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Добірка наукової літератури з теми "Ferrar"

Автор: Grafiati

Опубліковано: 4 червня 2021

Оновлено: 31 січня 2023

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Статті в журналах з теми "Ferrar"

1

Coltharp, Duane. "Richard Gough, Peter Peckard, and the Problem of Little Gidding." Journal of Anglican Studies 18, no. 1 (May 2020): 74–97. http://dx.doi.org/10.1017/s1740355320000212.

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AbstractThis article explores the ways in which Little Gidding and its inhabitants – including the leader of that pious seventeenth-century household, Nicholas Ferrar – were remembered in the late eighteenth and early nineteenth centuries. The memory of Little Gidding was shaped, in part, by a passage in Richard Gough’s British Topography, in which Gough dismissed Nicholas Ferrar as a ‘useless enthusiast’. Gough’s attack was answered by the liberal churchman Peter Peckard, who defended the reputation of his wife’s ancestor in his Memoirs of the Life of Mr. Nicholas Ferrar. And yet Peckard’s response to the Ferrars of Little Gidding was not entirely approving: while Peckard celebrated their piety and benevolence, he also worried over their ‘ceremonials’ and their ‘austerities’. This article presents a reading of the Memoirs, as well as a study of the relationship between Peckard’s text and other contemporary sources, in order to shed light on the complex nature of Peckard’s liberal Anglicanism.

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2

Neumann, Peter M., and M. E. Rayner. "William Leonard Ferrar." Bulletin of the London Mathematical Society 26, no. 4 (July 1994): 395–401. http://dx.doi.org/10.1112/blms/26.4.395.

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3

Barbour, Reid. "The Caroline Church Heroic: The Reconstruction of Epic Religion in Three Seventeenth-Century Communities." Renaissance Quarterly 50, no. 3 (1997): 771–818. http://dx.doi.org/10.2307/3039262.

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In his biography of Nicholas Ferrar, A.L. Maycock speaks volumes in describing the Ferrar family's transition in 1625 as a movement from one venture (the Virginia Company) to another, the “great adventure” of Little Gidding. In this one phrase Maycock comprehends the view of its founders that no less than the Virginia Company's epic plantation of true religion among the Indians, the community at Little Gidding ranks as a heroic enterprise, the discursive preoccupation of which proves to be the very nature of Christian heroism itself. Even if readers of the Ferrar papers do not know how highly Nicholas Ferrar prized the Acts and Monuments, it is impossible for them to miss the Foxeian narratives of “heroic suffering” so pervasive in the “story books” left as folio records of the dialogues performed by the so-called Little Academy.

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4

Brewer, T. S. "Mesozoic dolerites from Whichaway Nunataks." Antarctic Science 1, no. 2 (June 1989): 151–55. http://dx.doi.org/10.1017/s0954102089000222.

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The southernmost exposures of Mesozoic dolerites in Coats Land, the Omega dolerites, occur at Whichaway Nunataks. The dolerites are geochemically indistinguishable from the Theron Mountains' dolerites. In both regions high- and low-Ti compositions occur with trace element signatures more akin to island-arc magmas than within-plate tholeiites. From a preliminary Sr isotopic study the Omega dolerites can be classified as Ferrar type. The existence of Ferrar type material in these nunataks suggest that the boundary between the Ferrar and Weddell Sea sub-provinces occurs within the Theron Mountains.

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5

Smyth, Adam. "Thinking with Ferrar Papers 1422: A c. 1681 Verse Miscellany." Library 21, no. 2 (June 1, 2020): 192–215. http://dx.doi.org/10.1093/library/21.2.192.

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Abstract This article explores a late seventeenth-century manuscript verse miscellany held amongst the Ferrar Papers in Magdalene College, Cambridge, not previously discussed by critics. By attending to both the specific features of this manuscript miscellany (including poems by John Dryden, Katherine Philips. and others), and the larger Ferrar archive, the article considers broader questions about how to read and interpret manuscript miscellanies.

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6

Morrison, A. D., and A. Reay. "Geochemistry of Ferrar Dolerite sills and dykes at Terra Cotta Mountain, south Victoria Land, Antarctica." Antarctic Science 7, no. 1 (March 1995): 73–85. http://dx.doi.org/10.1017/s0954102095000113.

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At Terra Cotta Mountain, in the Taylor Glacier region of south Victoria Land, a 237 m thick Ferrar Dolerite sill is intruded along the unconformity between basement granitoids and overlying Beacon Supergroup sedimentary rocks. Numerous Ferrar Dolerite dykes intrude the Beacon Supergroup and represent later phases of intrusion. Major and trace element data indicate variation both within and between the separate intrusions. Crystal fractionation accounts for much of the geochemical variation between the intrusive events. However, poor correlations between many trace elements require the additional involvement of open system processes. Chromium is decoupled from highly incompatible elements consistent with behaviour predicted for a periodically replenished, tapped and fractionating magma chamber. Large ion lithophile element-enrichment and depletion in Nb, Sr, P and Ti suggests the addition of a crustal component or an enriched mantle source. The trace element characteristics of the Dolerites from Terra Cotta Mountain are similar to those of other Ferrar Group rocks from the central Transantarctic Mountains and north Victoria Land, as well as with the Tasmanian Dolerites. This supports current ideas that the trace element signature of the Ferrar Group is inherited from a uniformly enriched mantle source region.

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7

Leat, P. T., T. R. Riley, B. C. Storey, S. P. Kelley, and I. L. Millar. "Middle Jurassic ultramafic lamprophyre dyke within the Ferrar magmatic province, Pensacola Mountains, Antarctica." Mineralogical Magazine 64, no. 1 (February 2000): 95–111. http://dx.doi.org/10.1180/002646100549021.

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AbstractAn ultramafic lamprophyre dyke is described from the otherwise tholeiitic Ferrar magmatic province of Antarctica. We report an Ar-Ar age of 183 ± 2.2 Ma for the dyke, indistinguishable from those of the Ferrar tholeiites. However, the dyke has mineralogical and major and trace element compositions, and radiogenic isotopes ratios, very different from the Ferrar tholeiites. The sample consists of olivine and rare clinopyroxene phenocrysts with perovskite and spinel microphenocrysts in a groundmass of amphibole, nepheline and biotite. Carbonatitic globules contain calcite, dolomite, Fe-rich carbonate, nepheline, biotite, orthoclase, pyrite, clinopyroxene, apatite and silicate glass, and were formed by liquid immiscibility. The rock is mildly potassic and classifies as an ouachitite. It is strongly enriched in both moderately and highly incompatible trace elements and is the first high-Ti rock to be described from the Ferrar magmatic province. The rock has similar initial 143Nd/144Nd to OIB, notably Bouvet, Crozet and Réunion, but significantly higher initial 87Sr/86Sr. The lamprophyre magma is interpreted as having been generated by low-degree partial fusion of metasomatized lithospheric mantle as a result of heat conducted from an underlying Jurassic mantle plume. The same mantle plume was probably also responsible for generating one of the world’s largest layered gabbro bodies, the Dufek-Forrestal intrusions.

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8

Yanbin, Shen. "Jurassic conchostracans from Carapace Nunatak, southern Victoria Land, Antarctica." Antarctic Science 6, no. 1 (March 1994): 105–13. http://dx.doi.org/10.1017/s0954102094000131.

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Fossiliferous horizons of the Ferrar Group at Carapace Nunatak of southern Victoria Land have yielded the richest and most diverse freshwater Jurassic biota hitherto recorded from Antarctica. Fossil conchostracans are the most important in terms of number of individuals and distributional area. Scanning electron microscopy is used to establish a new genus and species (Carapacestheria balli), and Cyzicus (Lioestheria) disgregaris Tasch is attributed to Carapacestheria disgregaris (Tasch) emend. The conchostracan fauna of the Ferrar Group, characterized by Carapacestheria, is probably of early Middle Jurassic age.

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9

THISTLEWOOD, L., P. T. LEAT, I. L. MILLAR, B. C. STOREY, and A. P. M. VAUGHAN. "Basement geology and Palaeozoic–Mesozoic mafic dykes from the Cape Meredith Complex, Falkland Islands: a record of repeated intracontinental extension." Geological Magazine 134, no. 3 (May 1997): 355–67. http://dx.doi.org/10.1017/s0016756897007085.

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Mafic dykes (Groups A–D) intruded into Mesoproterozoic basement amphibolites, gneisses, and granitoids of the Cape Meredith Complex on the southern tip of West Falkland, provide an important record of at least three periods of lithospheric extension during Palaeozoic and Jurassic times. Group A dykes are calc-alkaline lamprophyres that were generated by partial melting of an enriched subcontinental lithospheric mantle in Cambro-Ordovician times. Group B dykes are Ordovician dolerites derived from an asthenospheric mantle source, perhaps during the same extensional episode as Group A dykes. Group C dykes were also derived from an asthenospheric source and are possibly of Silurian age. The youngest, Group D, dykes are part of the widespread Jurassic Gondwana province. This group contains an oceanic island basalt-like sample and an enriched sample similar to both Group A lamprophyres and to the Jurassic Ferrar province in Antarctica. These correlations have interesting implications for the composition and evolution of mantle sources through time; the co-existence of Cambrian lamprophyres and Jurassic Ferrar-type magmas in the Cape Meredith Complex demonstrate for the first time that the enriched lithospheric mantle source postulated for the Ferrar magmas existed as far back as Cambrian times.

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10

Dixit, Atul. "Analogues of the general theta transformation formula." Proceedings of the Royal Society of Edinburgh: Section A Mathematics 143, no. 2 (March 18, 2013): 371–99. http://dx.doi.org/10.1017/s0308210511001685.

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A new class of integrals involving the confluent hypergeometric function 1F1(a;c;z) and the Riemann Ξ-function is considered. It generalizes a class containing some integrals of Ramanujan, Hardy and Ferrar and gives, as by-products, transformation formulae of the form F(z, α) = F(iz, β), where αβ = 1. As particular examples, we derive an extended version of the general theta transformation formula and generalizations of certain formulae of Ferrar and Hardy. A one-variable generalization of a well-known identity of Ramanujan is also given. We conclude with a generalization of a conjecture due to Ramanujan, Hardy and Littlewood involving infinite series of the Möbius function.

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Дисертації з теми "Ferrar"

1

Plankell, Eric Thomas. "Magma emplacement models for the Jurassic Ferrar Dolerite Province, Antarctica /." Connect to resource, 1997. http://hdl.handle.net/1811/28549.

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2

Ziga, Jeffrey M. "Geochemistry of Ferrar Dolerite sills in the Shackleton Glacier region, Antarctica /." Connect to resource, 2003. http://hdl.handle.net/1811/6469.

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Thesis (Honors)--Ohio State University, 2003.
Advisor: David Elliot, Dept. of Geological Sciences. Includes bibliographical references (leaves 28-29). Available online via Ohio State University's Knowledge Bank

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3

Fleming, Thomas Harold. "Isotopic and Chemical Evolution of The Ferrar Group, Beardmore Glacier Region, Antarctica /." The Ohio State University, 1995. http://rave.ohiolink.edu/etdc/view?acc_num=osu1487929745335032.

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4

Riley, Kate E. "The good old way revisited : the Ferrar family of Little Gidding c.1625-1637." University of Western Australia. School of Humanities, 2008. http://theses.library.uwa.edu.au/adt-WU2008.0026.

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[Truncated abstract] The Ferrars are remembered as exemplars of Anglican piety. The London merchant family quit the city in 1625 and moved to the isolated manor of Little Gidding in Huntingdonshire. There they pursued a life of corporate devotion, supervised by the head of the household, Nicholas Ferrar, until he died in December 1637. To date, the life of the pious deacon Nicholas Ferrar has been the focus of histories of Little Gidding, which are conventionally hagiographical and give little consideration to the experiences of other members of the family, not least the many women in the household. Further, customary representations of the Ferrars have tended to remove them from their seventeenth-century context. Countering the biographical trend that has obscured many details of their communal life, this thesis provides a new, critical reading of the family's years at Little Gidding while Nicholas Ferrar was alive. It examines the Ferrars in terms of their own time, as far as possible using contemporary documents instead of later accounts and confessional mythology. It shows that, while certain aspects of life at Little Gidding were unusual, on the whole the family was less exceptional than traditional histories have implied; certainly the family was not so unified and unworldly as the idealised images have suggested. Moreover, the Ferrars were actively engaged in making those images, for immediate effect and for posterity. The Ferrars' identities, corporate and individual, and their largely textual practices of self-fashioning are central to the study. Other key concerns are the Ferrars' moral and religious ideals and practices, gender in the family, and intra-familial relationships. Evidence for the thesis is drawn from family documents dating from the early years of the seventeenth century to the time of Nicholas Ferrar's death. ... The Little Academy is considered first: in this unique dialogue circle, young women discussed morally edifying historical tales, offering them a textually-mediated experience of the world and working to reinforce conventional gender roles and religious values. The final three chapters pertain to the copious and little-studied family correspondence. A chapter that develops a theory of the functions of the family correspondence network is followed by one studying the affective relationships that the celibate sisters Mary and Anna Collet maintained through their letters with their unmarried uncle and spiritual mentor, Nicholas Ferrar. These chapters consider the identities as single people that all three developed through these relationships, within the maritally-focused framework of the Protestant family. The last chapter also concerns the lives of the unmarried, examining the relationships of single male adults and their roles in the family, focusing on the friendship of Nicholas Ferrar and his cousin Arthur Woodnoth. The thesis closes by reflecting on the fact that returning the Ferrars to their seventeenth-century context reveals their multi-faceted nature, comprising ideals and identities sometimes incongruous with one another, and certainly unaccounted for in the traditional narratives. It thus demonstrates the importance of the overall project of reconceiving the Ferrars? history, which forms an original contribution to the study of the social, cultural and religious history of early seventeenth-century England.

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5

Lafleur, Didier. "Enquête sur le stemma du groupe Ferrar dans l'Evangile de Marc : les nouvelles données de la recherche." Paris, EPHE, 2005. http://www.theses.fr/2005EPHE5053.

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Les manuscrits du groupe Farrar – appelés aussi famille 13 – comptent parmi les témoins de premier ordre du Nouveau Testament grec. Pour l’Evangile de Marc, onze manuscrits – tous copiés en écriture minuscule – sont actuellement reconnus : neuf tétraévengiles, un lectionnaire et un Nouveau Testament complet. De par leurs caractéristiques textuelles spécifiques ils appartiennent au type de texte dit « césaréen ». La première partie de ce travail porte sur la mise en perspective des quatre premiers manuscrits de ce groupe, dans des éditions imprimées : Nouveau Testament grec, répertoires catalographiques, de 1670 à la fin du dix-neuvième siècle. Cette histoire des éditions souligne le rôle essentiel joué par ces quatre témoins dans l’histoire de la critique textuelle néotestamentaire. L’élaboration d’un nouveau stemma pour le groupe Farrar dans l’Evangile de Marc prend appui sur l’édition intégrale du texte publié ici pour la première fois. L’ensemble de la collation, basée sur l’édition de Legg de 1935, représente 4631 lieux variants. L’édition de ce texte conduit à une enquête minutieuse de critique verbale, de critique interne et de critique externe. Elle montre que l’archétype du groupe, nommé x, s’est divisé en trois branches : a, qui regroupe cinq manuscrits dont un fortement contaminé par le texte byzantin ; c, qui rassemble trois manuscrits, et b, qui ne compte que deux descendants ; l’un de ceux-ci est le témoin le plus proche de l’archétype. L’étude s’attache à définir, pour chacun des groupes et pour l’archétype x, des ensembles de cariantes caractéristiques. L’enquête se termine par une bibliographie de 873 notices représentant 382 auteurs
Manuscripts of the Farrar Group – also called Family 13 – are first class witnesses of the Greek New Testament. Concerning Mark’s Gospel, eleven manuscripts – all copied in minuscule writing – are officially accepted: nine contain the four Gospels, one is a lectionary, the last one a complete New Testament. Because of their textual peculiar readings, they both belong to the so-called text-type “caesarean”. The first part of the thesis gives a wide outlook on the four first manuscripts of this group in the printed editions of Greek New Testament and manuscript catalogues, from 1670 to the end of the 19th century. The history of these editions points out the leading role of theses codices in the New Testament textual criticism. The edition of the text of the Ferrar manuscripts for the Gospel of Mark is given here for the very first time. The collations of the manuscripts, based on the Legg edition (1935), represent 4631 readings. The stemma codicum takes place on these collations. All kinds of textual criticism are meticulously detailed on the survey as internal and external evidence. It states that the archetype of the group, called x, is divided into three branches: a, which consists in five manuscripts whom one is strongly byzantine contaminated; c, which represents three manuscripts and b, which only has two manuscripts. One manuscript of this b-group certainly is the nearest to the archetype of Family 13. The study finally points out some peculiar reading for all these branches. The survey makes an end with a bibliography composed by 873 files divides in 382 authors

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6

Janosy, Robert John. "Structural investigations of the early paleozoic Victoria land dike swarm in the Ferrar-Koettlitz glacier region, Southern Victoria Land, Antarctica." The Ohio State University, 1994. http://rave.ohiolink.edu/etdc/view?acc_num=osu1300117001.

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7

Ware, Bryant Douglas. "Large Igneous Provinces of the Southern Hemisphere: Isotopic Geochemistry and Plagioclase and Pyroxene 40Ar/39Ar Geochronology of the Kalkarindji, Karoo and Ferrar Provinces." Thesis, Curtin University, 2017. http://hdl.handle.net/20.500.11937/57565.

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To develop a comprehensive understanding of geological processes a multidisciplinary approach must be utilized. This PhD research contributes to the understanding of Large Igneous Provinces (LIPs) petrogenesis through an integrated geochemical and high precision geochronological approach. This study integrates geochemical analyses and unprecedented high-precision and sensitive 40Ar/39Ar geochronology to continue to push various geochronological techniques and LIP research to new horizons.

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8

Freitas, Diogo Martins de. "Equity research - Ferrari N.V." Master's thesis, Instituto Superior de Economia e Gestão, 2018. http://hdl.handle.net/10400.5/17354.

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Mestrado em Finanças
O presente relatório de Equity Research tem por objectivo determinar o justo valor da fabricante italiana de supercarros de luxo, Ferrari. Nesse sentido, um preço-alvo para o final do ano de 2018 foi desenvolvido e posteriormente concretizado numa recomendação de investimento, tendo por base o processo de avaliação e o preço actual da acção. A primeira etapa do processo de avaliação compreende uma breve análise macroeconómica da indústria em que a empresa se insere, seguida de uma análise operacional. Posteriormente segue-se um tratamento de dados financeiros fundamentais para o desenvolvimento do modelo de Discount Cash Flow (DCF) e para o modelo de avaliação relativa com em base em Múltiplos. O modelo de Discount Cash Flow (DCF) deriva um preço por acção no final de 2018 de € 121.21. Em contraste, a abordagem via múltiplos é ligeiramente mais conservadora, com um valor-alvo por acção de € 115.36. Em 30 de Junho de 2018, o preço da acção em mercado foi fixado em € 116.50, o que deixa espaço para um potencial de valorização de cerca de 4%, considerando o valor obtido através do modelo DCF. O rendimento futuro dos dividendos é esperado ser de 0.70%. Desde o início do ano, o retorno anual da acção foi de 36%, juntamente com uma volatilidade anual de 31%, valores estes que podem ser explicados em certa medida pela ainda recente IPO e a consequente descoberta de preço pelo mercado.
The present equity research report aims to determine the fair value of the Italian Supercar manufacturer, Ferrari. In that sense, a target price towards the end of 2018 is developed and concretized in an investment recommendation given the outcome of the process of due diligence followed by the respective business valuation. The first step of the valuation process comprehends an analysis of both the industry where the company operates and its operational activity. Subsequently, the assumptions and the forecasted financials are present as they represent the fundamental quantitative data where both the discounted cash flow and multiples valuation models rely on. The discounted cash flow model (DCF) derives a share price towards the end of 2018 of €121.21. By contrast, the multiples approach is slightly more conservative with a share value of €115.36. On 30th of June 2018 the market share price was set at €116.50 which leaves room for an upside potential of about 4% given the DCF target share value. The forward dividend yield is expected to be 0.70%. Since the beginning of the year, the annual stock return averaged 36% with an annual volatility of 31%.
info:eu-repo/semantics/publishedVersion

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9

Felizardo, Rafael Grilli. "Equity research - Ferrari N.V." Master's thesis, Instituto Superior de Economia e Gestão, 2020. http://hdl.handle.net/10400.5/20808.

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Mestrado em Finanças
Este relatório é uma avaliação da Ferrari N.V., preparada como Projeto de Trabalho Final de Mestrado em Finanças pelo ISEG. O trabalho segue o formato recomendado pelo Instituto CFA. A avaliação foi conduzida considerando dados disponíveis publicamente em 07 de outubro de 2020, e diversas fontes de informação foram utilizadas, como relatórios da empresa, Thomson Reuters, Bloomberg L.P., yahoofinance.com. Novidades após essa data não estão contempladas na análise. O preço alvo de €177.48 (dezembro de 2020) representa um potencial de valorização de 17% em relação ao preço de fechamento de 30 de julho de 2020, e a recomendação para a Ferrari N.V. é COMPRA, com risco médio avaliado.
This report is a valuation of Ferrari N.V. prepared as a Master's in Finance Final Work Project at ISEG, following the format recommended by the CFA Institute for Equity Research reports. The study was conducted considering publicly available data on October 07th, 2020, and diverse sources of information were used, such as company reports, Thomson Reuters, Bloomberg L.P., yahoofinance.com. Novelties after this date were not included. The target price (TP) was achieved based on the DCF method, complemented with Adjusted Present Value, Economic Value Added and Relative Valuation. The TP of €177.48 (2020YE) represents an upside potential of 17% over the close price of July 30, 2020, and the final recommendation for Ferrari N.V. is BUY, with medium risk assessed.
info:eu-repo/semantics/publishedVersion

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10

Woolley, Benjamin. "The Angel of Ferrara." Thesis, Goldsmiths College (University of London), 2015. http://research.gold.ac.uk/11398/.

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This thesis comprises two components: an extract of The Angel of Ferrara, a historical novel, and a critical commentary entitled What is history doing in Fiction? The novel is set in the Italian city of Ferrara in February, 1579, a jewel of the Renaissance at the height of its powers but deep in debt. Amid the aristocratic pomp and popular festivities surrounding the duke’s marriage to his third wife, the secret child of the city’s most celebrated singer goes missing. A street-smart debt collector and lovelorn bureaucrat help her increasingly desperate attempts to find her son, their efforts uncovering the brutal instruments of ostentation and domination that gave rise to what we now know as the Renaissance. In the critical commentary, I draw on the experience writing The Angel of Ferrara, together with my own historical works, to explore the relationship between history and fiction. Beginning with a survey of the development of historical fiction since the inception of the genre’s modern form with the Walter Scott’s Waverley, I analyze the various paratextual interventions—prefaces, authors’ notes, acknowledgements—authors have used in their attempts to explore and explain the use of factual research in their works. I draw on this to reflect in more detail at how research shaped the writing of the Angel of Ferrara and other recent historical novels, in particular Hilary Mantel’s Wolf Hall. I then examine the issue form the opposite perspective: the use of fictional devices such as narrative in history, considering whether or not this compromises or enhances the authority and validity of historical work. I end by critically examining the prevailing notion that the borderline between fiction and history has become blurred, arguing that, while each influences the other, the distinction is one of type rather than degree.

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Книги з теми "Ferrar"

1

Further researches into the history of the Ferrar-Group. London: C.J. Clay, 1985.

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2

The web of friendship: Nicholas Ferrar and Little Gidding. Cambridge [Eng.]: James Clarke & Co., 2011.

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3

Maia, Virgílio. Album de iniciação à heráldica das marcas de ferrar gado. Fortaleza, Ceará: Biblioteca O Curumim Sem Nome Editora, 1992.

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4

Elliot, David H. Potassium-argon age determinations of Ferrar Group rocks, central Transantarctic Mountains. Washington, D.C: American Geophysical Union, 1985.

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5

Brown, Andrew J. Robert Ferrar: Yorkshire monk, Reformation bishop and martyr in Wales (c.1500-1555). London: Inscriptor Imprints, 1997.

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6

Der griechisch-syrische Text des Matthäus: E 351 im Verhältnis zu Tatian Ssc Ferrar. Leipzig: B.G. Teubner, 1989.

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7

H, Elliot David, Lindsay John F, and Wade F. Alton 1903-, eds. The Beacon Supergroup (Devonian-Triassic) and Ferrar Group (Jurassic) in the Beardmore Glacier Area, Antarctica. Washington, D.C: American Geophysical Union, 1986.

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8

On the origin of the Ferrar-Group: A lecture on the genealogical relations of New Testament mss. London: C.J. Clay, 1985.

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9

Ferrar, John. Materials for the life of Nicholas Ferrar: A reconstruction of John Ferrar's account of his brothers's life based on all the surviving copies. Leeds: Leeds Philosophical and Literary Society, 1996.

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10

Lehbrink, Hartmut. Ferrari. Köln: Könemann, 1995.

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Частини книг з теми "Ferrar"

1

Symonds, Richard. "Nicholas Ferrar." In Alternative Saints, 77–88. London: Palgrave Macmillan UK, 1988. http://dx.doi.org/10.1007/978-1-349-19690-6_8.

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2

Faure, Gunter, and Teresa M. Mensing. "The Ferrar Group: Kirkpatrick Basalt." In The Transantarctic Mountains, 373–414. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9390-5_12.

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3

Faure, Gunter, and Teresa M. Mensing. "Ferrar Group: Dolerite Sills and the Dufek Intrusion." In The Transantarctic Mountains, 415–69. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9390-5_13.

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4

Elliot, David H., Robert J. Fleck, and John F. Sutter. "Potassium-argon age determinations of Ferrar Group rocks, central Transantarctic Mountains." In Antarctic Research Series, 197–224. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ar036p0197.

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5

Cvijović, Djurdje, and Tibor K. Pogány. "Second Type Neumann Series Related to Nicholson’s and to Dixon–Ferrar Formula." In Trends in Mathematics, 67–84. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-35914-0_4.

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6

Barrett, P. J., David H. Elliot, and John F. Lindsay. "The Beacon Supergroup (Devonian-Triassic) and Ferrar Group (Jurrasic) in the Beardmore Glacier area, Antarctica." In Antarctic Research Series, 339–428. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ar036p0339.

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7

Elliot, D. H., T. H. Fleming, M. A. Haban, and M. A. Siders. "Petrology and Mineralogy of the Kirkpatrick Basalt and Ferrar Dolerite, Mesa Range Region, North Victoria Land, Antarctica." In Antarctic Research Series, 103–41. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1002/9781118668207.ch7.

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8

Elliot, D. H., T. H. Fleming, M. A. Haban, and M. A. Siders. "Petrology and mineralogy of the Kirkpatrick basalt and Ferrar Dolerite, Mesa Range region, north Victoria Land, Antarctica." In Antarctic Research Series, 103–41. Washington, D. C.: American Geophysical Union, 1995. http://dx.doi.org/10.1029/ar067p0103.

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9

Wild, Gerhard. "Ferrari, Paolo." In Kindlers Literatur Lexikon (KLL), 1. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-05728-0_3575-1.

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10

di Tella, Guido, and Carlos Rodríguez Braun. "Aldo Ferrer." In Argentina, 1946–83: The Economic Ministers Speak, 111–16. London: Palgrave Macmillan UK, 1990. http://dx.doi.org/10.1007/978-1-349-11756-7_9.

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Тези доповідей конференцій з теми "Ferrar"

1

Belyatsky, Boris, Nadezda Sushchevskaya, and German Leitchenkov. "The Karoo-Ferrar Igneous Province: geochemical peculiarity, genesis and evolution." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.5902.

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2

Al Suwaidi, Aisha, Calum Fox, Asma Al Naqbi, Andrea Ceriani, Alexander Dickson, Micha Ruhl, and Jessica H. Whiteside. "Close Encounters of the Ferrar Kind: Exploring the Impact of Volcanism on Early Jurassic Environments." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.41.

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3

Elliot, David, and Thomas H. Fleming. "THE FERRAR LARGE IGNEOUS PROVINCE, ANTARCTICA: FIELD AND GEOCHEMICAL EVIDENCE BEARING ON MODES OF EMPLACEMENT." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-280670.

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4

Ware, Bryant, Fred Jourdan, Massimo Chiaradia, and Oliver Nebel. "The Ferrar Continental Flood Basalt: A ~1.6 Ma Long Duration Evidenced by High-Precision 40Ar/39Ar Ages." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2811.

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5

Silenzi, Claudio. "Software Engineering in Ferrari F1." In 2015 IEEE/ACM 37th IEEE International Conference on Software Engineering (ICSE). IEEE, 2015. http://dx.doi.org/10.1109/icse.2015.22.

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6

Czigány, Ildikó. "Az operaszerző Vivaldi és Ferrara." In Új eredmények a színház- és drámatörténeti kutatásban (17-19. század). Eszterházy Károly Katolikus Egyetem Líceum Kiadó, 2022. http://dx.doi.org/10.17048/ujeredmenyekaszinhaz.2022.35.

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7

Kroushl, Dan, Amy Nesbit, Jin Kyoo Lee, Roy D. Marangoni, William W. Clark, Darrin Schwartz, and Pradeep P. Phulé. "Experimental Performance of a Magnetorheological Fluid Damper." In ASME 1997 Design Engineering Technical Conferences. American Society of Mechanical Engineers, 1997. http://dx.doi.org/10.1115/detc97/vib-3776.

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Abstract Magnetorheological (MR) and electrorheological (ER) fluids possess rheological or flow properties that can be controllably altered by the application of electric or magnetic fields, respectively. These fluids typically consist of dispersions of micrometer-sized dielectric or soft ferro (ferri) magnetic particles that become aligned in the presence of an external electric or electrical magnetic field, respectively. Such patterns in the material, which disappear when the field is removed, cause the material to resist mechanical deformation. This controllable property of the fluids allows them to be used in adaptive-passive actuators. This paper presents the results of a preliminary experimental investigation into the performance of the MR fluids in a linear vibration damper. A squeeze-flow MR fluid damper is used to suppress vibrations of a simply supported beam. Four different MR fluids are compared.

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8

Flouris, Ioannis, Vasiliki Manikaki, Nikos Giatrakos, Antonios Deligiannakis, Minos Garofalakis, Michael Mock, Sebastian Bothe, et al. "FERARI." In SIGMOD/PODS'16: International Conference on Management of Data. New York, NY, USA: ACM, 2016. http://dx.doi.org/10.1145/2882903.2899395.

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9

Hickl, Andrew, Patrick Wang, John Lehmann, and Sanda Harabagiu. "FERRET." In the COLING/ACL. Morristown, NJ, USA: Association for Computational Linguistics, 2006. http://dx.doi.org/10.3115/1225403.1225410.

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10

Lv, Qin, William Josephson, Zhe Wang, Moses Charikar, and Kai Li. "Ferret." In the 2006 EuroSys conference. New York, New York, USA: ACM Press, 2006. http://dx.doi.org/10.1145/1217935.1217966.

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Звіти організацій з теми "Ferrar"

1

Liebreich, Michael, Michal Grabka, and Piotr Pajda. Opportunities for Electric Ferries in Latin America. Edited by Marcelino Madrigal, Raúl Rodriguez Molina, and Juan Roberto Paredes. Inter-American Development Bank, February 2021. http://dx.doi.org/10.18235/0003026.

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This report provides an overview of the opportunity represented by the electrification of inland and coastal ferries in Latin America and the Caribbean. A review of electric ferry activity around the world and interviews with several project teams has been undertaken. In addition, a construction of an economic model the LATAM e-Ferry Model (LEFM) comparing the capital and operating costs of a typical mid-sized electric ferry to those of a conventional diesel-powered ferry was implemented. Finally, an assessment of five initial candidate routes for electrification and analysis of the electric ferry supply chain and identification of addressable market size in Latin America was determined.

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2

Smith, Timothy J., and Stephany Bryant. Ferret Workflow Anomaly Detection System. Fort Belvoir, VA: Defense Technical Information Center, February 2005. http://dx.doi.org/10.21236/ada430829.

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3

Lebron, Carmen A., and Patrick Evans. Bioavailable Ferric Iron (BAFelll) Assay. Fort Belvoir, VA: Defense Technical Information Center, February 2007. http://dx.doi.org/10.21236/ada607305.

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4

Lussiez, G., and L. Beckstead. Hydrolysis of ferric chloride in solution. Office of Scientific and Technical Information (OSTI), November 1996. http://dx.doi.org/10.2172/426965.

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5

Helfgott, Harald, and Michel Helfgott. A Modern Vision of the Work of Cardano and Ferrari on Quartics. Washington, DC: The MAA Mathematical Sciences Digital Library, July 2009. http://dx.doi.org/10.4169/loci003312.

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6

Wilmarth, W. R. Desilication from DWPF Recycle using Ferric Flocculation. Office of Scientific and Technical Information (OSTI), October 2002. http://dx.doi.org/10.2172/803617.

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7

Baumann, E. Colorimetric determination of ferrous-ferric ratio in glass. Office of Scientific and Technical Information (OSTI), February 1987. http://dx.doi.org/10.2172/7080410.

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8

Lanagan, M. T., I. Bloom, and T. D. Kaun. Lithium-ferrate-based cathodes for molten carbonate fuel cells. Office of Scientific and Technical Information (OSTI), December 1996. http://dx.doi.org/10.2172/460251.

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9

Hersman, L. E., and G. Sposito. Microbial acquisition of iron from ferric iron bearing minerals. Office of Scientific and Technical Information (OSTI), December 1998. http://dx.doi.org/10.2172/562540.

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10

Author, Not Given. Safety Evaluation Report on Tennessee Valley Authority: Browns Ferry Nuclear Performance Plan: Browns Ferry Unit 2 restart. Office of Scientific and Technical Information (OSTI), April 1989. http://dx.doi.org/10.2172/6343029.

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