952 resultados para John VI Cantacuzenus, Emperor of the East, 1292-1383.
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owing to the loss of the volume containing the entries for that period."--Pref.
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In verse.
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Colored plates accompanied by guard sheets with descriptive letterpress.
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v. 1. Arabian nights' entertainments [from the French version of A. Galland] New Arabian nights [from the French version of D. Chavis and J. Cazotte]--v. 2. Continuation of the New Arabian nights. Persian tales [from the translation of F. Pétis de la Croix] Persian tales of Inatulla of Delhi [tr. by A. Dow] Oriental tales [by A. C. P., comte de Caylus] The history of Nourjahad [by Mrs. Frances Sheridan] Additional tales from the Arabian nights.--v. 3. Mogul tales [by T. S. Gueulette] Turkish tales [from the translation of F. Pétis de la Croix] Tartarian tales; Chinese tales [by T. S. Gueulette] Tales of the genii [by J. Ridley] The history of Abdalla, the son of Hanif [by J. P. Bignon]
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Mode of access: Internet.
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Mode of access: Internet.
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"First edition April 1908, second impression, April, 1908."
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Mode of access: Internet.
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Mode of access: Internet.
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During the expeditions ARK-VII/1, ARK-VII/3 and ARK-Xl2 sediment cores were taken by "RV Polarstern" from the shelf and the fjords of East Greenland and the Greenland Sea. The magnetic susceptibility and heavy mineral were determined at 48 surface sediment samples from undisturbed box cores. The main objective of this study was the identification of source areas and transport processes of terrigenous sediments at the East Greenland continental margin. The results can be summarized as lollows: 1a) Magnetic susceptibility in the North Atlantic is useful to detect delivery regions of the material transported by currents. b) The magnetic susceptibility is controlled by the ferromagnetic particles of the silt fraction. c) There are four important source areas: . The ferromagnetic particles of the box core PS2644-2 are transported from the Iceland Archipelago. . The material from the Geiki-Plateau effects the magnetic susceptibility in the Scoresby Sund Basin. . The magnetic susceptibility in the shelf regions in the North are produced by material from the fjords. . The ferromagnetic particles in the Greenland Sea are derived from the Mid Atlantic Ridges in the east. d) It is possible to determine the rock type, which delivers the ferromagnetic material because of differences in magnetic susceptibility of different intensity. . The erosion of the basalts of the Geiki-Plateau and the basalts of the Mid Atlantic ridges produce the high magnetic susceptibility in the south. . The magnetic susceptibility on the shelf in the north are probably produced by erosionproducts of the gneises of East Greenland. (2a) Heavy mineral assemblages show a significant difference between material transported by the Transpolar Drift from the Eurasian shelf regions (amphiboles, clinopyroxene, orthopyroxene) and material derived from East Greenland (garnets and opaque minerals). Transport via ice is dominant. b) lt is also possible to show different petrographic provenances (volcanic and metamorphic provenances). These associations verify the source areas. c) The information of heavy mineral composition gives no more detailed hint on the rock type or rock formation in the source area, due to mixing processes, large area of investigation and the sample quantity.
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Audit report on Mental Health Disability Services of the East Central Region (MHDS-ECR) for the year ended June 30, 2015
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Bathymetric data from a Hydrosweep multibeam sonar survey of a 720 km long tectonic corridor on the east flank of the southern EPR at 14 degrees 14'S covered about 25,000 km(2) of zero-age to 8.5 m.y. old crust (magnetic anomaly 4A). In this corridor we document a strong correlation of robust along flowline changes in abyssal hill morphology and seamount size distribution with spreading rate changes deduced from our magnetic data. Indeed, we find that both rms height of abyssal hills and abundance and height of seamounts increase significantly as spreading rate changes from similar to 75 mm/yr to over 85 mm/yr (half rate). Moreover, we identified 46 seamounts taller than 100 m. Previous studies on the southern EPR reported a larger density of seamounts, organized primarily in chains. Our investigation, however, revealed seamounts not associated with major chains, leading us to the conclusion that different forms of off-axis volcanism occur along the spreading center.