Saitō Mussashi-bō Benkei : (Tales of the wars of the Gempei)

Title also in Japanese.

Gikeiki, Soga monogatari.

Includes index.

Servidores públicos del estado con especial protección constitucional. Políticas de prevención del daño antijurídico en relación con su retiro del servicio

El retiro del servicio de los empleados públicos aparece como una facultad reglada en las normas del empleo público que, cuando se da alguna de las hipótesis legales que lo hacen procedente, facultan al nominador para ejercer sus atribuciones legales, persiguiendo, ante todo, razones del servicio: su mejora, renovación, eficiencia y moralidad, entre otras. A partir del concepto de una buena administración del Estado, establecer la procedencia y elementos estructurales de una política de prevención del daño antijurídico en relación con el retiro del servicio de servidores públicos que, conforme al ordenamiento jurídico gozan de una especial protección constitucional. Conocer el concepto, el alcance, la regulación y desarrollo jurisprudencial de esta trascendental atribución para el servicio público, resulta indispensable para la debida aplicación del derecho, del ejercicio de las atribuciones públicas por parte de la Administración, y para la prevención del daño antijurídico.

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 1159 - Zum Streit zwischen Professor Böck und den Homöopathen

u.a. Besuch von Fedor Stauwe;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 1189 - Fragment des Ergebnisses der ausgeschriebenen Preisschrift an der Universität Leipzig

Empfang bei Professor Heinrich Wuttke in Leipzig; 1. Preis an Rudolph Seydel; Geschichtsphilosophie;

Ms. Ff. Mus. 1159 - Jubilate

[Georg Philipp Telemann]. [Text: Gottfried Simonis]

Mineralogy of altered whole rocks from ODP Sites 193-1188 and 193-1189, PACMANUS field

Postcruise X-ray diffraction (XRD) data for 95 whole-rock samples from Holes 1188A, 1188F, 1189A, and 1189B are presented. The samples represent alteration types recovered during Leg 193. The data set is incorporated into the shipboard XRD data set. Based on the newly obtained XRD data, distribution of alteration phases were redrawn for Ocean Drilling Program Sites 1188 and 1189.

Horizontal profiles of longwave and shortwave radiation components over sea ice near Barrow, Alaska during the 2011 melt

An integrated instrument package for measuring and understanding the surface radiation budget of sea ice is presented, along with results from its first deployment. The setup simultaneously measures broadband fluxes of upwelling and downwelling terrestrial and solar radiation (four components separately), spectral fluxes of incident and reflected solar radiation, and supporting data such as air temperature and humidity, surface temperature, and location (GPS), in addition to photographing the sky and observed surface during each measurement. The instruments are mounted on a small sled, allowing measurements of the radiation budget to be made at many locations in the study area to see the effect of small-scale surface processes on the large-scale radiation budget. Such observations have many applications, from calibration and validation of remote sensing products to improving our understanding of surface processes that affect atmosphere-snow-ice interactions and drive feedbacks, ultimately leading to the potential to improve climate modelling of ice-covered regions of the ocean. The photographs, spectral data, and other observations allow for improved analysis of the broadband data. An example of this is shown by using the observations made during a partly cloudy day, which show erratic variations due to passing clouds, and creating a careful estimate of what the radiation budget along the observed line would have been under uniform sky conditions, clear or overcast. Other data from the setup's first deployment, in June 2011 on fast ice near Point Barrow, Alaska, are also shown; these illustrate the rapid changes of the radiation budget during a cold period that led to refreezing and new snow well into the melt season.

Description, geochemistry and mineral composition of ODP Site 193-1189 jasperoids, PACMANUS field

Bright red "jasperoids" were recovered at three positions during Leg 193 drilling below Roman Ruins (Site 1189) in the PACMANUS hydrothermal field. These do not represent fossil exhalative oxide deposits equivalent to those associated with sulfide chimneys at the Roman Ruins seafloor. Rather, they constitute an integral, relatively early stage involving oxidized fluids in the development of veins and breccias that characterize the mostly sulfidic stockwork zone intersected below Roman Ruins in Hole 1189B. They formed by growth of quartz in open spaces created by hydrofracturing, the characteristic feature being mostly euhedral cores dusted by tiny hematite flakes. In one occurrence there are also frondlike aggregates and possible earlier cavity linings of hematite, overgrown by quartz, that potentially formed by maturation of ferruginous gels first deposited in the openings. The trace element geochemistry of the jasperoids, apart from minor enrichment in uranium, provides no indication that they represent subsurface conduits for fluids that deposit Fe-Mn-Si at the seafloor, though this remains a possibility for some such deposits.