http://dx.doi.org/10.4133/sageep2013-214.1.

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Golab, James A., and Jon J. Smith. "EFFECTS OF BIOGENIC POROSITY ON THE PETROPHYSICAL PROPERTIES OF THE KARSTIC LOWER CRETACEOUS GLEN ROSE LIMESTONE, BEXAR COUNTY, TEXAS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283302.

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Cooper, John R., Alexis Godet, Jeremy A. Kelley, Jeffrey W. Hardwick, and Jorge Spangenberg. "THE IMPACT OF TECTONIC AND ENVIRONMENTAL CHANGES ON DEPOSITIONAL GEOMETRIES OF THE AUSTIN CHALK GROUP IN BEXAR COUNTY, TEXAS." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289205.

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Schoen, Robert, and Chris A. Barker. "GEOLOGY OF THE ALTO RELEX AREA, SIERRA DEL CARMEN, BIG BEND NATIONAL PARK, BREWSTER COUNTY, TEXAS." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289558.

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Reports on the topic "Geology – Texas – Bexar County"

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Geologic framework and hydrogeologic characteristics of the Edwards Aquifer recharge zone, Bexar County, Texas. US Geological Survey, 1995. http://dx.doi.org/10.3133/wri954030.

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Geologic framework and hydrogeologic features of the Glen Rose Limestone, Camp Bullis Training Site, Bexar County, Texas. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034081.

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Vulnerability of ground water to contamination, northern Bexar County, Texas. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034072.

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Vulnerability of ground water to contamination, Edwards Aquifer recharge zone, Bexar County, Texas, 1998. US Geological Survey, 2000. http://dx.doi.org/10.3133/wri004149.

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Simulation of streamflow and estimation of streamflow constituent loads in the San Antonio River watershed, Bexar County, Texas, 1997-2001. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034030.

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Simulation of runoff and recharge and estimation of constituent loads in runoff, Edwards aquifer recharge zone (outcrop) and catchment area, Bexar County, Texas, 1997-2000. US Geological Survey, 2002. http://dx.doi.org/10.3133/wri024241.

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