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    RAAPNOTITIE 1062

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    onderzoeksrappor

    . 1062 Año 22 (2023) enero. El Tlacuache

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    La importancia del tema de la Epifanía en México, se manifiesta no solo en las festividades, sino en los programas pictóricos conventuales e incluso en la dedicatoria de los mismos, tal es el caso de los conventos agustinos del Meztitlán, en Hidalgo, y el de Huatlatlahuca, en Puebla. Retablos y una producción prolífica de cuadros representan la escena desde la segunda mitad del siglo XVI, siguiendo los modelos fijados en Europa a través de los grabados, con adaptaciones que se integran el contexto del Nuevo Mundo.- Epifanía la adoración de los Reyes Magos por Noel Serrano Aguirre y Mitzi de Lara Duarte.Mónica Morales, Pintura de los Reyes, Morelos. "Memoria Restauración", 2019.De Benavente, T. de (Motolinía), Historia de los Indios de la Nueva España, Sánchez García. D. (ed.),Barcelona, Herederos de Juan Gil, 1914, Trat. I, cap. 13. El Auto de los Reyes Magos, también conocido como Representación de los Reyes Magos, es una primitiva pieza dramática toledana que conmemora la visita de unos magos en la Epifanía; esta fue escrita probablemente en el siglo XII según se deduce de la letra. Obtenido de https://emad.defensa.gob.es/ Museo Nacional del Virreinato. Anónimo. S.XVII Óleo sobre tela. Mediateca INAH. Página 21. Epifanía de la Virgen /Catedral de Morelia Pitacua , S. XVIII – renovado en el S. XIX

    RAAPRAPPORT 1062

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    onderzoeksrappor

    Commento all'art. 1062 c.c.

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    Il contributo costituisce un commento all'art. 1062 del c.c. in tema di acquisto della servitù per destinazione del padre di famigli

    Sediment wave layer summary in ODP Site 172-1062

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    Abyssal mud waves (or fine-grained sediment waves) are often cited as evidence for deep current activity because subbottom profiles show that the wave form has migrated with time. The migration history of a fine-grained sediment wave on the Blake-Bahama Outer Ridge (ODP Site 1062) has been studied through the analysis of multiple ODP holes spaced across the wave. Additional information about wave migration patterns comes from 3.5-kHz records and watergun seismic profiles. These data suggest that wave migration has varied during the last not, vert, similar ~10 Myr, although the only sediments sampled are younger than 4.8 Ma. Seismic profiles suggest wave migration was initiated about 8-10 Ma, and wave migration was pronounced from about 5 Ma to about 1 Ma (with an episode of wave reorganization about 4.5 Ma). Analysis of ODP cores suggests that migration rates have been somewhat lower and more variable during the last 1 Myr. Intervals of no wave migration are observed for several time intervals and appear to characterize deglaciations, especially during the last 500 kyr. Comparisons between seismic profiles and the core record show that most of the seismic horizons correlate closely with time horizons, and thus that the seismic profiles give a reasonable representation of sediment wave migration. Models suggest that wave migration is more pronounced during periods of higher bottom current flow and less pronounced during periods of lower current flow. Thus the migration record is consistent with generally higher bottom flow speeds at this site prior to 1 Ma and lower bottom flow speeds after 1 Ma. The Mid-Pleistocene Transition from a dominant climatic periodicity of 40 kyr to a dominant climatic periodicity of 100 kyr starts at about this time, suggesting an overall reduction in bottom flow speed at this site coincident with changing climate patterns. These changes in flow speed could be related to changes in the depth of the Western Boundary Undercurrent as well as to changes in the speed of thermohaline circulation

    Going Beyond Counting First Authors in Author Co-citation Analysis

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    The present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed

    Variations on the Author

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    “Variations on the Author” discusses two of Eduardo Coutinho’s recent films (Um Dia na Vida, from 2010, and Últimas Conversas, posthumously released in 2015) and their contribution to the general question of documentary authorship. The director’s filmography is characterized by a consistent yet self-effacing form of authorial self-inscription: Coutinho often features as an interviewer that rather than express opinions propels discourses; an interviewer that is good at listening. This mode of self-inscription characterizes him as an author who is not expressive but who is nonetheless markedly present on the screen. In Um Dia na Vida, however, Coutinho is completely absent form the image, while Últimas Conversas, on the contrary, includes a confessional prologue that moves the director from the margins to the center of his films. This article examines the ways in which these works stand out in the filmography of a director who offers new insights into the notion of cinematic authorship

    English Episcopal Acta 33: Worcester 1062-1185

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    English Episcopal Acta 33: Worcester 1062-118

    Paleomagnetic, stable oxygen isotope ratios, and U/Th activities of ODP Site 172-1062

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    Geomagnetic excursions are recognized as intrinsic features of the Earth's magnetic field. High-resolution records of field behaviour, captured in marine sedimentary cores, present an opportunity to determine the temporal and geometric character of the field during geomagnetic excursions and provide constraints on the mechanisms producing field variability. We present here the highest resolution record yet published of the Blake geomagnetic excursion (~125 ka) measured in three cores from Ocean Drilling Program (ODP) Site 1062 on the Blake-Bahama Outer Ridge. The Blake excursion has a controversial structure and timing but these cores have a sufficiently high sedimentation rate (~10cm/ka) to allow detailed reconstruction of the field behaviour at this site during the excursion. Palaeomagnetic measurements of the cores reveal rapid transitions (<500 yr) between the contemporary stable normal polarity and a completely reversed state of long duration which spans a stratigraphic interval of 0.7 m. We determine the duration of the reversed state during the Blake excursion using oxygen isotope stratigraphy, combined with 230Th excess measurements to assess variations in the sedimentation rates through the sections of interest. This provides an age and duration for the Blake excursion with greater accuracy and with constrained uncertainty. We date the directional excursion as falling between 129 and 122 ka with a duration for the deviation of 6.5±1.3 kyr. The long duration of this interval and the fully reversed field suggest the existence of a pseudo-stable, reversed dipole field component during the excursion and challenge the idea that excursions are always of short duration
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