Academic literature on the topic 'Clew Bay'

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Journal articles on the topic "Clew Bay"

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CHEW, D. M. "Structural and stratigraphic relationships across the continuation of the Highland Boundary Fault in western Ireland." Geological Magazine 140, no. 1 (January 2003): 73–85. http://dx.doi.org/10.1017/s0016756802007008.

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The relationship between the Dalradian Supergroup and the Highland Border Complex in Scotland has remained contentious for over a century. In western Ireland, the contact between the Dalradian Supergroup and the Clew Bay Complex (a correlative of the Highland Border Complex) is superbly exposed on the island of Achill Beg on the North Mayo coast. The unfossiliferous South Achill Beg succession has been traditionally assigned to the Clew Bay Complex, and this interpretation is supported by a combination of Sm–Nd model age data, heavy mineral analysis and lithostratigraphic correlation. TDM ages range from 1.99–2.66 Ga (mean=2.28 Ga, n=6). Detailed structural mapping shows that both the Dalradian and the Clew Bay Complex share the same structural history. A D1 high strain event is common to both units, and is associated with the development of tectonic slides. The D2 event is responsible for the formation of crustal-scale nappes. In both units, beds are consistently downward facing on the S2 foliation. Later dextral shearing (D3) resulted in the tilting of the originally recumbent, S-facing D2 nappes into this downward-facing orientation. Rb–Sr and 40Ar–39Ar radiometric dating of muscovite confirms that both units were deformed contemporaneously as the S2 nappe fabric in each is dated at c. 460 Ma. This Middle Ordovician age for deformation of the Clew Bay Complex is highly significant, not least because published microfossil data suggest a Silurian age.
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RICE, A. H. N., and D. M. WILLIAMS. "Caledonian strike-slip terrane accretion in W. Ireland: insights from very low-grade metamorphism (illite–chlorite crystallinity and b0parameter)." Geological Magazine 147, no. 2 (October 5, 2009): 281–98. http://dx.doi.org/10.1017/s0016756809990446.

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AbstractAnalysis of pelites with detrital white-micas in the Clew Bay–Galway Bay segment of the Irish Caledonides indicates that b0data from whole-rock and < 2 μm fractions generally show differences smaller than the errors of the method, irrespective of (001) illite crystallinity values, probably due to metamorphic recrystallization. Intermediate pressure metamorphism of the Ordovician–Silurian Clew Bay Group indicates slow subduction, allowing partial thermal re-equilibration before exhumation. In contrast, the Croagh Patrick Group Laurentian shelf-sediments underwent high-pressure alteration, suggesting rapid subduction/exhumation, synchronous with strike-slip faulting. The Murrisk Group, which underwent high-intermediate pressure metamorphism in an Ordovician back-arc, forms a separate terrane to the Croagh Patrick Group to the north and also to the Ordovician Lough Nafooey and Tourmakeady groups and Rosroe Formation in the south, in which low-intermediate pressure alteration occurred. These, together with the Silurian North Galway Group, may have undergone heating due to movement over or deposition on the hot Gowlaun Detachment as the Connemara Dalradian was exhumed. The South Connemara Group also underwent a high-pressure alteration, consistent with its inferred subduction environment. Evidence of contact alteration, due to known or inferred buried late- to post-Caledonian granitoid plutons, has been found in the Clew Bay, Louisburg–Clare Island, Croagh Patrick, Murrisk and South Connemara groups. These show evidence of lower-pressure alteration than the surrounding country-rocks.
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Johnston, J. D., and W. E. A. Phillips. "Terrane amalgamation in the Clew Bay region, west of Ireland." Geological Magazine 132, no. 5 (September 1995): 485–501. http://dx.doi.org/10.1017/s0016756800021154.

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AbstractThe Caledonides of the west of Ireland provide a well-exposed and well-mapped example of an oblique collision zone. The east-northeast trending Deer Park and Achill Beg Fault system is a crustal scale ductile sinistral strike-slip duplex of late Ordovician age, imbricating late Precambrian granulite facies lower crustal rocks, near eclogite facies supracrustal rocks, up to amphibolite facies Dalradian metasedimentary rocks and greenschist facies Cambro-Ordovician rocks. This fault system is correlated with a pre-Devonian component of the Highland Boundary Fault system in southern Scotland. In the Clew Bay area, the high pressure-low temperature facies metamorphic rocks, in tectonic contact with greenschist facies Cambro-Ordovician rocks, are together interpreted as an accretionary prism complex related to northwestward directed subduction. Both of these are allocthonous terrains with respect to the Dalradian terrane to the north (North West Mayo). To the south, the Cambro-Ordovician rocks docked with a probable Dalradian block containing ultramafic intrusives (Deer Park Complex) during the late Ordovician. The Deer Park Complex and South Mayo Trough linked earlier, during the Arenig.Silurian and Lower-Middle Devonian redbed successions sit unconformably on the metamorphic rocks. Deposition and deformation of these cover rocks was controlled by oblique strike-slip movements on the Leek Fault whose strike swings from west-northwest to north-northeast, following earlier basement trends, as it is traced eastwards from Clew Bay. The Leek Fault System may be correlated with the Leannan Fault of northwest Donegal, a splay of the Great Glen Fault system of central Scotland. East of Clew Bay, this sinistral shear generated local dilation on the more northerly trending bend of the Leek Fault. Lower and Middle Old Red Sandstone redbeds were developed here. The west-northwest trend of the Leek Fault in Clew Bay acted as a compressional bend during these sinistral movements and transpressional southwest directed thrusting developed in Silurian rocks. Post-Middle Old Red Sandstone pre-late Tournaisian dextral displacement on the Leek Fault reversed this pattern with transtension in Clew Bay allowing intrusion of small carbonated peridotite bodies into Silurian rocks and easterly directed thrusting of Middle Old Red Sandstone rocks east of the Bay on the transpressional north-south bend.A tectonic model for the region is presented here. This model involves a northwestward directed subduction system, 150 to 750 km of Arenig sinistral strike slip movement, and eastwards insertion of the Connemara block with formation of the Ordovician South Mayo Trough as a pull-apart basin. Subsequently, a further 130 to 650 km eastward displacement of rocks took place south of the Deer Park Fault in later Ordovician times. The magnitudes of these estimates are directly proportional to an assumed maximum wavelength of 1500 km for promontories on the original Laurentian margin, and using the current juxtaposition of terranes, a minimum wavelength of 300 km is inferred.
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Knight, Jasper. "Subglacial processes from drumlins in Clew Bay, western Ireland." Earth Surface Processes and Landforms 41, no. 2 (December 16, 2015): 277–88. http://dx.doi.org/10.1002/esp.3865.

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Williams, D. M. "Evolution of Ordovician terranes in western Ireland and their possible Scottish equivalents." Transactions of the Royal Society of Edinburgh: Earth Sciences 81, no. 1 (1990): 23–29. http://dx.doi.org/10.1017/s0263593300005101.

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ABSTRACTIn the W of Ireland the Ordovician rocks of South Mayo and Clew Bay are now juxtaposed but a comparison of the sedimentary histories of these two sequences shows that they accumulated in basins which were probably separated during most of their history. The large amount of terrigenous detritus present in the Arenig to Llanvirn elements of the South Mayo succession is not manifest in that of Clew Bay until the Llandeilo/Caradoc, by which time sedimentation in South Mayo had ceased. A comparison of the South Mayo Ordovician with that of Girvan in Scotland demonstrates that both sequences had a similar provenance. This source contained an ophiolite, granites and some (probably pre-Dalradian) metamorphic rocks. Sediment dispersal directions for the two sequences are opposite in sense, being primarily northward in South Mayo and southward at Girvan. The two stratigraphies indicate that basement subsidence behaviour in South Mayo was virtually the opposite of that at Girvan where initial shallow water sedimentation was rapidly succeeded by deep water environments at the end of the Llanvirn. The two basins may thus have been marginal to a single Ordovician arc complex. One reason for the opposite sense of basin subsidence may lie in the suggested reversal of subduction polarity during the Ordovician. In this scenario the South Mayo basin may be envisaged as lying to the N of a northward-facing arc during the early Ordovician. A new, northward, subduction direction instigated during the Llanvirn, resulted in a fore-arc basin at Girvan complemented by a closing back-arc basin in South Mayo.
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TANNER, P. W. G. "The role of the Highland Border Ophiolite in the ∼ 470 Ma Grampian Event, Scotland." Geological Magazine 144, no. 3 (April 20, 2007): 597–602. http://dx.doi.org/10.1017/s0016756807003342.

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Field and petrological studies of the Highland Border Ophiolite demonstrate that it was obducted onto the Neoproterozoic–Ordovician rocks of the Dalradian block, and not emplaced against them by post-orogenic strike-slip movement. It was welded onto the upper, southward-younging limb of the already recumbent Tay Nappe (D1), and deformed by the Downbend Antiform (D4). However, its emplacement was not accompanied by significant internal deformation of the Dalradian block. As the ophiolite is correlated with those at Clew Bay, Tyrone and Shetland, this result will necessitate complete revision of the current model for basin closure on the southeastern margin of Laurentia.
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PALMER, D., J. D. JOHNSTON, T. DOOLEY, and K. MAGUIRE. "Short paper: The Silurian of Clew Bay, Ireland: part of the Midland Valley of Scotland?" Journal of the Geological Society 146, no. 3 (May 1989): 385–88. http://dx.doi.org/10.1144/gsjgs.146.3.0385.

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McCAFFREY, K. J. W. "Controls on reactivation of a major fault zone: the Fair Head–Clew Bay line in Ireland." Journal of the Geological Society 154, no. 1 (January 1997): 129–33. http://dx.doi.org/10.1144/gsjgs.154.1.0129.

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Harkin, J., D. M. Williams, J. F. Menuge, and J. S. Daly. "Turbidites from the Clew Bay Complex, Ireland: provenance based on petrography, geochemistry and crustal residence values." Geological Journal 31, no. 4 (December 1996): 379–88. http://dx.doi.org/10.1002/(sici)1099-1034(199612)31:4<379::aid-gj719>3.0.co;2-x.

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Max, Michael D. "The clew bay group: A displaced terrane of highland border group rocks (Cambro-ordovician) in Northwest Ireland." Geological Journal 24, no. 1 (April 30, 2007): 1–17. http://dx.doi.org/10.1002/gj.3350240102.

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Dissertations / Theses on the topic "Clew Bay"

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Carolan, J. "Late-Quaternary to present coastal change : a study linking the offshore with coastal sequences, Clew Bay, Co. Mayo, Ireland." Thesis, Queen's University Belfast, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.431528.

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Books on the topic "Clew Bay"

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Lawrence, Durrell. Clea. New York: Penguin Books, 1991.

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Tom & Clem. London: Faber and Faber, 1997.

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ill, Mockford Caroline, ed. Cleo and Caspar. Cambridge, MA: Barefoot Books, 2006.

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Yi, Xie Jingwen, ed. Zong you ni pei ban: Cleo: how an uppity cat helped heal a family. Zhangsha: Hu nan wen yi chu ban she, 2011.

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Leo, Tolstoy. The power of darkness, or, 'If a claw is caught, the bird is lost'. Bath, England: Absolute Classics, 1989.

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Leo, Tolstoy. The power of darkness, or If a claw is caught, the bird is lost. Bath, Eng: Absolute Classics, 1989.

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Oates, Joyce Carol. Blackwater. South Yarmouth, MA: Curley, 1993.

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Oates, Joyce Carol. Black water. London: Picador, 1994.

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Oates, Joyce Carol. Black water. New York, N.Y., U.S.A: Dutton, 1992.

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Oates, Joyce Carol. Black water. Hampton, N.H: Curley Large Print, 1993.

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Book chapters on the topic "Clew Bay"

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Galland, Bernard. "La «clef pendante» en stuc dans la troisième travée du bas-côté nord de la cathédrale Notre-Dame du Puy-en-Velay." In Bibliothèque de l'Antiquité Tardive, 237–38. Turnhout: Brepols Publishers, 2006. http://dx.doi.org/10.1484/m.bat-eb.3.145.

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Riggs, Nancy, Brian McConnell, and John Graham. "Sedimentary provenance of Silurian basins in western Ireland during Iapetus closure." In New Developments in the Appalachian-Caledonian- Variscan Orogen. Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2554(16).

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ABSTRACT Three Silurian basin fills, the Llandovery–Wenlock Croagh Patrick and Killary Harbour–Joyce Country successions and the Ludlow–Pridoli Louisburgh–Clare Island succession, overstep the tectonic contacts between elements of the Grampian (Taconic) accretionary history of the Caledonian-Appalachian orogeny in western Ireland. New U-Pb detrital zircon data from lower strata of these Silurian rocks provide insight into basin evolution and paleogeography. The shallow-marine Croagh Patrick succession unconformably overlies the Clew Bay Complex and the northern part of the Ordovician South Mayo Trough. Two samples have zircon populations dominated by Proterozoic grains typical of the Laurentian margin, with few younger grains. Up to 13% of the grains form a cluster at ca. 950–800 Ma, which is younger than known Grenville magmatism on the local Laurentian margin and older than known magmatism from Iapetan rifting; these may be recycled grains from Dalradian strata, derived from distal Tonian intrusions. The Killary Harbour–Joyce Country succession overlies the structural contact between the Lough Nafooey arc and the Connemara Dalradian block and records a transgressive-regressive cycle. Four samples of the Lough Mask Formation show contrasting age spectra. Two samples from east of the Maam Valley fault zone, one each from above Dalradian and Nafooey arc basement, are dominated by Proterozoic grains with ages typical of a Laurentian or Dalradian source, likely in north Mayo. One sample also includes 8% Silurian grains. Two samples from west of the fault overlie Dalradian basement and are dominated by Ordovician grains. Circa 450 Ma ages are younger than any preserved Ordovician rocks in the region and are inferred to represent poorly preserved arc fragments that are exposed in northeastern North America. Cambrian to late Neoproterozoic grains in association with young Ordovician ages suggest derivation from a peri-Gondwanan source in the late stages of Iapetus closure. The Louisburgh–Clare Island succession comprises terrestrial red beds. It unconformably overlies the Clew Bay Complex on Clare Island and is faulted against the Croagh Patrick succession on the mainland. The Strake Banded Formation yielded an age spectrum dominated by Proterozoic Laurentian as well as Ordovician–Silurian ages. Although the basin formed during strike-slip deformation along the Laurentian margin in Ireland and Scotland, sediment provenance is consistent with local Dalradian sources and contemporaneous volcanism. Our results support ideas that Ganderian continental fragments became part of Laurentia prior to the full closure of the Iapetus Ocean.
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Wendling, Linda Ann. "The Practice and the Pressure to Progress." In Handbook of Research on Future of Work and Education, 476–94. IGI Global, 2022. http://dx.doi.org/10.4018/978-1-7998-8275-6.ch028.

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As one of the most traditional professions, the practice of law has been slower than most to adapt to technological advances and recognize the impact on the changing nature of work for attorneys. Only two state bar associations currently require continuing legal education in technology. New York's bar association has recommended mandatory training in cybersecurity; however, it would comprise only 1 credit within the Ethics & Professionalism Continuing Legal Education (CLE) requirements. This chapter will explore the negative “domino effect” that disregarding or underestimating the power of technology in both legal education and practice can have on access, diversity, and ultimately justice. By presenting the evidence here, perhaps the profession through its many and varied institutions and organizations can finally turn against the tide of tradition. The profession and its oversight bodies must look farther back in the pathway to practice to re-imagine legal education and embrace that which is now possible through technology and innovative teaching and learning methods.
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Roeder, John. "Kaija Saariaho, “The claw of the magnolia … ,” From the Grammar of Dreams (1988)." In Analytical Essays on Music by Women Composers: Concert Music from 1960-2000, 155–75. Oxford University Press, 2016. http://dx.doi.org/10.1093/acprof:oso/9780190236861.003.0007.

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Conference papers on the topic "Clew Bay"

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Robson, Nina, Bin Yun Chen, Jong-Seob Won, and Gim Song Soh. "Creating Robust Passive Multi-Loop Wearable Hand Devices." In ASME 2019 International Design Engineering Technical Conferences and Computers and Information in Engineering Conference. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/detc2019-97623.

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Abstract This paper describes a process for assessing multi-loop wearable devices that use a common slider to passively drive the exo-fingers for the physical training of people with limited hand mobility. Each finger design, except for the thumb, is based on an RRR serial chain, termed backbone, constrained into a multi-loop eight-bar slider mechanism using two RR constraints. The thumb utilizes a planar RR backbone chain constrained into a parallel four bar slider. During the physical task acquisition experiments, the subject’s tip finger trajectories are captured using an optical motion capture and its dimensions are set such that they match each of the fingers kinematics as closely as possible. The dimensional synthesis procedure can yield a variety of design candidates that fulfill the desired fingertip precision grasping trajectory. Once it is ensured that the synthesized fingertip motion is close to the physiological fingertip grasping trajectories, performance assessment criteria related to user-device interference and natural joint angle movement are taken into account. After the most preferred design for each finger is chosen, minor modifications related to substituting the backbone chain with the wearer’s limb to provide the skeletal structure of the customized passive device are made. To illustrate the proposed technique, the development of a 3D prototype model of a passively actuated Closed Loop Articulated Wearable (CLAW) hand is presented. The CLAW hand performance with respect to wear-ability and robustness was assessed. Preliminary test results with healthy subjects show that the CLAW hand is easy to operate and able to guide the user’s fingers without causing any discomfort, ensuring both, precision and power grasping in a natural manner. The lack of electrical actuators and sensors simplifies the control, resulting in a lightweight and cost-effective solution for grasping of a variety of objects with different sizes. This work establishes the importance of incorporating novel design candidate assessment techniques, based on human finger kinematic models, within the conceptual design level that can assist in finding robust design candidates with naturalistic joint motion.
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THAYER, JOHN GREGG. "CLEO RESULTS FOR b → sγ AND $B^{\pm} \rightarrow K^{\pm}\nu\bar{\nu}$." In Proceedings of the Sixteenth Lake Louise Winter Institute. WORLD SCIENTIFIC, 2002. http://dx.doi.org/10.1142/9789812777706_0039.

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"CLE and BAM genes in phloem development in potato (Solanum tuberosum L.)." In Plant Genetics, Genomics, Bioinformatics, and Biotechnology. Novosibirsk ICG SB RAS 2021, 2021. http://dx.doi.org/10.18699/plantgen2021-126.

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Agrawal, Govind P. "Self-Phase Modulation in Optical Fiber Communications: Good or Bad?" In CLEO 2007. IEEE, 2007. http://dx.doi.org/10.1109/cleo.2007.4453562.

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ECKLUND, K. M. "A Search for C/P in ${B^0} - {\bar B^0}$ Mixing and a Measurement of |Vcb| Using ${\bar B^0}\, \to \,D{*^ + }{\ell ^ - }\bar \nu $ from CLEO." In Proceedings of the International Workshop. WORLD SCIENTIFIC, 2001. http://dx.doi.org/10.1142/9789812811219_0039.

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Nunn, Joshua, Tessa F. Champion, Joseph Munns, Cheng Qiu, Dylan Saunders, and Ian A. Walmsley. "Bad Cavities for Good Memories: Storing Broadband Photons with Low Noise." In CLEO: QELS_Fundamental Science. Washington, D.C.: OSA, 2015. http://dx.doi.org/10.1364/cleo_qels.2015.fth4b.1.

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Yang, Yong, Manuel Crespo-Ballesteros, and Misha Sumetsky. "Experimental demonstration of a bat microresonator." In 2021 Conference on Lasers and Electro-Optics Europe & European Quantum Electronics Conference (CLEO/Europe-EQEC). IEEE, 2021. http://dx.doi.org/10.1109/cleo/europe-eqec52157.2021.9542687.

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Lane, Randall J., Alan B. Petersen, and John Gloyd. "CW 795 nm Rb Vapor Laser Pumped by Volume Transmission Grating-Stabilized Diode Bar." In CLEO 2007. IEEE, 2007. http://dx.doi.org/10.1109/cleo.2007.4452949.

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Dai, Zijie, Jing Yang, Qiang Su, Pengfei Qi, Dan Lu, Cheng Gong, Lu Sun, and Weiwei Liu. "An broadband terahertz metamaterial filter based on multiplexed metallic bar resonators." In CLEO: Applications and Technology. Washington, D.C.: OSA, 2018. http://dx.doi.org/10.1364/cleo_at.2018.jth2a.178.

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Bonner, C. L., C. T. A. Brown, D. P. Shepherd, W. A. Clarkson, A. C. Tropper, D. C. Hanna, and B. Ferrand. "Diode-bar pumped, high-power, planar Nd:YAG waveguide laser." In Technical Digest Summaries of papers presented at the Conference on Lasers and Electro-Optics Conference Edition. 1998 Technical Digest Series, Vol.6. IEEE, 1998. http://dx.doi.org/10.1109/cleo.1998.676294.

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Reports on the topic "Clew Bay"

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Ahmed, Nabil, Anna Marriott, Nafkote Dabi, Megan Lowthers, Max Lawson, and Leah Mugehera. Inequality Kills: The unparalleled action needed to combat unprecedented inequality in the wake of COVID-19. Oxfam, January 2022. http://dx.doi.org/10.21201/2022.8465.

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The wealth of the world’s 10 richest men has doubled since the pandemic began. The incomes of 99% of humanity are worse off because of COVID-19. Widening economic, gender, and racial inequalities—as well as the inequality that exists between countries—are tearing our world apart. This is not by chance, but choice: “economic violence” is perpetrated when structural policy choices are made for the richest and most powerful people. This causes direct harm to us all, and to the poorest people, women and girls, and racialized groups most. Inequality contributes to the death of at least one person every four seconds. But we can radically redesign our economies to be centered on equality. We can claw back extreme wealth through progressive taxation; invest in powerful, proven inequality-busting public measures; and boldly shift power in the economy and society. If we are courageous, and listen to the movements demanding change, we can create an economy in which nobody lives in poverty, nor with unimaginable billionaire wealth—in which inequality no longer kills.
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