Relevant bibliographies by topics / North Carolina Granite Corporation

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Academic literature on the topic 'North Carolina Granite Corporation'

Author: Grafiati
Published: 4 June 2021
Last updated: 9 February 2022

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Journal articles on the topic "North Carolina Granite Corporation"

1

Delson, Martin, M. L. Chan, George C. Ferrell, and Brian Flattery. "A Statewide Load Control System at North Carolina Electric Membership Corporation." IEEE Power Engineering Review PER-5, no. 6 (June 1985): 29. http://dx.doi.org/10.1109/mper.1985.5526621.

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Delson, Martin, M. l. Chan, George Ferrell, and Brian Flattery. "A Statewide Load Control System at North Carolina Electric Membership Corporation." IEEE Transactions on Power Apparatus and Systems PAS-104, no. 6 (June 1985): 1270–75. http://dx.doi.org/10.1109/tpas.1985.319239.

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Levine, Steven P., Charles F. Redinger, and William P. Robert. "Community Exposure Assessment and Intervention Effectiveness at Trinity American Corporation, Glenola, North Carolina." AIHAJ 62, no. 5 (September 2001): 649–57. http://dx.doi.org/10.1202/0002-8894(2001)062<0649:ceaaie>2.0.co;2.

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Levine, Steven P., Charles F. Redinger, and William P. Robert. "Community Exposure Assessment and Intervention Effectiveness at Trinity American Corporation, Glenola, North Carolina." AIHAJ - American Industrial Hygiene Association 62, no. 5 (September 2001): 649–57. http://dx.doi.org/10.1080/15298660108984665.

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Everitt, Deborah T., and JoAnn M. Burkholder. "Seasonal dynamics of macrophyte communities from a stream flowing over granite flatrock in North Carolina, USA." Hydrobiologia 222, no. 3 (September 1991): 159–72. http://dx.doi.org/10.1007/bf00016155.

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Shedlock, Kaye M. "Seismicity in South Carolina." Seismological Research Letters 59, no. 4 (October 1, 1988): 165–71. http://dx.doi.org/10.1785/gssrl.59.4.165.

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Abstract The largest historical earthquake in South Carolina, and in the southeastern US, occurred in the Coastal Plain province, probably northwest of Charleston, in 1886. Locations for aftershocks associated with this earthquake, estimated using intensities based on newspaper accounts, defined a northwest trending zone about 250 km long that was at least 100 km wide in the Coastal Plain but widened to a northeast trending zone in the Piedmont. The subsequent historical and instrumentally recorded seismicity in South Carolina images the 1886 aftershock zone. Except for a few scattered earthquakes and a swarm of shallow (≤ 4 km deep), small (ML ≤ 2.5), primarily reverse faulting earthquakes that occurred along the flanks of a granite pluton about 60 km northwest of Columbia, the seismicity in the Piedmont province has been associated with water level changes in reservoirs. Reservoir induced seismicity (RIS) is shallow (≤ 6 km deep), primarily strike-slip or thrust faulting corresponding to an inferred maximum horizontal compressive stress oriented approximately N 60° E. Instrumentally recorded seismicity in the Coastal Plain province occurs in 3 seismic zones or clusters: Middleton Place-Summerville (MPSSZ), Adams Run (ARC), and Bowman (BSZ). Approximately 68% of the Coastal Plain earthquakes occur in the MPSSZ, a north trending zone about 22 km long and 12 km wide, lying about 20 km northwest of Charleston. The hypocenters of MPSSZ earthquakes range in depth from near the surface to almost 12 km. Thrust, strike-slip, and some normal faulting are indicated by the fault plane solutions for Coastal Plain earthquakes. The maximum horizontal compressive stress, inferred from the P-axes of the fault plane solutions, is oriented NE-SW in the shallow crust (< 9 km deep) but appears to be diffusely E-W between 9 to 12 km deep. Although there is localized variability, the current seismicity and associated faulting in South Carolina probably represent a regional response to the NE-SW maximum horizontal compressive stress prevalent throughout eastern North America.
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Corley-Lay, Judith B. "Friction and Surface Texture Characterization of 14 Pavement Test Sections in Greenville, North Carolina." Transportation Research Record: Journal of the Transportation Research Board 1639, no. 1 (January 1998): 155–61. http://dx.doi.org/10.3141/1639-17.

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Three locked-wheel skid trailers, International Cybernetics Corporation (ICC) Model MOR 5041 and K. J. Law Models M 1270 and M 1290, were tested at three speeds on 14 test sections located in Greenville, North Carolina. The test sections included a heavy-duty surface course, polymer-modified heavy-duty surface course, rubber-modified heavy-duty surface course, heavy-duty surface course with carbon black, stone mastic with fibers, polymer-modified stone mastic, and large-stone surface course. Multivariate regression analysis of friction number versus speed for the three test vehicles was performed. Despite having been load cell calibrated 1 day before testing, the ICC MOR 5041 results were statistically different from those of the other skid trailers on all but one test section. The two K. J. Law skid trailers were statistically different from each other, either on intercept or slope, on more than half of the test sections. Each individual skid trailer provided repeatable results with a standard deviation of about 2 when testing was done at 64 km/h, with a higher standard deviation for testing at lower speed. The frictional resistance of the test sections was compared by ranking frictional number at 64 km/h and rate of decline of friction number with speed. The best frictional performance was provided by the heavy-duty surface course and the large-stone surface course, and stone mastic with fibers and stone mastic with polymer were ranked poorest. None of the test sections had an average friction number less than 40, even when tested at 80 km/h.
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Carozzi, Albert, and Marguerite Carozzi. "Franz Joseph Märter, Travel Companion of Johann David Schöpf in a Journey From Philadelphia to Florida and the Bahamas in 1783-1784." Earth Sciences History 13, no. 1 (January 1, 1994): 5–20. http://dx.doi.org/10.17704/eshi.13.1.60757v173568t071.

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Two years before Johann David Schöpf (1752-1800) published his Beyträge … (1787), Franz Joseph Märter (1753-1827) sent letters from Pennsylvania, Virginia, South Carolina, and East-Florida to Ignaz von Born, describing plants, animals, and geological features of the newly independent states. These letters were speedily printed in Physikalische Arbeiten … in Vienna (1785). A last letter sent from the Bahamas appeared in the same periodical in 1786. Märter's geological observations are translated and analyzed here for the first time. His descriptions of various rocks along the Schuylkill River, upstream from Philadelphia (granites, limestones, marble quarries, widespread weathered iron ores), and his interpretation of the fossiliferous sandstones in the Appalachian mountains are very similar to those by Schöpf. So are Märter's observations of shell banks, either exposed in ditches many miles from the sea, or in cliffs at Yorktown, Virginia, and Wilmington, North Carolina, as well as his description of granite and of a large coal mine near Richmond, Virginia. Finally, both travelers noticed that the rocky cliffs in the Bahamas consisted of limestone formed by Muschelsand [beachrock]. We established that Märter and Schöpf traveled together from Philadelphia to the Bahamas (November 1783 to March 1784). But neither acknowledged the influence, or at least the presence of the other, probably for political reasons.
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Dana, Kamal, Nima Nezafati, and Mansuor Vossoughi Abedini. "Study of involved fluids and geochemistry of rare earth elements of Aghbolagh copper deposit, in North Oshnavieh, West Azerbaijan Province of Iran." Earth Sciences Research Journal 24, no. 2 (April 1, 2020): 231–43. http://dx.doi.org/10.15446/esrj.v24n2.83340.

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Aghbolagh copper deposit is located in the southwest of West Azarbaijan Province, 10 km north of Oshnavieh city. Most of the existing rock outcrops in the area include Cambrian deposits (carbonated and clastic deposits). These deposits are metamorphosed by intrusive-granite masses (skarn-genesis). The infiltration of the mineralization solution at distances beyond contact and inside the sandstone sequences has resulted in the formation of copper ore veins. For microscopic and geochemical studies, 21 thin sections, and 22 doubly-polished cross-sections, 22 XRD specimens, 22 ICP-MS specimens, and three samples for analysis of 10 oxides were analyzed by Zarazma Corporation. In the study of the fluids involved, measurements were made using a Linkham THMSG600 heater and freezer plate, mounted on a polarized microscope with a separate stage and Olympus model. Studies on quartz minerals (3 samples) and garnet minerals (2 samples) were performed on five polished double sections by micro-thermometry measurements on 30 inclusion in quartz mineral and 15 inclusion in garnet mineral at Rizkavan Land Company. The results show that the La/Y ratio, which is a proper indicator for the pH conditions of the formation environment of ore deposit, in Aghbolagh deposit is a range from 0.09 to 2.26. The granite mass has the highest amount, and the skarn zone represents two types of conditions. Type 1: Section where the La/Y> 1 ratio observed in samples close to the skarn mass and ore. Type 2: Part where the ratio La/Y <1 is close to marble lithology. In the case of a vein deposit, the samples have mineralization under alkaline conditions, and other samples show acidic conditions. The examination of fluid inclusions determined two main groups of fluids in this mineralization system. Group 1: Supersaturated fluids of salt, which is the origin of halite multiphase inclusions in the garnet ore during the progressive skarn alteration process. Group 2: Salt-saturated fluids, which are the source of fluid-rich two-phase intermediates in the garnet and quartz minerals, and have been effective in regressive alteration in the skarn system.
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Calles-Escandón, Jorge, Jaimie C. Hunter, Sarah E. Langdon, Eva M. Gómez, Vanessa T. Duren-Winfield, and Kristy F. Woods. "La Clínica del Pueblo: A Model of Collaboration Between a Private Media Broadcasting Corporation and an Academic Medical Center for Health Education for North Carolina Latinos." Journal of Immigrant and Minority Health 11, no. 6 (January 21, 2009): 513–19. http://dx.doi.org/10.1007/s10903-008-9223-6.

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Dissertations / Theses on the topic "North Carolina Granite Corporation"

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Hund, Erik A. "U-Pb dating of granites from the Charlotte belt of the southern Appalachians." Thesis, Virginia Tech, 1987. http://hdl.handle.net/10919/45758.

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New U-Pb zircon ages from plutons in the Charlotte belt of the southern Appalachians have provided evidence of Cambro-Ordovician and Siluro-Devonian magmatic activity. Several U-Pb zircon ages of Cambro-Ordovician plutons predate their Rb-Sr whole rock ages by as much as 60 m.y., suggesting a post emplacement disturbance of the Rb-Sr isotopic systems. Comparison of geologic setting, chemistry, and temporal and spatial distribution of Charlotte belt Siluro-Devonian plutons with those of other tectonic environments, specifically plutons from tensional environments, suggests a model for strike-slip accretion.
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Witanachchi, Channa Devinda. "Isovolumetric weathering of granite in Wake County, North Carolina." 2004. http://www.lib.ncsu.edu/theses/available/etd-04152004-161512/unrestricted/etd.pdf.

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Powell, Elizabeth Erin. "An analysis of project management methodology as applied to demand forecasting software implementation within a leading apparel corporation." 2004. http://www.lib.ncsu.edu/theses/available/etd-04152004-163137/unrestricted/etd.pdf.

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Byars, Heather E. "Tectonic evolution of the west-central portion of the Newton window, North Carolina Inner Piedmont timing and implications for the emplacement of the Paleozoic Vale charnockite, Walker Top Granite, and mafic complexes /." 2010. http://trace.tennessee.edu/utk_gradthes/607.

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Byars, Heather Elizabeth. "Tectonic evolution of the west-central portion of the Newton window, North Carolina Inner Piedmont: Timing and implications for the emplacement of the Paleozoic Vale charnockite, Walker Top Granite, and mafic complexes." 2010. http://trace.tennessee.edu/utk_gradthes/607.

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Detailed geologic mapping of portions of the Banoak, Reepsville, Lincolnton West, and Cherryville 7.5-minute quadrangles has confirmed the easternmost exposure of the Brindle Creek fault, which frames the Newton window. The Brindle Creek fault is a terrane boundary that separates the overlying Siluro-Devonian assemblage of metasedimentary rocks and Devonian-Mississippian anatectic plutons of the Cat Square terrane from the Neoproterozoic(?)-Ordovician metasedimentary and igneous rocks of the Tugaloo terrane. Structures related to six deformational events have been identified in this portion of the Inner Piedmont. The Brindle Creek fault has been folded multiple times, resulting in a sinuous outcrop pattern and the formation of the Newton window and smaller Howards Creek window. Portions of three map-scale sheath folds have been identified by map patterns and orientation of dominant mineral lineations, fold axes, and shear-sense indicators. The discontinuity of map-scale bodies of metagraywacke, mafic complexes, and amphibolite is attributed to extension during sheath fold formation. Dominant foliation, mineral lineation, and fold-axis orientations suggest north-northwest directed flow occurred in this portion of the Inner Piedmont. Zircon geochronology data indicate crystallization of the Vale charnockite at 366.4 ± 3.1 Ma and the enclosing Walker Top Granite at 356.5 ± 5.3 Ma. Zircon saturation thermometry estimates minimum magmatic temperatures for the granitoids at 800-840⁰ C. Whole-rock geochemical and isotopic data indicate the Vale charnockite and Walker Top Granite are genetically related and were derived from deep crustal melting of largely Proterozoic-affinity metasediments in an arc environment. Both granitoids crystallized from the same parent magma; the Vale charnockite is an autolith, or early crystallization of the melt, incorporated into the later crystallizing Walker Top Granite. Geochemical analyses of Cat Square terrane mafic complexes west of the Newton window suggest these bodies represent vestiges of oceanic crust formed in a back-arc basin setting or from both MORB and volcanic-arc sources as characterized by mixed N-MORB and calc-alkaline volcanic-arc signatures. This back-arc basin likely formed from east-dipping subduction during the development of Ordovician volcanic arcs outboard of Laurentia.
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Books on the topic "North Carolina Granite Corporation"

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Once and forever: The story of Mount Airy Granite. Ararat, VA: Laurel Hill Pub., 2011.

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Robinson, Russell M. Robinson on North Carolina corporation law. 7th ed. Newark, NJ: LexisNexis, 2002.

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Robinson, Russell M. Robinson on North Carolina corporation law. Charlottesville, Va: Michie Co., 1990.

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Robinson, Russell M. Robinson on North Carolina corporation law. 6th ed. New York: LEXIS Pub., 2000.

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Robinson, Russell M. Robinson on North Carolina corporation law. 5th ed. Charlottesville, Va: Michie, 1995.

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E, Snyder James. Snyder North Carolina corporation law and practice forms. Norcross, GA (3110 Crossing Park, Norcross, 30091-7500): Harrison Co., 1990.

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E, Snyder James. Snyder North Carolina corporation law and practice forms. 3rd ed. Suwanee, GA (1327 Northbrook Pkwy., Suite 400, Suwanee 30024-3586): Harrison Co., 1999.

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E, Snyder James. Snyder North Carolina corporation law and practice forms. 4th ed. [St. Paul, Minn.]: Thomson/West, 2003.

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E, Snyder James. Snyder North Carolina corporation law and practice forms. 2nd ed. Norcross, GA (3110 Crossing Park, Norcross, 30071-1367): Harrison Co., 1995.

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How to incorporate and start a business in North Carolina. Holbrook, Mass: Adams Media Corp., 1997.

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Book chapters on the topic "North Carolina Granite Corporation"

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Huffard, R. Scott. "Fighting the Octopus." In Engines of Redemption, 198–230. University of North Carolina Press, 2019. http://dx.doi.org/10.5149/northcarolina/9781469652818.003.0008.

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This chapter focuses on the creation and expansion of the Southern Railway corporation and the ways in which the corporation overcame anti-monopoly sentiment in the South. While the company styled itself as an embodiment of the New South, northern capitalist J.P. Morgan financed its reorganization, and its expansion engendered resistance in Georgia and North Carolina. This chapter traces the origins of this company in the economic depression and wave of railroad bankruptcies in the 1890s and notes the attempts to brand this new company as a southern enterprise under the leadership of its first president Samuel Spencer. The chapter then traces resistance to the new company in Georgia and North Carolina, two states in which the Southern Railway tried to purchase other railroads. Foes of the railroad, which formed a broad coalition of Populists, Democrats, and other anti-monopolists, labelled the road as an “octopus” for its monopolistic tendencies. In two case study states – Georgia and North Carolina – appeals to white supremacy and elections marked with violence, as in the Wilmington Massacre of 1898, defeated the anti-monopoly critique and preserved the power and size of the Southern Railway.
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Jenkins, E. W., R. C. Berger, J. P. Hallberg, S. E. Howington, C. T. Kelley, J. H. Schmidt, A. K. Stagg, and M. D. Tocci. "A Two-Level Aggregation-Based Newton-Krylov-Schwarz Method for Hydrology * *This research was supported in part by Army Research Office contract DAAD19-99-1-0186, US Army contract DACA39-95-K-0098, National Science Foundation grant DMS-9700569, a Cray Research Corporation Fellowship, and a Department of Education GAANN fellowship. Computing activity was partially supported by an allocation from the North Carolina Supercomputing Center." In Parallel Computational Fluid Dynamics 1999, 257–63. Elsevier, 2000. http://dx.doi.org/10.1016/b978-044482851-4.50032-3.

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Conference papers on the topic "North Carolina Granite Corporation"

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Daniels, Meredith, Brandon Governo, and Brittani D. McNamee. "IDENTIFICATION OF MINERALS IN SULFIDE BODY WITHIN GRANITE HOST AT NORTH BUNCOMBE QUARRY IN WESTERN NORTH CAROLINA." In 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-290706.

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Nose, Takehiko, Alexander Babanin, and Kevin Ewans. "Directional Analysis and Potential for Spectral Modelling of Infragravity Waves." In ASME 2016 35th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/omae2016-54282.

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In this paper, we interrogated wave data collected by US Army Corps of Engineers at their well-known Field Research Facility, Duck, North Carolina and SHELL Corporation at Lagos, Nigeria. Both measurements were designed to collect wind waves with a conventional wave sampling configuration and not a dedicated infragravity wave sampling regime. Here, we developed a new approach to obtain directional information of and explored the potential to model infragravity waves in the spectral domain. It was found that infragravity wave heights had a strong dynamic relationship with an inverse relative depth parameter and that directional spreadings were moderately correlated with wind wave spreadings and wave energy. Further, infragravity directional spreadings were typically broader compared to their wind wave directional spreading counterparts.
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Reports on the topic "North Carolina Granite Corporation"

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In-depth survey report: control of dust in a textile dyeing transfer operation at Logisco Corporation, Charlotte, North Carolina. U.S. Department of Health and Human Services, Public Health Service, Centers for Disease Control and Prevention, National Institute for Occupational Safety and Health, October 2002. http://dx.doi.org/10.26616/nioshephb22612a.

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