Relevant bibliographies by topics / Geology – Georgia – Clay County

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Academic literature on the topic 'Geology – Georgia – Clay County'

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

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Journal articles on the topic "Geology – Georgia – Clay County"

1

Cook, Robert B. "Lazulite Graves Mountain, Lincoln County, Georgia." Rocks & Minerals 83, no. 4 (July 2008): 328–33. http://dx.doi.org/10.3200/rmin.83.4.328-333.

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Gordon, Jennings B. "A Gahnite Occurrence in Carroll County, Georgia." Rocks & Minerals 63, no. 6 (November 1988): 471–72. http://dx.doi.org/10.1080/00357529.1988.11761885.

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Cook, Robert B. "Connoisseur's Choice: Rutile, Graves Mountain, Lincoln County, Georgia." Rocks & Minerals 78, no. 2 (April 2003): 112–16. http://dx.doi.org/10.1080/00357529.2003.9926704.

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Barwood, Henry, and Robert B. Cook. "The Hogg Estate or Mineral Processing Mine, LaGrange, Troup County, Georgia." Rocks & Minerals 81, no. 3 (January 2006): 180–86. http://dx.doi.org/10.3200/rmin.81.3.180-186.

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Santamaria, Jose, and Jeff Deere. "Through the 'Scope: Baryte Microcrystals from the Cartersville Mining District, Bartow County, Georgia." Rocks & Minerals 96, no. 3 (April 26, 2021): 270–76. http://dx.doi.org/10.1080/00357529.2021.1875753.

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Wight, Georgina Deweese, and Henri D. Grissino-Mayer. "Dendrochronological Dating of an Antebellum Period House, Forsyth County, Georgia, U.S.A." Tree-Ring Research 60, no. 2 (December 2004): 91–99. http://dx.doi.org/10.3959/1536-1098-60.2.91.

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Geffner, Paul. "The Treasure Chest Pockets: An Update on the Jacksons Crossroads Amethyst Mine Wilkes County, Georgia." Rocks & Minerals 83, no. 6 (November 2008): 550–52. http://dx.doi.org/10.3200/rmin.83.6.550-552.

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Turgut, Bülent, and Merve Ateş. "Factors of soil diversity in the Batumi delta (Georgia)." Solid Earth 8, no. 1 (January 3, 2017): 1–12. http://dx.doi.org/10.5194/se-8-1-2017.

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Abstract. The aim of this study was to determine certain basic properties of soils in the Batumi delta (southwestern Georgia) to determine the relationships of studied properties and to identify differences with regards to these properties between different sampling sites in the delta that were selected based on the delta morphology. In this context, a total of 125 soil samples were collected from five different sampling sites, and the clay, silt and sand content of the samples were determined along with their mean weight diameter (MWD) values, aggregate stability (AS) values, amount of water retained under −33 (FC) and −1500 kPa (WP) pressure and organic matter (OM) content. Correlation analysis indicated that clay content and OM were positively correlated with MWD, and OM was positively correlated with AS. However, the sand content was found to be negatively correlated with MWD. In addition, clay, silt and OM content were positive correlated with FC and WP. Variance analysis results determined statistically significant differences between the sampling sites with respect to all of the evaluated properties. The active delta section of the study area was characterized by high sand content, while the lower delta plain was characterized by high OM and AS values, and the upper delta plain was characterized by high MWD values, high FC and WP moisture content levels and high clay and silt content. In conclusion, it was demonstrated that the examined properties were significantly affected by the different morphological positions and usages of these different areas. These results may help with the management of agricultural lands in the Batumi delta, which has never been studied before.
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Hower, James C., Dali Qian, Nicolas J. Briot, Madison M. Hood, and Cortland F. Eble. "Mineralogy of a rare earth element-rich Manchester coal lithotype, Clay County, Kentucky." International Journal of Coal Geology 220 (March 2020): 103413. http://dx.doi.org/10.1016/j.coal.2020.103413.

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Li, Xiao, Timothy Grey, William Vencill, James Freeman, Katilyn Price, George Cutts, and Andrew Price. "Evaluation of Cotton Responses to Fomesafen-Based Treatments Applied Preemergence." Weed Technology 32, no. 4 (May 3, 2018): 431–38. http://dx.doi.org/10.1017/wet.2018.31.

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AbstractFomesafen provides effective control of glyphosate-resistant Palmer amaranth in cotton. However, cotton seedlings can be injured when fomesafen is applied PRE. Therefore, greenhouse and field experiments were conducted at Athens, GA, and at six locations in Alabama and Georgia in 2013 and 2016 to evaluate cotton growth and yield response to fomesafen applied PRE at 70, 140, 280, 560, 1,120, or 2,240 g ai ha−1, and in combination with pendimethalin, diuron, acetochlor, and fluridone at 1×label rates. Greenhouse bioassays indicated that fomesafen reduced cotton height and dry weight with increasing rate in Cecil sandy loam and Tifton loamy sand but not in Greenville sandy clay loam––possibly as a result of this soil’s higher organic matter (OM) and clay content. Fomesafen applied at 2,240 g ai ha−1 reduced cotton stand by as much as 83% compared to the nontreated check (NTC) at all field locations except Alabama’s Macon and Baldwin counties, and 1,120 g ai ha−1 reduced cotton stand only at Pulaski County, GA, by 52%. Cotton height was reduced by the two highest rates of fomesafen at all locations except Clarke County, GA, and Baldwin County, AL. Injury data indicated more visual injury followed increasing fomesafen rates, and high-rate treatments produced more injury in sandier soils. Cotton yield was unaffected by herbicide treatments at any location, except for the 1,120 g ai ha−1 rate at Pulaski County (49% yield loss compared to NTC), 2,240 g ai ha−1 at Pulaski County (72% yield loss), and Tift County (29% yield loss). These data indicated cotton yield should not be negatively affected by fomesafen applied PRE alone within label rates or in combination with pendimethalin, diuron, acetochlor, and fluridone at 1×label rates, although some visual injury, or stand or height reduction may occur early in the growing season.
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Dissertations / Theses on the topic "Geology – Georgia – Clay County"

1

Degnan, Keith Terence. "Organic-walled microplankton paleoecology and biostratigraphy of the Upper Cretaceous Ripley Formation, southwestern Georgia." Thesis, Virginia Polytechnic Institute and State University, 1987. http://hdl.handle.net/10919/101342.

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This study documents the occurrence of dinoflagellate, chlorophyte, and acritarch cysts from the Upper Cretaceous upper Cusseta, Ripley, and lower Providence Formations in the USGS Fort Gaines core, drilled in Clay County, Georgia. A total of 75 taxa were identified, consisting of 36 genera, 61 species, and 5 subspecies of dinoflagellates, 3 genera and 4 species of chlorophytes, 3 genera and 4 species of acritarchs, and 1 problematical protozoan. 15 of these taxa are unpublished. The study's cyst assemblage was statistically analyzed to ascertain paleoecologic patterns. The results from cluster analysis and detrended correspondence analysis indicate the presence of four cyst associations. The Deflandrea pannucea association is interpreted as indicative of low salinity related to nearby river discharge. The Deflandrea sp. A association is confined to the inner shelf. The Exochosphaeridium bifidum and Glaphyrocysta reticulosa associations alternate under normal marine conditions. The associations correlate well with observed lithologies and lithologic change. Comparison of this study's assemblage with other Late Cretaceous assemblages provides limited information, since many biostratigraphically-important species are not present in this study. However, comparisons with Wilson's (1974), Benson's (1976), and Firth's (1984) zonations suggest a Lower Maastrichtian age for all strata in this study.
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Alkhammali, Sultan A. "Geochemical and clay mineralogical characteristics of the Woodford Shale, Payne County, Oklahoma." Thesis, Kansas State University, 2015. http://hdl.handle.net/2097/19166.

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Master of Science
Geology
Sambhudas Chaudhuri
Chemical and mineralogical compositions of < 2 µm-size fraction clays of the shale source rocks of Devonian-Mississippian age in northern Oklahoma were determined to find any link between the minerals and the generation of petroleum. Ten samples of clay separates were analyzed for their mineral composition, major element contents, K/Rb ratios, and REE contents. XRD analyses and SEM showed the presence of discrete illite, the most dominant clay mineral, with smaller amounts of mixed-layer illite/smectite, chlorite, and kaolinite. The non-clay minerals found in the Woodford Shale from this study include quartz, dolomite, calcite, pyrite, feldspar (albite and microcline), and apatite. The clays in these rocks have a range of K/Rb ratios between 160 and 207. These ratios are considerably lower than the ratios of average silicate minerals (clays), with expected ratios between 250 and 350. It could be that clays received K and Rb from a solution, which was partly involved in oil generation by which oil received more K relative to Rb making the aqueous phase depleted in K/Rb ratios (Alvarez, 2015). Thus, the low K/Rb ratios for these clays may be reflecting signatures of reactions involving oil generation. The total REE contents ranged between 13 and 30 ppm. The low total REE contents of < 2 µm-size fraction clays in the Woodford Shale as compared to average sedimentary rocks which may be represented by values given either PAAS 184 ppm or NASC with 178 ppm, may suggest that the formation of the clays was linked to oil generation, having known of the face from the study of Alvarez (2015) that crude oils could have higher specific REE concentrations than the associated formation waters. PAAS-normalized REE patterns for these samples display positive Gd anomalies. Two out of the ten samples had prominent Ce anomalies. Only three out of ten samples had Eu positive anomalies, one of which was quite prominent. All samples had MREE enrichment, superimposed on either a flat REE distribution patterns with enrichment in LREE. Only one pattern showed the distribution with a distinct HREE enrichment. The MREE anomalies could be from the effect of phosphate mineralization. In fact, the X-ray diffraction patterns of random powder samples showed the presence of fluorapatite and chlorapatite in most of the studied samples. The total organic carbon (TOC) contents of the whole rocks ranged from 0.5 to 6.54 wt.%. Thus, it can be concluded that hydrocarbon generation potential of the Woodford shale (0.8-4.44 wt.%) is significantly higher than Mississippian Lime unit (0.5 wt.%). Only one sample, which belonged to pre-Woodford Shale Hunton group, had the highest value of TOC. The available K-Ar dates of < 2 µm-size fraction clays suggest that the clays are authigenic (illites) for at least some samples. The dates ranged from 318.6 ± 7.9 Ma (Serpukhovian) to 353.9 ± 7.9 Ma (Tournaisian). All dates are younger than the times of deposition of the Woodford Shale. Assuming there is a genetic link between formation of authigenic illite and hydrocarbon generation, this study suggests that oil generation may have taken place on an average about 30 Ma after the deposition of the Woodford Shale.
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Ayorinde, Adebayo O. "MINERALOGY AND GEOCHEMISTRY OF THE BAUXITE DEPOSITS (CRETACEOUS), WILKINSON COUNTY, GEORGIA." Digital Archive @ GSU, 2011. http://digitalarchive.gsu.edu/geosciences_theses/30.

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Cretaceous bauxite deposits from Hall and Veneer mines, Wilkinson County, Georgia are composed of kaolinite, gibbsite, goethite, anatase, nordstrandite and bohemite. Quartz and micas are absent in the samples. The presence of boehmite and goethite are evidence of intense weathering forming the bauxite deposits. The extremely high values of the Chemical Index of Alteration (CIA) which is over 99, and the low values of the alkali metals and alkali earth metals, support an intense weathering origin for the bauxite deposit. There is evidence of deposition in the mines based on the presence of pisoids in the bauxite samples and the composition of the parent materials, which vary markedly by the non-uniform TiO2/Al2O3 values which represent the accumulation of transported materials from contrasting source areas. Kaolin minerals were first produced by the hydrolytic weathering of aluminous sediments and then gibbsite was formed as early kaolin was desilicated.
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4

Bradford, Matt. "Mapping clay alteration across the northern Goldstrike property using spectroscopy and remote sensing, Eureka County, Nevada." Bowling Green, Ohio : Bowling Green State University, 2008. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=bgsu1216923357.

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Anderson, John R. II. "The Effects of High Density Septic Systems on Surface Water Quality in Gwinnett County, Georgia." Digital Archive @ GSU, 2010. http://digitalarchive.gsu.edu/geosciences_theses/28.

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Gwinnett County, Georgia experienced rapid growth in the 1970’s without the infrastructure so septic systems were installed for residential homes. The number of septic systems grew to over 85,000 with a density of 487 septic systems per square mile. This study mapped the distribution of septic systems to determine regions of potential pathogen surface water. This study addressed what potential health risks do high density septic systems have on surface water quality and how can the history of Gwinnett County assist in future development in the Metropolitan Atlanta area? It was found that the density of septic systems has reduced the surface water quality for streams in the Yellow and Alcovy River basins. An average rainfall cause septic flushing and an increase in the fecal coliform. Other trends observed in the surface water quality of increased BOD, water temperature, and various metals also indicated this flushing effect.
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Thornberry, Trista L. "The Petrography of the Buck Creek Dunite Body, Clay County, NC : Implications about its Origin and Emplacement." Oberlin College Honors Theses / OhioLINK, 1998. http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1411990381.

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Neurath, Robert Carl. "Comparative Baseflow Hydrochemistry of Various Septic System Density Groups within the Yellow River Watershed, Gwinnett County, Georgia." Digital Archive @ GSU, 2007. http://digitalarchive.gsu.edu/geosciences_theses/9.

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Baseflow water chemistry between different septic system density groups was analyzed to understand how septic system usage impacts the water quality of the Yellow River Watershed located in Gwinnett County, Georgia. Seventy water samples were collected at baseflow conditions in the summer of 2006. The samples were analyzed for the abundance and distribution of chlorides, sulfates, nitrates, and specific conductance. Geographic Information Systems were used to determine sample collection sites, assign samples into density groups, and spatially analyze and display the results. Statistical methods were used to compare the results of each density group with all others,and to find any correlation of the anions with respect to specific conductance. Regression coefficient values between nitrate and specific conductance in all groups average 0.77 and the elevated nitrate concentrations in group four suggest a limited relationship between septic system density and baseflow water quality.
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8

Bradford, Matthew S. "Mapping Clay Alteration Across the Northern Goldstrike Property Using Spectroscopy and Remote Sensing, Eureka County, Nevada." Bowling Green State University / OhioLINK, 2008. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1216923357.

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Nostrom, Rachel. "Portable X-ray Fluorescence Analysis of Pottery at the Bayshore Homes Site in Pinellas County, Florida." Scholar Commons, 2014. https://scholarcommons.usf.edu/etd/5285.

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The Bayshore Homes site was occupied intermittently over a period of approximately twelve hundred years, with the two main occupation periods being CE 150-550 and CE 900-1350. During those lengthy occupations a substantial amount of plain and decorated pottery was discarded at the site. A portable X-ray fluorescence (pXRF) spectrometer was utilized to analyze the elemental composition of 133 sherds, both decorated and plain. The resulting elemental composition data were then analyzed using multivariate statistics in an attempt to discern discrete clay sources that may have been exploited by inhabitants of the Bayshore Homes site. Principal component analysis (PCA) and discriminant function analysis (DA) were employed to identify three discrete clay sources exploited in the production of pottery. The results of the statistical analyses were then used to answer two basic, yet pertinent, questions about the Bayshore pottery: 1) Were the same clay sources exploited during both occupation periods? 2) Were the same clay sources exploited for both decorated and plain pottery? The results of the statistical analyses indicate that the same clay sources were exploited for both occupation periods, though evidence suggests that the dominant clay source in use did change over time. The results also imply that the same clay sources were utilized in the production of plain and decorated pottery, which suggests that at least some portion of the decorated pottery excavated from the Bayshore site was produced locally, and not obtained through trade. Finally, the results of this research demonstrate that pXRF is a useful tool for preliminary differentiation of clay sources in Florida.
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Magdic, Matthew James. "Assessment of Soil Properties in Proximity to Abandoned Oil Wells usingRemote Sensing and Clay X-ray Analysis, Wood County, Ohio." Bowling Green State University / OhioLINK, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1462537679.

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Books on the topic "Geology – Georgia – Clay County"

1

O'Connor, Bruce J. Ceramic and structural clays and shales of Floyd County, Georgia. Atlanta, Ga: Georgia Dept. of Natural Resources, Environmental Protection Division, Georgia Geologic Survey, 1986.

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O'Connor, Bruce J. Ceramic and structural clays, and shales of Walker County, Georgia. Atlanta, Ga: Georgia Dept. of Natural Resources, Environmental Protection Division, Georgia Geologic Survey, 1988.

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O'Connor, Bruce J. Ceramic and structural clays and shales of Whitfield County, Georgia. Atlanta, Ga: Georgia Dept. of Natural Resources, Environmental Protection Division, Georgia Geologic Survey, 1988.

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O'Connor, Bruce J. Ceramic and structural clays, shales, and slates of Murray County, Georgia. Atlanta, Ga: Georgia Dept. of Natural Resources, Environmental Protection Division, Georgia Geologic Survey, 1986.

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O'Connor, Bruce J. Ceramic and structural clays, shales and slates of Gordon County, Georgia. Atlanta, Ga: Georgia Dept. of Natural Resources, Environmental Protection Division, Georgia Geologic Survey, 1987.

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O'Connor, Bruce J. Ceramic and structural clays, shales and slates of Polk County, Georgia. Atlanta, Ga: Georgia Geologic Survey, 1988.

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Pollastro, Richard M. Composition, clay mineralogy ,and diagenesis of the Simpson Group (Middle Ordovician), Grady County, Oklahoma. [Washington]: U.S. G.P.O., 1991.

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Xu, Jianzhong. The Cypress Sandstone (Mississippian) reservoir and its recovery potential at Xenia East Oil Field, Clay County, Illinois. Champaign, Ill: Illinois State Geological Survey, 1995.

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Strom, Eric W. Location and depth of sand and clay intervals in Jackson County, Mississippi. Pearl, Miss: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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Swiggart, Carolyn Clay. Shades of gray: The Clay and McAllister families of Bryan County, Georgia during the plantation years (ca. 1760-1888). Darien, CT: Two Bytes Pub., 1999.

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Reports on the topic "Geology – Georgia – Clay County"

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Geology, geochemistry and mineral resource assessment of the Rand Mountain Roadless Area, Rabun County, Georgia. US Geological Survey, 1987. http://dx.doi.org/10.3133/mf1983.

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Chapter I: Geology of a Middle Tertiary Clay Deposit in thePatagonia Mountains near Harshaw, Santa Cruz County, Southeastern Arizona. US Geological Survey, 2005. http://dx.doi.org/10.3133/b2209i.

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Geology, geochemistry, and mineral resource assessment of the southern Nantahala Wilderness and adjacent roadless areas, Rabun and Towns counties, Georgia, and Clay and Macon counties, North Carolina. US Geological Survey, 1991. http://dx.doi.org/10.3133/b1883.

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