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Academic literature on the topic 'Geology – Barbados'

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Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Geology – Barbados"

Donovan, Stephen K., and David A. T. Harper. "Barbados." Geology Today 25, no. 4 (2009): 151–58. http://dx.doi.org/10.1111/j.1365-2451.2009.00724.x.

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Larue, D. K., and K. G. Provine. "Vacillatory turbidites, Barbados." Sedimentary Geology 57, no. 3-4 (1988): 211–19. http://dx.doi.org/10.1016/0037-0738(88)90028-0.

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MacDonald, William D. "Caribbean Geological Conference, Barbados." Geology 15, no. 1 (1987): 89. http://dx.doi.org/10.1130/0091-7613(1987)15<89:cgcb>2.0.co;2.

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Speed, R. C., L. H. Barker, and P. L. B. Payne. "GEOLOGIC AND HYDROCARBON EVOLUTION OF BARBADOS." Journal of Petroleum Geology 14, no. 2 (1991): 323–42. http://dx.doi.org/10.1111/j.1747-5457.1991.tb00315.x.

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Takizawa, Shigeru, and Yujiro Ogawa. "Dilatant clayey microstructure in the Barbados décollement zone." Journal of Structural Geology 21, no. 1 (1999): 117–22. http://dx.doi.org/10.1016/s0191-8141(98)00097-2.

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BURNS, STEPHEN J., and VICTOR ROSSINSKY. "Late Pleistocene mixing zone dolomitization, southeastern Barbados, West Indies." Sedimentology 36, no. 6 (1989): 1135–37. http://dx.doi.org/10.1111/j.1365-3091.1989.tb01547.x.

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HUMPHREY, JOHN D. "Late Pleistocene mixing zone dolomitization, southeastern Barbados, West Indies." Sedimentology 35, no. 2 (1988): 327–48. http://dx.doi.org/10.1111/j.1365-3091.1988.tb00951.x.

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Brown, K. M., and G. K. Westbrook. "The tectonic fabric of the Barbados Ridge accretionary complex." Marine and Petroleum Geology 4, no. 1 (1987): 71–81. http://dx.doi.org/10.1016/0264-8172(87)90022-5.

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Humphrey, J. D. "New Geochemical Support for Mixing-Zone Dolomitization at Golden Grove, Barbados." Journal of Sedimentary Research 70, no. 5 (2000): 1160–70. http://dx.doi.org/10.1306/101399701160.

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Babaie, Hassan A., Robert C. Speed, David K. Larue, and George E. Claypool. "Source rock and maturation evaluation of the Barbados accretionary prism." Marine and Petroleum Geology 9, no. 6 (1992): 623–32. http://dx.doi.org/10.1016/0264-8172(92)90035-d.

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Dissertations / Theses on the topic "Geology – Barbados"

Cuevas, Elba Dayton. "The radiolarian biostratigraphy of the oceanic formation, Conset Bay, Barbados, West Indies." FIU Digital Commons, 1994. http://digitalcommons.fiu.edu/etd/2681.

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A hemipelagic/pelagic sequence from Conset Bay, Barbados, West Indies, was prepared and reviewed to establish the radiolarian biostratigraphy and zonation of the area. This study shows that the sequence extends from the Middle Eocene, Dictyoprora mongolfieri zone, to the Late Eocene, Thyrsocyrtis bromia zone. Two zones, the Podocyrtis ampla zone and the Podocyrtis mitra zone have not been identified although the sequence appears to be stratigraphically continuous. Their absence is related to a sampling gap where an interval of the outcrop is covered with slope wash. The Conset Bay sediments are characterized by extensive reworking of older taxa from several stratigraphic level throughout the time span covered in the present study.

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Ouellette, Gilman Reno. "Late Holocene Paleoenvironmental Reconstruction in Barbados." TopSCHOLAR®, 2013. http://digitalcommons.wku.edu/theses/1285.

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Barbados is the easternmost island in the Caribbean region, and is uniquely situated between the Atlantic Ocean and Caribbean Sea. Being an isolated island with a karstified aquifer providing the majority of the nation’s water resources, Barbados has found itself in water scarce situations in recent years. In order to better understand natural shifts in groundwater recharge (which is determined by shifts in precipitation), longer records of precipitation are needed than are available from modern measurements. This study presents a paleoclimate reconstruction for the late Holocene on Barbados using stable and radiogenic isotope ratios in speleothem lamina as proxies. In addition, it introduces the use of novel mineralogical analyses using Raman spectroscopy and large chamber-scanning electron microscopy to supplement the oxygen isotope record. For the past 1,500 years, the speleothem record indicates average δ18O values near -4.1 0/00, maximum δ18O values around -3.2 0/00 that coincide with the Little Ice Age climate event, while minimum δ18O values around -5.3 0/00 occur during the Medieval Climate Anomaly. Raman spectral analysis shows a recent period of increased Mg substitution, which potentially represents anthropogenic changes to the island’s epikarst aquifer caused by European settlement and sugar cane cultivation on Barbados. Electron imaging revealed chemically distinct layers of detritus within the stalagmite sample, facilitating precise sampling for U-series dating while also providing some information on the nature of weathering on the island. Additionally, time series analysis of the isotope record indicates multidecadal and multicentennial periodicities that conform well to that of the Atlantic Multidecadal Oscillation exerting influence on rainfall variability at the decadal scale, and the Intertropical Convergance Zone modulating rainfall at the multicentennial scale. Collectively, these data provide a climate reconstruction for the island of Barbados that is useful for better understanding change in cyclic precipitation patterns, as well as non-destructive methods for speleothem analysis that complement the isotopic study, while allowing sample preservation.

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Hall, Veronica. "Addressing Water Resource Issues In Barbados Through An Isotopic and Atmospheric Characterization of Precipitation Variability." TopSCHOLAR®, 2014. http://digitalcommons.wku.edu/theses/1356.

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Numerous studies have analyzed isotopic variation of meteoric and dripwater in karst environments for paleoclimate reconstructions or aquifer recharge capacity. What is poorly understood is how the isotopic signal of δ18O and δ2H is transferred through the hydrologic cycle based upon storm type, frequency, intensity, and teleconnection activity in the tropical karst areas. At Harrison’s Cave, Barbados, a Hobo Onset event data logger was attached to a tipping bucket rain gauge to count the tips and record the total rainfall every 10 minutes. In the cave a Hobo data logger was used to record relative humidity and temperature at 10-minute intervals. Rainwater, dripwater, and stream water samples were collected at a weekly resolution and refrigerated before sample analysis. The study period was from July, 2012 to October, 2013, with data from the data loggers only until June, 2013 due to inability to reach the study site. The samples were analyzed using the Picarro Cavity Ring Down Spectroscopy Unit-Water L1102-I through laboratories at the University of Kentucky and the University of Utah. The samples were reported in per mil and calibrated. The teleconnection (NAO, AMO, and ENSO) and other atmospheric data were obtained from the Climate Prediction Center or the NOAA Earth System Research Laboratory-Physical Sciences Division. The weekly isotope signatures were linearly regressed against total rainfall for Harrison’s Cave and surface temperature with no statistically significant correlation, indicating the amount effect was not present at a weekly resolution. The amountweighted precipitation δ18O values were calculated on a monthly basis and compared to TRMM monthly rainfall and island-wide monthly rainfall, and a statistically significant negative correlation was found between both datasets. This confirmed that the amount effect dominates the island’s rainfall isotopic signature at a monthly resolution, and that specific atmospheric influences represented in weekly rainfall were less influential on a weekly basis. It is hypothesized that the variation in weekly rainfall is due to quick initiating, rain-out, and dissipation of convective storm systems over the island. In terms of evaporative influences, the samples do not deviate much from the Global Meteoric Water Line (GMWL), indicating minimal evaporation, which is typical for tropical locations. When the d-excess parameters were calculated, there were distinct variations with minimal evaporation occurring in the 2013 calendar year. This is attributed to coastal storm formation in the tropics.

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Carpentier, Marion. "Composition chimique des sédiments entrant dans la zone de subduction des Petites Antilles." Phd thesis, Universite Libre de Bruxelles, 2007. http://tel.archives-ouvertes.fr/tel-00187335.

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Les laves provenant de l'arc des Petites Antilles sont caractérisées par une grande variabilité chimique et leurs compositions isotopiques suggèrent une contribution variable de matériel crustal ancien dans leur genèse. L'arc des Petites Antilles est également caractérisé par une zonation chimique nord-sud, les laves des îles du sud présentant généralement des signatures isotopiques crustales plus fortes que celles des îles du nord. Nous avons tenté dans cette étude d'établir s'il existe des variations de la composition chimique des sédiments entrant en subduction le long de l'arc, et si d'éventuels changements de leur composition peuvent expliquer les variations chimiques observées au sein des laves. Pour ce faire, nous avons réalisé une étude géochimique approfondie (majeurs, traces, isotopes du Sr, du Nd, de l'Hf et du Pb) du flux sédimentaire potentiellement entrant dans la zone de subduction à différentes latitudes. L'échantillonnage comprend des sédiments forés au niveau des sites 543 (nord de l'arc) et 144 (extrême sud de l'arc) lors des campagnes DSDP 78A et 14 respectivement, et des sédiments provenant de l'île de la Barbade (sud de l'arc). <br />Les échantillons présentent une grande hétérogénéité lithologique correspondant globalement à un mélange en proportion variable entre une composante détritique et une composante biogénique (siliceuse ou carbonatée). De plus, au niveau du site 144, des niveaux très riches en matière organique (black shales) datant du Cénomanien supérieur au Santonien (~ 95 à 84 Ma) ont été forés. Ces formations correspondent à l'enregistrement des Oceanic Anoxic Events 2 et 3. Nous avons montré que la « dilution » variable de la fraction détritique par la composante biogénique est le facteur qui contrôle largement les variations de concentrations en éléments traces observées. De plus, nous avons révélé un enrichissement en U extrêmement important au sein des black shales du site 144. Les signatures isotopiques de l'Hf, du Nd et du Pb sont dominées par la composante détritique, alors que celle du Sr, dans le cas d'échantillons riches en carbonates est dominée par celle de l'eau de mer. Les sédiments des trois sites présentent des compositions isotopiques du Pb fortement radiogéniques par rapports aux sédiments océaniques « classiques », que nous avons associées à une forte contribution de matériel issu de l'altération des cratons guyanais et brésilien dans la composante détritique. De plus, la décroissance radioactive de l'U dans les black shales du site 144 a généré des rapports 206-207Pb/204Pb extrêmement radiogéniques. <br />Un mélange entre le manteau appauvri et les sédiments du site 543 reproduit les compositions isotopiques des laves de la partie nord de l'arc. Pour la partie sud de l'arc un mélange entre les sédiments les plus radiogéniques en Pb du site 144 et le manteau appauvri explique les compositions des laves des îles de la Martinique à Grenade. Une contribution croissante des black shales du nord vers le sud est nécessaire, et est de plus en accord avec l'augmentation du nord vers le sud de l'âge du plancher océanique subduit. Enfin, quelques sédiments de l'île de la Barbade présentent certaines caractéristiques compatibles avec leur implication dans la genèse des laves de la partie sud de l'arc.

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Jones, Ian Christopher. "Geochemical evolution of groundwater in the Pleistocene limestone aquifer of Barbados." Thesis, 2002. http://wwwlib.umi.com/cr/utexas/fullcit?p3110625.

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Books on the topic "Geology – Barbados"

H, Schomburgk Robert. The history of Barbados: Comprising a geographical and statistical description of the island : a sketch of the historical events since the settlement, and an account of its geology and natural productions. Frank Cass, 1998.

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Speed, Robert C., and Hai Cheng. Emergence and Evolution of Barbados. Edited by Christine Speed, Richard Sedlock, and Lawrence Andreas. Geological Society of America, 2021. http://dx.doi.org/10.1130/spe549.

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Emergence and Evolution of Barbados is a three-part analysis of the Quaternary geologic and geomorphologic evolution of the island of Barbados in the southeastern Caribbean. “Geology of Southeastern Barbados” assembles and integrates detailed observations into a complex 700 k.y. history of marine sculpting and riverine flooding processes. “Marine Terrace Evolution of Windward Barbados” revises the Quaternary stratigraphy of the island, describes the tectonics of emergence, and demonstrates that uplift rates vary by location. “Active Emergence, Chronology, and Limestone Facies in Southeastern Windward Barbados” is the first comprehensive study to integrate marine erosion and deposition with tectonic uplift rates. Major findings of this work are that Barbados’ Central Highlands are an erosional remnant, and that terraces originated principally by marine erosion rather than by reef construction.

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Geology and Geomorphology of Barbados: A Companion Text to Maps with Accompanying Cross Sections, Scale 1:10,000. Geological Society of America, 2013. http://dx.doi.org/10.1130/9780813724911.

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Speed, Robert C., Christine Speed, and Richard Sedlock. Geology and Geomorphology of Barbados: A Companion Text to Maps with Accompanying Cross Sections, Scale 1:10,000. Geological Society of America, 2013. http://dx.doi.org/10.1130/spe491.

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H, Schomburgk Robert. History of Barbados: Comprising a Geographical and Statistical Description of the Island; a Sketch of the Historical Events since the Settlement; and an Account of Its Geology and Natural Productions. University of Cambridge ESOL Examinations, 2010.

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Book chapters on the topic "Geology – Barbados"

Taylor, Elliott, Patti J. Burkett, Jeri D. Wackler, and John N. Leonard. "Physical Properties and Microstructural Response of Sediments to Accretion-Subduction: Barbados Forearc." In Frontiers in Sedimentary Geology. Springer New York, 1991. http://dx.doi.org/10.1007/978-1-4612-4428-8_22.

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Tribble, Jane Schoonmaker, Fred T. Mackenzie, and Jozsef Urmos. "Physical Property Changes Accompanying Deep Burial of Clay-Rich Sediments, Barbados Convergent Margin." In Frontiers in Sedimentary Geology. Springer New York, 1991. http://dx.doi.org/10.1007/978-1-4612-4428-8_8.

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Speed*, Robert C., and Hai Cheng†. "Geology of southeastern Barbados." In Emergence and Evolution of Barbados. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2549(03).

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ABSTRACT This chapter presents geological documentation of Quaternary (and perhaps older) event histories of southeastern Barbados. The Barbados Limestone is herein formally defined. A time-stratigraphic division of the Barbados Limestone in southeastern Barbados and the properties of the stratigraphic units are presented. A major finding of this study is that the marine terraces originated wholly by marine erosion, not by reef construction, and evolved in stages over a long duration. The hydrology and thickness data of the Barbados Limestone are discussed, and hypotheses on causes of thickness variations are given. The study domain is divided into seven areas that contain a continuous flight of nine marine terraces preserved in various partial sequences. Discussions of these key seven areas in southeastern Barbados are supported by geologic maps at large scale and cross sections. Sections with VE &gt; 1 display limestone stratigraphy and facies over relatively large lengths. Sections with VE = 1 show true structural configurations over short lengths. Detailed observations and radio isotopic dating of the limestone units permit differentiation and correlation among them.

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Deville, Eric, and Alain Mascle. "The Barbados ridge." In Phanerozoic Regional Geology of the World. Elsevier, 2012. http://dx.doi.org/10.1016/b978-0-444-53042-4.00021-2.

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Humphrey, John D. "Geology and Hydrogeology of Barbados." In Developments in Sedimentology. Elsevier, 2004. http://dx.doi.org/10.1016/s0070-4571(04)80033-5.

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Maltman, A., P. Labaume, and B. Housen. "Structural geology of the décollement at the toe of the Barbados accretionary prism." In Proceedings of the Ocean Drilling Program, 156 Scientific Results. Ocean Drilling Program, 1997. http://dx.doi.org/10.2973/odp.proc.sr.156.037.1997.

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Speed, Robert C., Christine Speed, and Richard Sedlock. "Geology and Geomorphology of Barbados: A Companion Text to Maps with Accompanying Cross Sections, Scale 1:10,000." In Geology and Geomorphology of Barbados: A Companion Text to Maps with Accompanying Cross Sections, Scale 1:10,000. Geological Society of America, 2013. http://dx.doi.org/10.1130/2012.2491.

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"CD-ROM Contents." In Geology and Geomorphology of Barbados: A Companion Text to Maps with Accompanying Cross Sections, Scale 1:10,000. Geological Society of America, 2013. http://dx.doi.org/10.1130/2012.2491.vii.

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Speed, Christine, and Richard Sedlock. "Note from the Editors." In Geology and Geomorphology of Barbados: A Companion Text to Maps with Accompanying Cross Sections, Scale 1:10,000. Geological Society of America, 2013. http://dx.doi.org/10.1130/2012.2491.ix.

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Wothers, Peter. "Goblins and Demons." In Antimony, Gold, and Jupiter's Wolf. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780199652723.003.0008.

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The belief that there were no more than seven metals persisted for hundreds of years, and it was not until the seventeenth century that the inconvenient, inescapable realization came that there were probably many more. I’ve already mentioned Barba’s report from 1640 about the new metal bismuth; it was one of a number of metals or metal-like species that began to be noticed in the sixteenth and seventeenth centuries. In his History of Metals from 1671, Webster begins Chapter 27: ‘Having now ended our Collections and Discourse of the seven Metals, vulgarly accounted so; we now come to some others, that many do also repute for Metals; and if they be not so, at least they are semi-Metals, and some of them accounted new Metals or Minerals, of that sort that were not known to the Ancients.’ In the chapter Webster speaks of antimony, arsenic, bismuth, cobalt, and zinc. While we now understand these as distinct elements, earlier on there was great confusion, with the names being used for compounds rather than the elements themselves—and, furthermore, the different compounds and elements often being mistaken for each other. This makes unravelling their history all the more complicated. We’ll start with Barba’s ‘Mettal between Tin and Lead, and yet distinct from them both’: bismuth. The first mention of bismuth predates Barba’s reference by more than one hundred years. The name appears in its variant spelling, ‘wissmad’, in what is probably the very first book on mining geology. This was published around the turn of the sixteenth century and attributed to one Ulrich Rülein von Calw, the son of a miller who entered the University of Leipzig in 1485. Ulrich mentions in passing that bismuth ore can be an aid to finding silver, since the latter is often found beneath it. Consequently, miners called bismuth ‘the roof of silver’. As Webster later put it in his History of Metals, ‘The ore from whence it is drawn . . . is also more black, and of a leaden colour, which sometimes containeth Silver in it, from whence in the places where it is digged up, they gather that Silver is underneath, and the Miners call it the Cooping, or Covering of Silver.’

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Conference papers on the topic "Geology – Barbados"

Deville, E., N. Ellouz, J.-P. Herbin, J.-P. Houzay, and A. Prinzhofer. "The Mud Volcanoes Tectonic Setting and Associated Hydrocarbon Migrations - New Insight from Barbados, Trinidad and Sicily." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406081.

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Reports on the topic "Geology – Barbados"

Speed, Robert. Geologic Map of Barbados: Volume II. Geological Society of America, 2019. http://dx.doi.org/10.1130/speed_map-vol_2.

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