Relevant bibliographies by topics / Castlegate

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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 'Castlegate'

Author: Grafiati
Published: 4 June 2021
Last updated: 10 February 2022

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Journal articles on the topic "Castlegate"

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Pattison, Simon A. J. "High resolution linkage of channel-coastal plain and shallow marine facies belts, Desert Member to Lower Castlegate Sandstone stratigraphic interval, Book Cliffs, Utah-Colorado, USA." GSA Bulletin 131, no. 9-10 (2019): 1643–72. http://dx.doi.org/10.1130/b35094.1.

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AbstractThe Campanian Desert Member and Lower Castlegate Sandstone in the Book Cliffs of east-central Utah to western Colorado, USA, has served as a foundational data set in the development of sequence stratigraphy. Contrary to previous work, no third-order sequence boundaries are recognized. These were originally thought to partition the neighboring coastal plain and shallow marine facies belts into separate systems tracts, unlinked in time or space. In contrast, adjoining channel-coastal plain and shallow marine facies belts are genetically-, temporally-, and spatially-related. Evidence includes the (i) synchronous, strongly progradational stacking patterns within each facies belt, (ii) gradational and conformable transitions between adjoining facies belts, accentuated by the ubiquity of flat-topped, rooted foreshore sandstones passing upwards into carbonaceous-rich-mudstone-dominated coastal plain, (iii) parasequence-scale interfingering of coastal plain-channel and foreshore-shoreface deposits, with channels, white caps and coals embedded within stacked shoreface parasequences, (iv) regional correlation of coals and flooding surfaces, and (v) near orthogonal paleocurrent relationship between channels and shorelines. Terminal channels incise into proximal foreshore-shoreface sandstones in most Desert-Castlegate parasequences. Incisions are generally confined to the parasequence in which the channels are nested, rarely cutting deeper. These shoreface-incised channels are cut and filled at a parasequence-scale, and are bounded above by the same flooding surface that caps each foreshore-shoreface package. The ubiquity of ascending regressive shoreface trajectories and near absence of descending regressive trajectories that intersect depositional slope argues against any significant sea level fall. Increased rates of sediment supply, driven by autogenic and/or allogenic processes, likely generated the strongly progradational Desert-Castlegate great tongue of sandstone.
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Wordsworth, J., and N. A. McGavin. "Archaeological Work in Lanark 1979." Glasgow Archaeological Journal 12, no. 1 (1985): 93–104. http://dx.doi.org/10.3366/gas.1985.12.12.93.

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Summary Four areas of archaeological interest within the medieval burgh of Lanark were examined in advance of redevelopment by the Urban Archaeological Unit (now Scottish Urban Archaeological Trust). The medieval deposits were poorly preserved, but the excavations did suggest when the focus of the town shifted from the Castlegate to a High Street axis.
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Vinegar, H. J., J. A. De Waal, and S. L. Wellington. "CT studies of brittle failure in castlegate sandstone." International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts 28, no. 5 (1991): 441–50. http://dx.doi.org/10.1016/0148-9062(91)90082-w.

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Kibikas, William M., and Stephen J. Bauer. "Mechanical Response of Castlegate Sandstone under Hydrostatic Cyclic Loading." Geofluids 2021 (April 23, 2021): 1–18. http://dx.doi.org/10.1155/2021/8871103.

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The stress history of rocks in the subsurface affects their mechanical and petrophysical properties. Rocks can often experience repeated cycles of loading and unloading due to fluid pressure fluctuations, which will lead to different mechanical behavior from static conditions. This is of importance for several geophysical and industrial applications, for example, wastewater injection and reservoir storage wells, which generate repeated stress perturbations. Laboratory experiments were conducted with Castlegate sandstone to observe the effects of different cyclic pressure loading conditions on a common reservoir analogue. Each sample was hydrostatically loaded in a triaxial cell to a low effective confining pressure, and either pore pressure or confining pressure was cycled at different rates over the course of a few weeks. Fluid permeability was measured during initial loading and periodically between stress cycles. Samples that undergo cyclic loading experience significantly more inelastic (nonrecoverable) strain compared to samples tested without cyclic hydrostatic loading. Permeability decreases rapidly for all tests during the first few days of testing, but the decrease and variability of permeability after this depend upon the loading conditions of each test. Cycling conditions do affect the mechanical behavior; the elastic moduli decrease with the increasing loading rate and stress cycling. The degree of volumetric strain induced by stress cycles is the major control on permeability change in the sandstones, with less compaction leading to more variation from measurement to measurement. The data indicate that cyclic loading degrades permeability and porosity more than static conditions over a similar period, but the petrophysical properties are dictated more by the hydrostatic loading rate rather than the total length of time stress cycling is imposed.
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Ingraham, M. D., K. A. Issen, and D. J. Holcomb. "Response of Castlegate sandstone to true triaxial states of stress." Journal of Geophysical Research: Solid Earth 118, no. 2 (2013): 536–52. http://dx.doi.org/10.1002/jgrb.50084.

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McLaurin, Brett T., and Ron J. Steel. "Fourth-order nonmarine to marine sequences, middle Castlegate Formation, Book Cliffs, Utah." Geology 28, no. 4 (2000): 359–62. http://dx.doi.org/10.1130/0091-7613(2000)028<0359:fontms>2.3.co;2.

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McLaurin, Brett T., and Ron J. Steel. "Fourth-order nonmarine to marine sequences, middle Castlegate Formation, Book Cliffs, Utah." Geology 28, no. 4 (2000): 359. http://dx.doi.org/10.1130/0091-7613(2000)28<359:fntmsm>2.0.co;2.

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Rudnicki, J. W. "A three invariant model of failure in true triaxial tests on Castlegate sandstone." International Journal of Rock Mechanics and Mining Sciences 97 (September 2017): 46–51. http://dx.doi.org/10.1016/j.ijrmms.2017.06.007.

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Miall, A. D., and M. Arush. "The Castlegate Sandstone of the Book Cliffs, Utah: Sequence Stratigraphy, Paleogeography, and Tectonic Controls." Journal of Sedimentary Research 71, no. 4 (2001): 537–48. http://dx.doi.org/10.1306/103000710537.

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Stroisz, Anna Magdalena, and Erling Fjær. "Tracing causes for the stress sensitivity of elastic wave velocities in dry Castlegate sandstone." Geophysical Journal International 192, no. 1 (2012): 137–47. http://dx.doi.org/10.1093/gji/ggs029.

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Dissertations / Theses on the topic "Castlegate"

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Cross, David B. "High-frequency tectonic sequences in the Campanian Castlegate Formation during a transition from the Sevier to Laramide orogeny, Utah, U.S.A." ScholarWorks@UNO, 2016. http://scholarworks.uno.edu/td/2133.

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Though stratigraphic correlations are abundant in the Cordilleran basin-fill, they rarely include along-strike transects providing a spatio-temporal sense of deformation, sediment-supply and subsidence. A new, high-resolution, regional strike-correlation of the Castlegate Formation reveals progressive northward-growth of the San Rafael Swell during two embryonic episodes of Laramide-style deformation in central Utah. The intrabasinal deformation-events produced gentle lithospheric-folding punctuated by erosional-truncation of upwarped regions. The earliest episode occurred at 78 Ma in the southern San Rafael Swell likely causing soft-sediment deformation and stratal-tilting. Following this the alluvial-plain was leveled and rapid, extensive-progradation took place. A second episode, at 75 Ma, where deformation was focused in the northern San Rafael Swell, also caused sediment-liquefaction and erosional beveling. The stratal-tilting and sediment-liquefaction is attributed to seismicity induced by basal-traction between a subducting flat-slab and continental-lithosphere. The south-to north time-transgression of uplift is spatio-temporally consistent with NE-propagation of an oceanic-plateau subducted shallowly beneath the region.
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Willis, Andrew John. "Non-marine sequence stratigraphy of the Sego Sandstone and Upper Castlegate Sandstone, Upper Cretaceous, Book Cliffs, Utah, United States of America." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp02/NQ27752.pdf.

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Yocum, Daniel A. "Iron oolited from the cretaceous interor seaway Albian Paddy Member of the Peace River Formation, Alberta, Canada, and Campanian Castlegate Formation, Colorado, USA /." 1996. http://catalog.hathitrust.org/api/volumes/oclc/37183706.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 1996.
Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 70-74).
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Petter, Andrew Lucas 1980. "Stratigraphic implications of the spatial and temporal variability in sediment transport in rivers, deltas and shelf margins." Thesis, 2010. http://hdl.handle.net/2152/ETD-UT-2010-05-880.

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Sediment delivery to a basin exerts a first-order control over sedimentation, and therefore study of sedimentary rocks can reveal information about the nature of sediment delivery in the past. This dissertation examines several aspects of this problem using experimental, outcrop, and subsurface data. Flume experiments were undertaken to test the combined effects of autogenic alluvial aggradation and forced regression on the development of fluviodeltaic stratigraphy. Alluvial aggradation occurred in response to steady relative sea-level fall, and eventually consumed the entire sediment budget as the river lengthened in response to forced regression. The Campanian Lower Castlegate Sandstone (Utah) was studied as a potential ancient analog resulting from similar autogenic behaviors as observed in the experiments. Extensive measurement of grain-size distributions and paleo-flow depths from outcrop were utilized to explore downstream changes in paleo-hydraulics of the ancient fluvial systems in the Lower Castlegate in response to extensive alluvial aggradation and consequent loss of sediment from transport. An interesting finding was the stratigraphic signature of backwater hydraulic conditions in the distal reaches of the Lower Castlegate paleo-rivers. Finally, a simple and novel inversion scheme was developed for estimating paleo-sediment flux from ancient shelf-margin successions. An advantage of the methodology is that it allows for both spatial and temporal reconstruction of paleo-sediment flux patterns. The inversion scheme was applied to shelf-margin successions in the Washakie-Sand Wash Basin of Wyoming, the New Jersey Atlantic margin, the North Slope of Alaska, and the Zambezi margin of East Africa using published subsurface datasets. The Neogene passive margins within the studied datasets were found to consistently deposit around one-third of their total sediment budget on the shelf-margin topset, and bypass two-thirds of their budget beyond the shelf edge. The implications of this finding on the flux of terrestrial-derived particulate organic carbon (POC) from rivers to the ocean were explored, and a long-term average flux of POC to deepwater storage was estimated. The sediment-flux inversion scheme was also applied to derive input parameters for stratigraphic modeling of the Ebro margin. The modeling results indicate that the autostratigraphic behavior of the margin may have been previously underestimated.
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Books on the topic "Castlegate"

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The secret of Castlegate Manor. Avalon Books, 2003.

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Hercules and the farmer's wife: And other stories from a Cumbrian art gallery. Aurum, 2009.

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Farrar, Karen W. Castlegar: A confluence. Castlegar and District Heritage Society, 2000.

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Laoi, Padraic O. History of Castlegar Parish. P. Ó Laoi, 1996.

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Volovsek, Walter O. Trails in time: Reflections : an illustrated history about the development of walking and ski touring trails in the vicinity of Castlegar, British Columbia. Otmar Pub., 2012.

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Hercules and the Farmers Wife. Aurum Press, 2010.

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Coalbed methane resource map, Castlegate D bed, Book Cliffs coal field, Utah. Utah Geological Survey, 1991. http://dx.doi.org/10.34191/ofr-176e.

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Coalbed methane resource map, Castlegate A bed, Book Cliffs coal field, Utah, 1990. Utah Geological Survey, 1990. http://dx.doi.org/10.34191/ofr-176a.

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Coalbed methane resource map, Castlegate B bed, Book Cliffs coal field, Utah, 1990. Utah Geological Survey, 1990. http://dx.doi.org/10.34191/ofr-176b.

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Coalbed methane resource map Castlegate C Bed, Book Cliffs coal field, Utah, 1990. Utah Geological Survey, 1990. http://dx.doi.org/10.34191/ofr-176c.

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Book chapters on the topic "Castlegate"

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Ingraham, Mathew D., Kathleen A. Issen, and David J. Holcomb. "Failure of Castlegate Sandstone Under True Triaxial Loading." In Advances in Bifurcation and Degradation in Geomaterials. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-1421-2_42.

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Butterworth, Carolyn, and Ranald Lawrence. "Provocateurs or consultants? The role of Sheffield School of Architecture in the co-production of Castlegate." In Architecture and Resilience. Routledge, 2018. http://dx.doi.org/10.4324/9781315159478-10.

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Wagoner, John C. Van. "Road Log, Day FourNonmarine Sequence Stratigraphy and Facies Architecture of the Downdip Castlegate Sandstone in the Book Cliffs of Western Colorado and Eastern Utah." In Sequence Stratigraphy Applications to Shelf Sandstone ReservoirsOutcrop to Subsurface Examples. American Association of Petroleum Geologists, 1991. http://dx.doi.org/10.1306/sp548c10.

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Wagoner, John C. Van. "Road Log, Day ThreeNonmarine Sequence Stratigraphy and Facies Architecture of the Updip Desert and Castlegate Sandstones in the Book Cliffs of Western Colorado and Eastern Utah." In Sequence Stratigraphy Applications to Shelf Sandstone ReservoirsOutcrop to Subsurface Examples. American Association of Petroleum Geologists, 1991. http://dx.doi.org/10.1306/sp548c9.

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Wagoner, John C. Van. "Sequence Stratigraphy and Facies Architecture of the Desert Member of the Blackhawk Formation and the Castlegate Formation in the Book Cliffs of Eastern Utah and Western Colorado." In Sequence Stratigraphy Applications to Shelf Sandstone ReservoirsOutcrop to Subsurface Examples. American Association of Petroleum Geologists, 1991. http://dx.doi.org/10.1306/sp548c3.

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Pattison, Simon A. J. "Alternative sequence stratigraphic model for the Desert Member to Castlegate Sandstone interval, Book Cliffs, eastern Utah: Implications for the high-resolution correlation of falling stage nonmarine, marginal-marine, and marine strata." In Through the Generations: Geologic and Anthropogenic Field Excursions in the Rocky Mountains from Modern to Ancient. Geological Society of America, 2010. http://dx.doi.org/10.1130/2010.0018(08).

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Conference papers on the topic "Castlegate"

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Chamberlin, Ellen P., Annabel Spranger, and Elizabeth Hajek. "FINE-GRAINED SEDIMENT STORAGE IN ANCIENT DEPOSITS: AN EXAMPLE FROM THE BLACKHAWK-CASTLEGATE FORMATION BOUNDARY (CRETACEOUS, UTAH, USA)." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-299924.

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Papamichos, Euripides, Lars Erik Walle, Andreas Nicolas Berntsen, and Dawid Szewczyk. "Sand Mass Production in Anisotropic Stresses From Lab to Field Predictions." In SPE Annual Technical Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/205929-ms.

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Abstract Sand onset and sand rate predictions are important in hydrocarbon production to optimize production, increase recovery, and reduce costs and the environmental footprint. Recent laboratory results on Castlegate sandstone from sand production tests in a True Triaxial test system have revealed that stress anisotropy plays an important role not only on sand onset but also in sand rate. The results confirmed our hypothesis that stress anisotropy means earlier sand produced but less sand. The laboratory results also revealed the effect of fluid saturation, i.e., oil, brine or irreducible water saturation on sand onset and sand rate. They allow the calibration of SandPredictor, a field sand prediction model, for stress anisotropy and production before and after water breakthrough. A field case analysis demonstrated the effects and showed the importance of in situ stress anisotropy and watercut on sand mass and rate.
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Chamberlin, Ellen P., and Elizabeth Hajek. "ESTIMATING THE RELATIVE SAND-TO-MUD RATIOS OF PALEO-SEDIMENT SUPPLY: AN EXAMPLE FROM THE MUD-DOMINATED BLACKHAWK TO SAND-DOMINATED CASTLEGATE FORMATION TRANSITION, UPPER CRETACEOUS, UTAH, USA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283037.

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Reports on the topic "Castlegate"

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Halwas, D. B., and P. S. Simony. The Castlegar Gneiss Complex, southern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120428.

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Structure contour map of the top of the Castlegate Sandstone, eastern part of the Uinta Basin and the western part of the Piceance Creek basin, Utah and Colorado. US Geological Survey, 1986. http://dx.doi.org/10.3133/mf1826.

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