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Panola Granite

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Map of Panola Mountain Research Watershed. Panola granite (gray area, GR) intrudes amphibolite-biotite gneiss (black dashed line, ABG), based on data provided by Williams (2006). The black rectangle denotes an area on the map, which is compared to the images from the scattered surface waves (see Figure 12). The map is adopted from Hooper (2001).
Published: 01 December 2007
Figure 1 Map of Panola Mountain Research Watershed. Panola granite (gray area, GR) intrudes amphibolite-biotite gneiss (black dashed line, ABG), based on data provided by Williams (2006). The black rectangle denotes an area on the map, which is compared to the images from the scattered surface
Journal Article
Published: 01 December 2007
Journal of Environmental and Engineering Geophysics (2007) 12 (4): 337–351.
...Figure 1 Map of Panola Mountain Research Watershed. Panola granite (gray area, GR) intrudes amphibolite-biotite gneiss (black dashed line, ABG), based on data provided by Williams (2006). The black rectangle denotes an area on the map, which is compared to the images from the scattered surface...
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Image
Pore water Mg concentrations reflecting biotite weathering in saprolite profiles in Rio Icacos and solid state Mg concentration reflecting biotite weathering in saprolite profiles at Panola, GA. The solute concentration co refers to average rainfall at Rio Icacos and the solid Mg concentrations Co to the unweathered Panola granite. The diagonal lines represent linear regressions through the data with the slopes corresponding to the solute and solid weathering gradients (see Eqns. 11 and 12).
Published: 01 January 2009
concentrations C o to the unweathered Panola granite. The diagonal lines represent linear regressions through the data with the slopes corresponding to the solute and solid weathering gradients (see Eqns. 11 and 12).
Image
a) Three-dimensional image of scatterers, generated for average semblance coefficient of 0.09 and above. The solid black line denotes the location of the creek and the dark gray circle denotes the center of the geophone array; b) a map view of the 3D image (a). The boundaries of the outcropping granite are superimposed as dotted black lines, and the contact between Panola granite and amphibolite-biotite gneiss (following Figure 1) is presented with a dashed black line.
Published: 01 December 2007
of the outcropping granite are superimposed as dotted black lines, and the contact between Panola granite and amphibolite-biotite gneiss (following Figure 1 ) is presented with a dashed black line.
Image
(a) Geologic map of northeast Georgia and surrounding states (after Dallmeyer et al., 1981) showing the regional setting of the Elberton granite. Other granite bodies of similar age are shown in black; BH = Ben Hill granite, PG = Panola granite. (b) Larger-scale map of the Elberton granite [after Ellwood (1980) and Jurdy and Phinney (1983)] showing the main body of the granite and outliers believed to be continuous at depth. Solid line with dots is COCORP line 1, with vibrator station numbers for reference. Dotted lines are raypaths for shots recorded for the present study; stars are the blast locations, and heavy bars are the seismic array locations. The blasts recorded for raypath D are just off the map, at a distance of roughly 23 km from the center of the array.
Published: 12 October 2005
Figure 1. (a) Geologic map of northeast Georgia and surrounding states (after Dallmeyer et al., 1981 ) showing the regional setting of the Elberton granite. Other granite bodies of similar age are shown in black; BH = Ben Hill granite, PG = Panola granite. (b) Larger-scale map of the Elberton
Image
Plot of mass transfer coefficient (τ) versus depth for weathering profiles for plagioclase and trace amounts of disseminated calcite developed on the Panola Granite, Georgia (after White et al. 2001). The close correspondence between these two completely developed reaction fronts is consistent with both reactions being limited by transport rather than kinetics, i.e., regions I and II in Figure 5. The calcite may be a profile-controlling mineral in this system (see text).
Published: 01 January 2009
Figure 7. Plot of mass transfer coefficient (τ) versus depth for weathering profiles for plagioclase and trace amounts of disseminated calcite developed on the Panola Granite, Georgia (after White et al. 2001 ). The close correspondence between these two completely developed reaction fronts
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Completely developed profiles for the three steady-state regolith case studies: A) τNa plotted versus depth for one core into the Rio Blanco quartz diorite, Luquillo Experimental Forest, Puerto Rico (Buss et al. 2008); B) Na (albite) concentration versus depth for Panola GA (White et al. 2001); C) Na (albite) concentration versus depth for Davis Run, VA (White et al. 2001). The reaction front thickness for Na decreases from Davis Run granite (~10 m) to Panola granite (~6 m) to Puerto Rico quartz diorite (~40 cm) as the ratio of transport to dissolution rate decreases. A first-order control on this ratio is the physical state of the weathering material: at Davis Run, weathering of Na-feldspar is occurring in saprolite where advective transport dominates, while Na release from Panola occurs within the reacting low-porosity bedrock where diffusion dominates. In Puerto Rico, fracturing due to spheroidal weathering has been observed to create onionskin-like rindlets around weathering bedrock, accelerating the transport of reactants into the weathering bedrock (Fletcher et al. 2006). Curve fits to the data are also shown for the sigmoidal (B, D, Eqn. 30) and exponential models (C, E, Eqn. 35). The loss of Na in the Rio Blanco quartz diorite occurs in the 30–40 cm thick rindlet zone that defines the reaction front for Na plagioclase at the bedrock-saprolite transition. In Panola, the bedrock-saprolite transition lies just deeper than 5 m. For Davis Run, the bedrock-saprolite transition is more than a meter wide and lies below 20 m.
Published: 01 January 2009
( White et al. 2001 ); C) Na (albite) concentration versus depth for Davis Run, VA ( White et al. 2001 ). The reaction front thickness for Na decreases from Davis Run granite (~10 m) to Panola granite (~6 m) to Puerto Rico quartz diorite (~40 cm) as the ratio of transport to dissolution rate decreases
Journal Article
Published: 01 January 2009
Reviews in Mineralogy and Geochemistry (2009) 70 (1): 435–484.
... concentrations C o to the unweathered Panola granite. The diagonal lines represent linear regressions through the data with the slopes corresponding to the solute and solid weathering gradients (see Eqns. 11 and 12). ...
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(A) Scanning electron microscope image of weathered granite, sampled 7.5 m below the surface at Panola, Georgia, USA. It shows altered plagioclase with pristine K-feldspar and biotite. (B and C) Soil water (crosses) and groundwater (circles) are far from saturation (dotted line) for albite, but groundwater is saturated with respect to K-feldspar (fromWhite 2005).
Published: 01 October 2007
FIGURE 4 ( A ) Scanning electron microscope image of weathered granite, sampled 7.5 m below the surface at Panola, Georgia, USA. It shows altered plagioclase with pristine K-feldspar and biotite. ( B and C ) Soil water (crosses) and groundwater (circles) are far from saturation (dotted line
Journal Article
Journal: Clay Minerals
Published: 01 December 2007
Clay Minerals (2007) 42 (4): 415–435.
... the structure is compressed (saprolite). Using mass-balance calculations for the Panola granite profile, White et al . (2001) showed that weathering proceeded through four successive alteration stages. From stage 1 to stage 4, the progress of the weathering reactions is controlled by a continuous...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1979
AAPG Bulletin (1979) 63 (11): 2103–2104.
.... Their genetic relation to the little-known late Paleozoic or early Mesozoic granites of Grenada and Yalobusha Counties, Mississippi, and to the microgranite sills(?) of Tallahatchie County, Mississippi, is unknown (see Denison and Muehlberger, 1963 ; also, Riggs, 1976 ). Subsequent to the Moody...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 May 2005
GSA Bulletin (2005) 117 (5-6): 783–794.
...., Solute Modelling in Catchment Systems : New York , John Wiley & Sons , Inc., p. 193 – 209 . White , A.F. , Blum , A.E. , Schulz , M.S. , Huntington , T.G. , Peters , N.E. , and Stonestrom , D.A. , 2002 , Chemical weathering of the Panola Granite: Solute and regolith...
FIGURES
Journal Article
Published: 01 November 2002
American Mineralogist (2002) 87 (11-12): 1616–1625.
... rate of mass loss in the surrounding Piedmont. This evaluation can only be determined by knowing the duration of weathering and the mass loss. The nearest estimate of Piedmont exposure ages comes from a study of the Panola granite ( Schroeder et al. 2001 ). Based on measurement of the 10 Be and 26 Al...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1920
AAPG Bulletin (1920) 4 (2): 117–136.
... developments have found acid igneous rock evidently of pre-Cambrian age in Ranch Creek Oil Company, Masterson No. 1, in Potter county. Granite has also been found in a test in New Mexico west of Amarillo. Evidently buried hills prolong the topography of the Wichita Mountains far westward and extend...
FIGURES
Journal Article
Journal: Geology
Published: 01 February 2014
Geology (2014) 42 (2): 171–174.
...%, and 9.0%, respectively). In the case of Ca-feldspar to kaolinite (R5), an important weathering reaction affecting granitic and basaltic rocks, chemical denudation is clearly overstimated by TDS sil (Φ = 49.9%). The reaction of chlorite to kaolinite (R6), typical of sedimentary rock weathering...
FIGURES
Journal Article
Journal: Geophysics
Published: 12 October 2005
Geophysics (2005) 70 (6): B67–B72.
...Figure 1. (a) Geologic map of northeast Georgia and surrounding states (after Dallmeyer et al., 1981 ) showing the regional setting of the Elberton granite. Other granite bodies of similar age are shown in black; BH = Ben Hill granite, PG = Panola granite. (b) Larger-scale map of the Elberton...
FIGURES | View All (7)
Journal Article
Journal: Elements
Published: 01 October 2007
Elements (2007) 3 (5): 315–319.
...FIGURE 4 ( A ) Scanning electron microscope image of weathered granite, sampled 7.5 m below the surface at Panola, Georgia, USA. It shows altered plagioclase with pristine K-feldspar and biotite. ( B and C ) Soil water (crosses) and groundwater (circles) are far from saturation (dotted line...
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Journal Article
Journal: Geology
Published: 01 February 2009
Geology (2009) 37 (2): 151–154.
.... Stonestrom D.A. 2002 , Chemical weathering of the Panola Granite: Solute and regolith elemental fluxes and the weathering rate of biotite, in Hellman R. Wood S.A. eds...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1949
AAPG Bulletin (1949) 33 (7): 1206–1250.
... the limestones of the Smackover have been penetrated by drilling in Bowie, Panola, Shelby, Red River, Morris, Titus, Franklin, Wood, Hunt, Kaufman, Smith, Freestone, Limestone, and Robertson counties. The stratigraphy of the Smackover in The Texas Company’s Adams No. C-1, Panola County, and the Humble Oil...
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Journal Article
Published: 01 July 2016
The Journal of Geology (2016) 124 (4): 501–517.
... 32 33 0  Panola 2 .71–.5 .75 92 4 4 0 0  Panola 2 .5–.25 1.5 63 22 13 2 0 Tuscaloosa Gravel, Tennessee:  Tuscaloosa, TN 19 2.0–4.0 −1.5 0 2 98 0 0  Tuscaloosa, TN 19 1.0–2.0 −.5 0 0 100 0 0  Tuscaloosa, TN 19 .5–1.0 .5 1 0 99...
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