Статті в журналах: "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.

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.

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.

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.

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.

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.

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.

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.

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.

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 composition (SiO2=c.58%; MgO =c.2.3%; Zr =c.230 ppm; Sri= 0.7090–0.7097;εNd= −4.4 to −4.1). Both chemical types are characterized by enriched initial isotope compositions of neodymium and strontium, low abundances of high field strength elements, and crust-like trace element patterns. The most basic rocks, olivine-bearing dolerites, indicate that these geochemical characteristics were inherited from a mantle source modified by subduction processes, possibly the incorporation of sediment. In one model, magmas were derived from a linear source having multiple sites of generation each of which evolved to yield, in sum, the province-wide coherent geochemistry. The preferred interpretation is that the remarkably coherent geochemistry and short duration of emplacement demonstrate derivation from a single source inferred to have been located in the proto-Weddell Sea region. The spatial variation in geochemical characteristics of the lavas suggests distinct magma batches erupted at the surface, whereas no clear geographical pattern is evident for intrusive rocks.

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 form immense phreatocauldrons filled with structureless tuff breccias and lapilli tuffs with thicknesses of as much as 400 m. Stratified sequences of tuff breccias, lapilli tuffs and tuffs are up to 200 m thick. Thin tuff beds are sparsely distributed in the lava sequences. Lava successions are mainly 400–500 m thick, and comprise individual lavas ranging from 1 to 230 m thick, although most are in the range of 10–100 m. Well-defined colonnade and entablature are seldom displayed. Lava sequences were confined topographically and locally ponded. Water played a prominent role in eruptive activity, as exhibited by phreatomagmatism, hyaloclastites, pillow lava and quenching of lavas. Vents for lavas have yet to be identified.

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 she who largely influenced his development. At the age of seventeen he was a Fellow of Clare College, Cambridge, but soon after his twentieth birthday he left Cambridge for the sake of his health, spending the years 1613–17 on the continent, chiefly at Padua, where he studied medicine. On his return to England he did not resume his fellowship at Clare, but remained in London with his parents, attending to his now elderly father's business affairs which included membership of the East India and Virginia Companies – and acting as his executor upon his death in 1620.

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-element, trace-element, and isotopic data combined with binary mixing, assimilation-fractional crystallization (AFC), and energy-constrained AFC models are consistent with formation of Butcher Ridge igneous complex silicic rocks by contamination of mafic Ferrar parental magma(s) with local Paleozoic plutonic basement rocks. Field and petrographic observations and evidence for alkali ion exchange suggest that the kilometer-long, meter-thick enigmatic rhythmic layering formed as a result of secondary hydration and devitrification of volcanic glass along parallel fracture networks. The regularity and scale of fracturing/layering imply a thermally driven process that occurred during shallow emplacement and supercooling of the intrusion in the upper crust. We suggest that layering observed in the Butcher Ridge igneous complex is analogous to that reported from terrestrial and Martian cryptodomes, and therefore it is an ideal locality at which to study layering processes in igneous bodies.

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, and included pioneering work on irrigation and hydrogeology in Egypt, as well as a series of geological mapping campaigns in New Zealand. The latter extended to systematic soil surveys in New Zealand, in particular in Central Otago, where soil types and their properties were characterized in the field and laboratory. This paper outlines some of Ferrar's key contributions to New Zealand geoscience, as well as some of his notable overseas achievements.

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 geometries, and lack of dominant rift-related structures in the country rock indicate that magma overpressure, local stresses between mutually interacting dykes and vertical variations of host rock mechanical properties controlled the intrusive process throughout the thick and otherwise undeformed pile of sedimentary rocks (Victoria Group). Dolerite sills connected to one another by inclined sheets are inferred to record the preferred mode of propagation for magma-carrying cracks that represent the shallow portions of the Ferrar LIP plumbing system.

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, the wider application of single grain 40Ar/39Ar and/or U–Pb geochronology has produced more robust and precise dating of the magmatism. This paper reviews the recent advances in high precision geochronology and provides a full recalibrated 40Ar/39Ar dataset. Application of these methods across the majority of the volcanic provinces indicates that approximately 80% of the volcanic rocks were erupted within a short, 3–4 Myr period at c. 182 Ma. This burst of magmatism occurred in the Karoo province at c. 183 Ma and in the Ferrar provinces at c. 180 Ma, and was dominated by mafic volcanism. This peak in volcanism is coincident with a second order mass extinction event at the end of the Pliensbachian when c. 5% of marine families were wiped out coinciding with widespread oceanic anoxia in the early Toarcian. A prolonged period of silicic volcanism occurred along the proto-Pacific margin, prior to, and during the main phase of break-up. Silicic volcanism was initially coincident with the plume related Karoo-Ferrar provinces, but continued over c. 40 Myr, associated with lithospheric extension and subduction along the proto-Pacific continental margin.

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 palynostratigraphy revealed that explosive silicic volcanism began with minor pulses during the early Sinemurian (c. 195 Ma) and reached a peak phase beginning in the middle Pliensbachian (c. 187 Ma) (Bomfleur et al. 2014). A basin-wide correlation of these widely separated age frameworks has so far been hampered by the scarcity of data on coeval deposits in southern Victoria Land (SVL). Here, we present new palynostratigraphic data from mixed epiclastic–volcaniclastic deposits in the Prince Albert Mountains that provide supporting evidence for the widespread synchronicity of silicic volcanic episodes preceding Ferrar magmatism.

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 phyllosilicates using the visible and near-infrared (VNIR), short-wave infrared (SWIR) and thermal-infrared (TIR) bands of ASTER. Results indicate that Al-rich phyllosilicates are strongly detected in the exposed outcrops of the Granite Harbour granitoids, Wilson Metamorphic Complex and the Beacon Supergroup. The presence of the smectite mineral group derived from the Jurassic basaltic rocks (Ferrar Dolerite and Kirkpatrick Basalts) by weathering and decomposition processes implicates Fe3+-rich and Fe2+-rich phyllosilicates. Biotite (Fe2+-rich phyllosilicate) is detected associated with the Granite Harbour granitoids, Wilson Metamorphic Complex and Melbourne Volcanics. Mg-rich phyllosilicates are mostly mapped in the scree, glacial drift, moraine and crevasse fields derived from weathering and decomposition of the Kirkpatrick Basalt and Ferrar Dolerite. Chlorite (Mg-rich phyllosilicate) was generally mapped in the exposures of Granite Harbour granodiorite and granite and partially identified in the Ferrar Dolerite, the Kirkpatrick Basalt, the Priestley Formation and Priestley Schist and the scree, glacial drift and moraine. Statistical results indicate that Al-rich phyllosilicates class pixels are strongly discriminated, while the pixels attributed to Fe3+-rich class, Fe2+-rich and Mg-rich phyllosilicates classes contain some spectral mixing due to their subtle spectral differences in the VNIR+SWIR bands of ASTER. Results derived from TIR bands of ASTER show that a high level of confusion is associated with mafic phyllosilicates pixels (Fe3+-rich, Fe2+-rich and Mg-rich classes), whereas felsic phyllosilicates (Al-rich class) pixels are well mapped. Ground truth with detailed geological data, petrographic study and X-ray diffraction (XRD) analysis verified the remote sensing results. Consequently, ASTER image-map of phyllosilicate minerals is generated for the Mesa Range, Campbell and Priestley Glaciers, northern Victoria Land of Antarctica.

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 Political Tolerance Scale. Participants were 300 Indonesian-Muslims. The results support the Political Tolerance Scale as a unidimensional scale consists of flexible, approval, and allowance dimensions. However, the limitation of the samples’ characteristic suggests future studies to conduct further researches on samples with different characteristics.AbstractDalam ilmu perilaku politik, toleransi adalah merupakan elemen penting untuk menjaga keharmonisan hubungan. Kajian saintifik harus mampu mengukur konstruk toleransi yang valid dalam upaya memahaminya lebih jauh. Ferrar (1979) melakukan penelitian yang berfokus pada konsep toleransi politik dimana toleransi politik diteorikan memiliki tiga dimensi, yaitu fleksibel, persetujuan, dan pengakomodiran. Penelitian ini bertujuan untuk mengkonstruksi alat ukur toleransi politik. Analisis faktor konfirmatori (CFA) digunakan untuk menguji validitas konstruk dan dimensi Skala Toleransi. Pesertanya adalah 300 orang Muslim Indonesia. Hasil yang didapat mendukung Skala Toleransi Politik sebagai skala unidimensional yang terdiri dari dimensi fleksibel, persetujuan, dan pengakomodiran. Namun, keterbatasan karakteristik sampel mendorong studi selanjutnya untuk melakukan penelitian lebih lanjut pada karakteristik sampel yang berbeda.

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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30

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 with thermal history models of zircon and apatite fission track (ZFT, AFT) and (U–Th–Sm)/He (AHe) data. Petrographic, geochemical and 40Ar/39Ar analyses of a sedimentary cover sequence identify volcaniclastic rocks related to the Ferrar/Karoo magmatic event. Thermal history modelling of ZFT ages of 160–215 Ma, AFT ages of 124–225 Ma, AHe ages of 95–169 Ma and kinematic proxies in combination with geological information indicates a complex thermal history comprising at least three cooling episodes interrupted by reheating pulses. Thermal history refers to inversion of part of the Carboniferous–Triassic Transantarctic Basin prior to the 180 Ma Ferrar/Karoo Event and formation of an up to 3.4 km deep extensional Jurassic – Early Cretaceous basin due to Weddell Sea rifting. Basin depth was diminished by regional middle Cretaceous stress field changes. Final basin inversion and surface uplift were likely triggered by far-field tectonics and climatic influence. This history represents a typical example for the transition from an active to passive margin setting along the outer rim of Gondwana.

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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34

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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36

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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37

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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38

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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39

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 Sirius Group with Ferrar/Beacon-dominated geochemical compositions, at elevations of 1300-1600 m a.s.l. on striated summit plateaus and high-elevation terraces; (3) fine-grained tills with high SiO2 contents from ice-cored moraines at the lee sides of large nunataks. The geochemical composition of sandy tills from the highest summit plateaus suggests that valleys had not yet cut through the Kirkpatrick Basalt and into Beacon and Ferrar rocks at the time of deposition. These tills represent a phase of temperate glaciation prior to deposition of diatom-bearing Sirius Group tills. The latter were deposited after a first phase of landscape dissection as inferred from geochemical data. The fine-grained ice-cored moraines are late-Pleistocene basal tills. The presence of pre-Pliocene Glacial deposits on high mountain summits in the Prince Albert Mountains has implications for the interpretation of high-elevation Sirius Group sediments in other areas of the Transantarctic Mountains. It is possible that the “Sirius debate” has its origin in interpretations of both thin, barren pre-Pliocene deposits on high mountain summits and thick sequences of diatom-bearing deposits in valleys elsewhere in the Transantarctic Mountains. Both types of deposits are associated with the Sirius Group, but they belong to separate Glacial episodes.

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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42

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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43

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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44

Farina, Roberto. "Roberto Farina, DDS, MSC, PHD, Research Centre for the Study of Periodontal & Peri-Implant Diseases, Department of Periodontology, School of Dentistry, University of Ferrar, Ferrara, Italy." Endodontic Topics 25, no. 1 (September 2011): 99. http://dx.doi.org/10.1111/etp.12016_1.

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45

Pálfy, József, and Paul L. Smith. "Synchrony between Early Jurassic extinction, oceanic anoxic event, and the Karoo-Ferrar flood basalt volcanism." Geology 28, no. 8 (August 2000): 747–50. http://dx.doi.org/10.1130/0091-7613(2000)028<0747:sbejeo>2.3.co;2.

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46

Pálfy, József, and Paul L. Smith. "Synchrony between Early Jurassic extinction, oceanic anoxic event, and the Karoo-Ferrar flood basalt volcanism." Geology 28, no. 8 (2000): 747. http://dx.doi.org/10.1130/0091-7613(2000)28<747:sbejeo>2.0.co;2.

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47

Irving-Stonebraker, Sarah. "From Little Gidding to Virginia: the seventeenth century Ferrar family in the Atlantic colonial context." Seventeenth Century 33, no. 2 (August 2017): 183–94. http://dx.doi.org/10.1080/0268117x.2017.1336473.

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48

Mukasa, S. B., G. Ravizza, J. Bédard, T. Fleming, A. Boudreau, B. D. Marsh, and S. H. Choi. "PGE abundance patterns for the basement sill and Dufek intrusion, Ferrar large igneous province, Antarctica." Geochimica et Cosmochimica Acta 70, no. 18 (August 2006): A434. http://dx.doi.org/10.1016/j.gca.2006.06.871.

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49

Gröcke, Darren R., Susan M. Rimmer, Lois E. Yoksoulian, Bruce Cairncross, Harilaos Tsikos, and Jeroen van Hunen. "No evidence for thermogenic methane release in coal from the Karoo-Ferrar large igneous province." Earth and Planetary Science Letters 277, no. 1-2 (January 2009): 204–12. http://dx.doi.org/10.1016/j.epsl.2008.10.022.

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50

Elliot, D. H., and T. H. Fleming. "Weddell triple junction: The principal focus of Ferrar and Karoo magmatism during initial breakup of Gondwana." Geology 28, no. 6 (June 2000): 539–42. http://dx.doi.org/10.1130/0091-7613(2000)028<0539:wtjtpf>2.3.co;2.

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