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Artigos de revistas sobre o tema "Ferrar"

Autor: Grafiati

Publicado: 4 de junho de 2021

Última modificação: 31 de janeiro de 2023

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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 re

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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

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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 Mountain

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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 addition

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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-ri

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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 M

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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. Gro

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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 t

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11

Elliot, David H., and Thomas H. Fleming. "Chapter 2.1b Ferrar Large Igneous Province: petrology." Geological Society, London, Memoirs 55, no. 1 (2021): 93–119. http://dx.doi.org/10.1144/m55-2018-39.

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AbstractThe Lower Jurassic Ferrar Large Igneous Province consists predominantly of intrusive rocks, which crop out over a distance of 3500 km. In comparison, extrusive rocks are more restricted geographically. Geochemically, the province is divided into the Mount Fazio Chemical Type, forming more than 99% of the exposed province, and the Scarab Peak Chemical Type, which in the Ross Sea sector is restricted to the uppermost lava. The former exhibits a range of compositions (SiO2= 52–59%; MgO = 9.2–2.6%; Zr = 60–175 ppm; Sri= 0.7081–0.7138;εNd= −6.0 to −3.8), whereas the latter has a restricted

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12

Elliot, David H., James D. L. White, and Thomas H. Fleming. "Chapter 2.1a Ferrar Large Igneous Province: volcanology." Geological Society, London, Memoirs 55, no. 1 (2021): 75–91. http://dx.doi.org/10.1144/m55-2018-44.

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AbstractPreserved rocks in the Jurassic Ferrar Large Igneous Province consist mainly of intrusions, and extrusive rocks, the topic of this chapter, comprise the remaining small component. They crop out in a limited number of areas in the Transantarctic Mountains and southeastern Australia. They consist of thick sequences of lavas and sporadic occurrences of volcaniclastic rocks. The latter occur mainly beneath the lavas and represent the initial eruptive activity, but also are present within the lava sequence. The majority are basaltic phreatomagmatic deposits and in at least two locations for

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13

BARRETT, P. J., and M. J. HAMBREY. "Plio-Pleistocene sedimentation in Ferrar Fiord, Antarctica." Sedimentology 39, no. 1 (February 1992): 109–23. http://dx.doi.org/10.1111/j.1365-3091.1992.tb01025.x.

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14

Ransome, David R. "The Parliamentary Papers of Nicholas Ferrar, 1624." Camden Fifth Series 7 (July 1996): 3–104. http://dx.doi.org/10.1017/s0960116300000361.

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Nicholas Ferrar's fame in the twentieth century rests largely upon religious foundations – as a saint of the Church of England and as one of the moving spirits at Little Gidding – but in fact his historical importance is more than merely religious, and indeed religion did not dominate his life before 1625. Born in London in February 1593, the youngest but one of a family of six, Nicholas was named for his father, a highly successful Merchant Adventurer who was also a Master of the Skinners Company. Small, fair-haired, precocious and frail, Nicholas was always his mother's favourite, and it was

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15

Nelson, Demian A., John M. Cottle, and Blair Schoene. "Butcher Ridge igneous complex: A glassy layered silicic magma distribution center in the Ferrar large igneous province, Antarctica." GSA Bulletin 132, no. 5-6 (October 26, 2019): 1201–16. http://dx.doi.org/10.1130/b35340.1.

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Abstract The Butcher Ridge igneous complex, Antarctica, is an ∼6000 km3 hypabyssal silicic intrusion containing rhythmically layered glassy rocks. Baddeleyite U-Pb geochronologic analysis on a sample of the Butcher Ridge igneous complex yielded an age of ca. 182.4 Ma, which confirms that it was emplaced synchronously with the Ferrar large igneous province. Rocks of the Butcher Ridge igneous complex vary from basaltic andesite to rhyolite, and so the inferred volume of the Butcher Ridge igneous complex makes it the most voluminous silicic component of the Ferrar large igneous province. Major-el

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16

Ransome, David R. "John Ferrar: a half-hidden propagandist for Virginia." Seventeenth Century 35, no. 5 (November 18, 2019): 611–24. http://dx.doi.org/10.1080/0268117x.2019.1688553.

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17

Zavala, Karina, Alison M. Leitch, and George W. Fisher. "Silicic Segregations of the Ferrar Dolerite Sills, Antarctica." Journal of Petrology 52, no. 10 (September 21, 2011): 1927–64. http://dx.doi.org/10.1093/petrology/egr035.

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18

Leat, Philip T. "On the long-distance transport of Ferrar magmas." Geological Society, London, Special Publications 302, no. 1 (2008): 45–61. http://dx.doi.org/10.1144/sp302.4.

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19

BROOK, MARTIN S., and SUSANNA FERRAR. "HARTLEY TRAVERS FERRAR (1879–1932) AND HIS GEOLOGICAL LEGACY IN ANTARCTICA, EGYPT AND NEW ZEALAND." Earth Sciences History 38, no. 1 (April 1, 2019): 43–58. http://dx.doi.org/10.17704/1944-6178-38.1.43.

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ABSTRACT Hartley Travers Ferrar was the geologist on Scott's first expedition to the Antarctic (the ‘Discovery’ Expedition) in 1901–1904. Ferrar undertook the first geological surveys in the Transantarctic Mountains, which he mapped to 83°S, and made some discoveries of major scientific importance, such as fossil leaves, later identified as Glossopteris indica. He then worked in Egypt, Palestine and New Zealand, and was Acting Director of the New Zealand Geological Survey when he died suddenly in 1932. Little has been acknowledged about Ferrar's other contributions to geology, which were vast,

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20

Airoldi, Giulia, James D. Muirhead, James D. L. White, and Julie Rowland. "Emplacement of magma at shallow depth: insights from field relationships at Allan Hills, south Victoria Land, East Antarctica." Antarctic Science 23, no. 3 (February 1, 2011): 281–96. http://dx.doi.org/10.1017/s0954102011000095.

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AbstractAllan Hills nunatak, south Victoria Land, Antarctica, exposes an exceptional example of a shallow depth (< 500 m) intrusive complex formed during the evolution of the Ferrar large igneous province (LIP). Dyke distribution, geometries and relationships allow reconstruction of its history and mechanics of intrusion. Sills interconnect across host sedimentary layers, and a swarm of parallel inclined dolerite sheets is intersected by a radiating dyke-array associated with remnants of a phreatomagmatic vent, where the dolerite is locally quenched and mixed to form peperite. Intrusion geo

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21

Riley, Teal R., and Kim B. Knight. "Age of Pre-Break-Up Gondwana Magmatism." Antarctic Science 13, no. 2 (June 2001): 99–110. http://dx.doi.org/10.1017/s0954102001000177.

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Extensive outpourings of basalt, and to a lesser extent rhyolite, are closely associated with continental break-up and plume–lithosphere interactions. The Gondwana supercontinent began to fragment during Early–Middle Jurassic times and was associated with the eruption of over three million km3 of dominantly basaltic magma. This intense magmatic episode is recorded in volcanic rocks of the Karoo (Africa), Ferrar (Antarctica) and Chon Aike (South America). K–Ar and Rb–Sr whole rock geochronology has consistently failed to produce reliable ages for these volcanic rocks, but in the last four years

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22

Unverfärth, Jan, Thomas Mörs, and Benjamin Bomfleur. "Palynological evidence supporting widespread synchronicity of Early Jurassic silicic volcanism throughout the Transantarctic Basin." Antarctic Science 32, no. 5 (July 7, 2020): 396–97. http://dx.doi.org/10.1017/s0954102020000346.

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Throughout the Transantarctic Mountains, Early Jurassic silicic magmatism preceding the emplacement of the Ferrar flood-basalt province (Heimann et al. 1994) is documented by the increasing input of silicic ash into otherwise epiclastic, fluviolacustrine deposits of the Beacon Supergroup (see Elliot et al. 2017). Vertebrate biostratigraphy and radiometric analyses indicate a Sinemurian to Pliensbachian age span for silicic volcaniclastic deposits in the central Transantarctic Mountains (CTMs) (Elliot et al. 2017). For northern Victoria Land (NVL), radiometric geochronology and palynostratigrap

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23

Fleming, T. H., A. Heimann, K. A. Foland, and D. H. Elliot. "40Ar/39Ar geochronology of Ferrar Dolerite sills from the Transantarctic Mountains, Antarctica: Implications for the age and origin of the Ferrar magmatic province." Geological Society of America Bulletin 109, no. 5 (May 1997): 533–46. http://dx.doi.org/10.1130/0016-7606(1997)109<0533:aagofd>2.3.co;2.

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24

Brotzu, Pietro, Giuseppe Capaldi, Lucia Civetta, Giovanni Orsi, Gabriella Gallo, and Leone Melluso. "Geochronology and geochemistry of Ferrar rocks from North Victoria Land, Antarctica." European Journal of Mineralogy 4, no. 3 (June 11, 1992): 605–18. http://dx.doi.org/10.1127/ejm/4/3/0605.

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25

Jepp, Mary. "Joyce Ransome, The Web of Friendship: Nicholas Ferrar and Little Gidding." Theology 116, no. 5 (August 2, 2013): 389–90. http://dx.doi.org/10.1177/0040571x13493974v.

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26

Joyce Ransome. "George Herbert, Nicholas Ferrar, and the "Pious Works" of Little Gidding." George Herbert Journal 31, no. 1 (2009): 1–19. http://dx.doi.org/10.1353/ghj.0.0008.

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27

Pour, Amin Beiranvand, Milad Sekandari, Omeid Rahmani, Laura Crispini, Andreas Läufer, Yongcheol Park, Jong Kuk Hong, et al. "Identification of Phyllosilicates in the Antarctic Environment Using ASTER Satellite Data: Case Study from the Mesa Range, Campbell and Priestley Glaciers, Northern Victoria Land." Remote Sensing 13, no. 1 (December 24, 2020): 38. http://dx.doi.org/10.3390/rs13010038.

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In Antarctica, spectral mapping of altered minerals is very challenging due to the remoteness and inaccessibility of poorly exposed outcrops. This investigation evaluates the capability of Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) satellite remote sensing imagery for mapping and discrimination of phyllosilicate mineral groups in the Antarctic environment of northern Victoria Land. The Mixture-Tuned Matched-Filtering (MTMF) and Constrained Energy Minimization (CEM) algorithms were used to detect the sub-pixel abundance of Al-rich, Fe3+-rich, Fe2+-rich and Mg-rich ph

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28

Latifa, Rena, Melanie Nyhof, Muthia Rahmah, and Abdul Rahman Saleh. "POLITICAL TOLERANCE IN INDONESIAN-MUSLIM." Mimbar Agama Budaya 38, no. 2 (March 11, 2022): 106–16. http://dx.doi.org/10.15408/mimbar.v38i2.25145.

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Abstract In the field of political behavior, tolerance is a crucial element to keep harmonious relationship. Studies should be able to measure a valid construct of tolerance in an effort to understand it further. Ferrar (1979) conducted a research focusing on the concept of political tolerance and theorized political tolerance to have three dimensions, namely flexible, approval, and allowance. This study aims to construct a political tolerance scale based on Ferrar’s concept and dimensions. Confirmatory Factor Analysis (CFA) is employed to test the construct validity and dimensionality of the

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29

Whyte, Bob. "The Web of Friendship: Nicholas Ferrar and Little Gidding - By Joyce Ransome." Reviews in Religion & Theology 19, no. 3 (July 2012): 362–65. http://dx.doi.org/10.1111/j.1467-9418.2012.01075.x.

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RILEY, T. R., M. L. CURTIS, P. T. LEAT, M. K. WATKEYS, R. A. DUNCAN, I. L. MILLAR, and W. H. OWENS. "Overlap of Karoo and Ferrar Magma Types in KwaZulu-Natal, South Africa." Journal of Petrology 47, no. 3 (December 8, 2005): 541–66. http://dx.doi.org/10.1093/petrology/egi085.

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31

Badir, Patricia. "Fixing Affections: Nicholas and John Ferrar and the Books of Little Gidding." English Literary Renaissance 49, no. 3 (September 2019): 390–422. http://dx.doi.org/10.1086/704510.

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32

KROHNE, NICOLE, FRANK LISKER, GEORG KLEINSCHMIDT, ANDREAS KLÜGEL, ANDREAS LÄUFER, SOLVEIG ESTRADA, and CORNELIA SPIEGEL. "The Shackleton Range (East Antarctica): an alien block at the rim of Gondwana?" Geological Magazine 155, no. 4 (December 12, 2016): 841–64. http://dx.doi.org/10.1017/s0016756816001011.

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AbstractThe Shackleton Range is a truncated Pan-African Orogen situated at the Weddell Sea margin of East Antarctica. It almost exclusively consists of basement rocks exposed at an elevated, escarpment-bound palaeosurface and is covered locally by patchy remnants of Ordovician, Permian and, controversially, Jurassic terrestrial deposits. This inventory does not match the geological record of any other place in Antarctica. Here we reconstruct the Phanerozoic evolution of the Shackleton Range by means of a multi-disciplinary approach combining petrological, geochemical and geochronological data

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33

Mortimer, N., D. Parkinson, J. I. Raine, C. J. Adams, I. J. Graham, P. J. Oliver, and K. Palmer. "Ferrar magmatic province rocks discovered in New Zealand: Implications for Mesozoic Gondwana geology." Geology 23, no. 2 (1995): 185. http://dx.doi.org/10.1130/0091-7613(1995)023<0185:fmprdi>2.3.co;2.

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Encarnación, John, Thomas H. Fleming, David H. Elliot, and Hugh V. Eales. "Synchronous emplacement of Ferrar and Karoo dolerites and the early breakup of Gondwana." Geology 24, no. 6 (1996): 535. http://dx.doi.org/10.1130/0091-7613(1996)024<0535:seofak>2.3.co;2.

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35

Ribecai, C. "Early Jurassic miospores from Ferrar Group of Carapace Nunatak, South Victoria Land, Antarctica." Review of Palaeobotany and Palynology 144, no. 1-2 (April 2007): 3–12. http://dx.doi.org/10.1016/j.revpalbo.2005.09.005.

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Elliot, David H., Thomas H. Fleming, Philip R. Kyle, and Kenneth A. Foland. "Long-distance transport of magmas in the Jurassic Ferrar Large Igneous Province, Antarctica." Earth and Planetary Science Letters 167, no. 1-2 (March 1999): 89–104. http://dx.doi.org/10.1016/s0012-821x(99)00023-0.

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Elliot, D. H., and T. H. Fleming. "Physical volcanology and geological relationships of the Jurassic Ferrar Large Igneous Province, Antarctica." Journal of Volcanology and Geothermal Research 172, no. 1-2 (May 2008): 20–37. http://dx.doi.org/10.1016/j.jvolgeores.2006.02.016.

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Elliot, David H., and Thomas H. Fleming. "Occurrence and Dispersal of Magmas in the Jurassic Ferrar Large Igneous Province, Antarctica." Gondwana Research 7, no. 1 (January 2004): 223–37. http://dx.doi.org/10.1016/s1342-937x(05)70322-1.

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Passchier, Sandra, Anja L. L. M. Verbers, Frederik M. Van Der Wateren, and Frans J. M. Vermeulen. "Provenance, geochemistry and grain-sizes of glacigene sediments, including the Sirius Group, and Late Genozoic Glaciol history of the southern Prince Albert Mountains, Victoria Land, Antarctica." Annals of Glaciology 27 (1998): 290–96. http://dx.doi.org/10.3189/1998aog27-1-290-296.

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The southern Prince Albert Mountains, between David and Mawson Glaciers (75°30' to 76°S) in Victoria Land, Antarctica, comprise a series of nunataks with elevations ranging from 800m near the coast to 2300 m ~130 km inland. Geochemical and grain-size analyses of tills from these nunataks reveal three major groups of deposits: (1) coarse to medium sandy tills, found on Glaciolly streamlined summit plateaus of Kirk-pat rick Basalt above 2000 ma.s.l.., with geochemical compositions very similar to those of the underlying jurassic Kirkpatrick Basalt; (2) bimodal silty and sanely tills of the Siriu

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40

Laurent, Jane K., and Trevor Dean. "Land and Power in Late Medieval Ferrar: The Rule of the Este, 1350-1450." American Historical Review 94, no. 3 (June 1989): 749. http://dx.doi.org/10.2307/1873812.

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41

Lanza, Roberto, and Elena Zanella. "Palaeomagnetism of the Ferrar dolerite in the northern Prince Albert Mountains (Victoria Land, Antarctica)." Geophysical Journal International 114, no. 3 (September 1993): 501–11. http://dx.doi.org/10.1111/j.1365-246x.1993.tb06983.x.

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Riley, Teal R., Philip T. Leat, Bryan C. Storey, Ian J. Parkinson, and Ian L. Millar. "Ultramafic lamprophyres of the Ferrar large igneous province: evidence for a HIMU mantle component." Lithos 66, no. 1-2 (January 2003): 63–76. http://dx.doi.org/10.1016/s0024-4937(02)00213-x.

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Staiger, J. W., D. R. Marchant, J. M. Schaefer, P. Oberholzer, J. V. Johnson, A. R. Lewis, and K. M. Swanger. "Plio-Pleistocene history of Ferrar Glacier, Antarctica: Implications for climate and ice sheet stability." Earth and Planetary Science Letters 243, no. 3-4 (March 2006): 489–503. http://dx.doi.org/10.1016/j.epsl.2006.01.037.

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