930 resultados para Hodges, James Gregory, 1828-1863.
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James Francis Crocker. A short biography... .--My personal experiences in taking up arms and in the battle of Malvern Hill.--Gettysburg - Pickett's charge.--Prison reminiscences.--Life and character of Colonel James Gregory Hodges.--Our Confederate dead.--Citizenship - its rights and duties.
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La tesis indaga las relaciones entre prensa periódica y cultura literaria que durante la primera mitad del siglo XIX, tanto en Chile como en el Río de la Plata, viabilizaron los procesos de formación de un imaginario y un público lector nacionales, y contribuyeron a la creación -temporal y territorialmente diferenciada- de un canon literario y estético. La tesis analiza las modalidades de construcción pública de las culturas literarias chilena y argentina ya consolidada la independencia, y especialmente los modos en que la prensa periódica incidió en los programas literarios de las respectivas élites letradas. Para ello, se estudia un amplio corpus de publicaciones periódicas que se extiende desde El Recopilador (1836) hasta El Talismán o El Corsario (1840) en el Río de la Plata, y desde El Semanario de Santiago (1842) hasta El Correo Literario (1858) o La Semana (1859) en Chile. Los límites de la periodización propuesta acompañan el itinerario de esas publicaciones de la primera mitad del siglo, y coinciden con el ingreso y la difusión de las ideas románticas que incentivaron la preocupación letrada por definir la problemática relación entre cultura y nacionalidad. El enfoque comparativo, por su parte, contempla particularidades, así como simetrías y divergencias, en la formación de imaginarios y tradiciones culturales de ambos territorios.
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La tesis indaga las relaciones entre prensa periódica y cultura literaria que durante la primera mitad del siglo XIX, tanto en Chile como en el Río de la Plata, viabilizaron los procesos de formación de un imaginario y un público lector nacionales, y contribuyeron a la creación -temporal y territorialmente diferenciada- de un canon literario y estético. La tesis analiza las modalidades de construcción pública de las culturas literarias chilena y argentina ya consolidada la independencia, y especialmente los modos en que la prensa periódica incidió en los programas literarios de las respectivas élites letradas. Para ello, se estudia un amplio corpus de publicaciones periódicas que se extiende desde El Recopilador (1836) hasta El Talismán o El Corsario (1840) en el Río de la Plata, y desde El Semanario de Santiago (1842) hasta El Correo Literario (1858) o La Semana (1859) en Chile. Los límites de la periodización propuesta acompañan el itinerario de esas publicaciones de la primera mitad del siglo, y coinciden con el ingreso y la difusión de las ideas románticas que incentivaron la preocupación letrada por definir la problemática relación entre cultura y nacionalidad. El enfoque comparativo, por su parte, contempla particularidades, así como simetrías y divergencias, en la formación de imaginarios y tradiciones culturales de ambos territorios.
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La tesis indaga las relaciones entre prensa periódica y cultura literaria que durante la primera mitad del siglo XIX, tanto en Chile como en el Río de la Plata, viabilizaron los procesos de formación de un imaginario y un público lector nacionales, y contribuyeron a la creación -temporal y territorialmente diferenciada- de un canon literario y estético. La tesis analiza las modalidades de construcción pública de las culturas literarias chilena y argentina ya consolidada la independencia, y especialmente los modos en que la prensa periódica incidió en los programas literarios de las respectivas élites letradas. Para ello, se estudia un amplio corpus de publicaciones periódicas que se extiende desde El Recopilador (1836) hasta El Talismán o El Corsario (1840) en el Río de la Plata, y desde El Semanario de Santiago (1842) hasta El Correo Literario (1858) o La Semana (1859) en Chile. Los límites de la periodización propuesta acompañan el itinerario de esas publicaciones de la primera mitad del siglo, y coinciden con el ingreso y la difusión de las ideas románticas que incentivaron la preocupación letrada por definir la problemática relación entre cultura y nacionalidad. El enfoque comparativo, por su parte, contempla particularidades, así como simetrías y divergencias, en la formación de imaginarios y tradiciones culturales de ambos territorios.
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Dr James George Beaney (1828-1891) was a flamboyant and controversial Melbourne surgeon and paediatrician. He was the first in Australia, in 1859, to publish a medical textbook; and the first, in 1873, to publish a paediatric text, Children: their treatment in health and disease. An analysis of four of his published works relating to paediatrics and paediatric surgery establishes his place as a true pioneer in the chronology of children's medicine and welfare in his adopted land. He undertook heroic yet conservative surgery on children, was the first to write in detail about paediatric anaesthesia, and was the pioneer of family planning in Australia. In Children: their treatment in health and disease, he described in detail the supreme importance of breastfeeding, detailed clear practical concepts for the weaning of infants and discussed the diagnosis and management of diseases of the mouth, ears, eyes and teeth of infants. Beaney was shunned by much of the established medical profession because of his self-promoting flamboyance and his egotism. However, an audit of surviving archives and of his published works affords him a place as another, hitherto unacknowledged true pioneer of Australian paediatrics.
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Each vol. has special t.p. added.
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Includes bibliographical references.
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Text in double columns.
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Amer. Art. Assoc., catalog, 4-6 Feb. 1919 (Townsend sale) no. 560, describes as the 1st ed. with these ill.; only ed. cited in BM 238:106 and NUC pre-1956 591:538.
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Includes bibliographical references and index.
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Mode of access: Internet.
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The steeply dipping, isoclinally folded early Precambrian (Archean) Berry Creek Metavolcanic Complex comprises primary to resedimented pyroclastic, epiclastic and autoclastic deposits. Tephra erupted from central volcanic edifices was dumped by mass flow mechanisms into peripheral volcanosedimentary depressions. Sedimentation has been essentially contemporaneous with eruption and transport of tephra. The monolithic to heterolithic tuffaceous horizons are interpreted as subaerial to subaqueous pumice and ash flows, secondary debris flows, lahars, slump deposits and turbidites. Monolithic debris flows, derived from crumble breccia and dcme talus, formed during downslope collapse and subsequent gravity flowage. Heterolithic tuff, lahars and lava flow morphologies suggest at least temporary emergence of the edifice. Local collapse may have accompanied pyroclastic volcanism. The tephra, produced by hydromagmatic to magmatic eruptions, were rapidly transported, by primary and secondary mechanisms, to a shallow littoral to deep water subaqueous fan developed upon the subjacent mafic metavolcanic platform. Deposition resulted from traction, traction carpet, and suspension sedimentation from laminar to turbulent flows. Facies mapping revealed proximal (channel to overbank) to distal facies epiclastics (greywackes, argillite) intercalated with proximal vent to medial fan facies crystal rich ash flows, debris flows, bedded tuff and shallow water to deep water lava flows. Framework and matrix support debris flows exhibit a variety of subaqueous sedimentary structures, e.g., coarse tail grading, double grading, inverse to normal grading, graded stratified pebbly horizons, erosional channels. Pelitic to psammitic AE turbidites also contain primary stru~tures, e.g., flames, load casts, dewatering pipes. Despite low to intermediate pressure greenschist to amphibolite grade metamorphism and variably penetrative deformation, relicts of pumice fragments and shards were recognized as recrystallized quartzofeldspathic pseudomorphs. The mafic to felsic metavolcanics and metasediments contain blasts of hornblende, actinolite, garnet, pistacitic epidote, staurolite, albitic plagioclase, and rarely andalusite and cordierite. The mafic metavolcanics (Adams River Bay, Black River, Kenu Lake, Lobstick Bay, Snake Bay) display _holeiitic trends with komatiitic affinities. Chemical variations are consistent with high level fractionation of olivine, plagioclase, amphibole, and later magnetite from a parental komatiite. The intermediate to felsic (64-74% Si02) metavolcanics generally exhibit calc-alkaline trends. The compositional discontinuity, defined by major and trace element diversity, can be explained by a mechanism involving two different magma sources. Application of fractionation series models are inconsistent with the observed data. The tholeiitic basalts and basaltic andesites are probably derived by low pressure fractionation of a depleted (high degree of partial melting) mantle source. The depleted (low Y, Zr) calc-alkaline metavolcanics may be produced by partial melting of a geochemically evolved source, e.g., tonalitetrondhjemite, garnet amphibolite or hydrous basalt.
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Objective: To measure 2-week postoperative sensitivity in Class II composite restorations placed with a self-etching adhesive (Clearfil SE Bond) or a total-etch adhesive (Prime&Bond NT) with or without a flowable composite as cervical increment. Method and materials: Upon approval by the University of Guarulhos Committee on Human Subjects, 100 restorations were inserted in 46 patients who required Class II restorations in their molars and premolars. Enamel and dentin walls were conditioned with a self-etching primer (for Clearfil SE Bond) or etched with 34% phosphoric acid (for Prime&Bond NT). A 1- to 2-mm-thick increment of a flowable composite (Filtek Flow) was used in the proximal box in 50% of the restorations of each adhesive. Preparations were restored with a packable composite (Surefil). The restorations were evaluated preoperatively and 2 weeks postoperatively for sensitivity to cold, air, and masticatory forces using a visual analog scale. Marginal integrity of the accessible margins was also evaluated. Statistical analysis used a mixed linear model with subject as a random effect. Results: Ninety-eight teeth from 44 subjects were observed at 2 weeks. The type of adhesive and use of flowable composite had no significant effects or interaction for any of the four outcomes of interest, ie, change from baseline to 2 weeks in sensitivity and response time for the cold or air stimulus. For the air stimulus, the overall average change from baseline was not significant for either sensitivity or response time. For the cold stimulus, the overall average change from baseline was significant for both sensitivity and response time. No case of sensitivity to masticatory forces was observed. Conclusion: No differences in postoperative sensitivity were observed between a self-etch adhesive and a total-etch adhesive at 2 weeks. The use of flowable composite did not decrease postoperative sensitivity.
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We present a synthesis of some 20,504 mineral analyses of ~500 Hole 735B gabbros, including 10,236 new analyses conducted for this paper. These are used to construct a mineral stratigraphy for 1.5-km-deep Hole 735B, the only long section of the lower crust drilled in situ in the oceans. At long wavelengths, generally >200 m, there is a good chemical correlation among the principal silicate phases, consistent with the in situ crystallization of three or four distinct olivine gabbro bodies, representing at least two major cycles of intrusion. Initial cooling and crystallization of these bodies must have been fairly rapid to form a crystal mush, followed by subsequent compaction and migration of late iron-titanium-rich liquids into shear zones and fractures through which they were emplaced to higher levels in the lower crust where they crystallized and reacted with the olivine gabbro host rock to form a wide variety of ferrogabbros. At the wave lengths of the individual intrusions, as represented by the several olivine gabbro sequences, there is a general upward trend of iron and sodium enrichment but a poor correlation between the compositions of the major silicate phases. This, together with a wide range in minor incompatible and compatible element concentrations in olivine and pyroxene at a given Mg#, is consistent with widespread permeable flow of late melt through these intrusions, in contrast to what has been documented for a 600-m section of reputedly fast-spreading ocean crust in the Oman Ophiolite. This unexpected finding could be related to enhanced compaction and deformation-controlled late-stage melt migration at the scale of intrusion at a slow-spreading ocean ridge, compared to the relatively static environment in the lower crust at fast-spreading ridges.