920 resultados para Juan Duns Escoto , Beato, ca. 1266-1308-Crítica i interpretació
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Indices.
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"Oracion funebre en las reales exequias con que la ... ciudad de Zaragoza acompañò el dolor de sus ... monarcas en la muerte de los ... delfines de Francia Luis de Borbon y Maria Adelaida de Saboya / dixola ... el Rmo Padre Francisco Bru de la Compañia de Jesus ... ", con portadilla orlada y pag. propia.
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CCBE S. XV,I
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I. Aureliensis 2-67.
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Contiene: T. I (568, [2] p., [18] h. de lám.) -- T. II (400, [4] p., [15] h. de lám.)
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Segunda parte de la Diana de George de Monte Mayor / por Alonso Perez, con port. propia en p. 361.
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Mode of access: Internet.
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Contiene: T. I (593 p., [11] h. lám.) -- T. II (497 p., [22] h. lám.)
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Mode of access: Internet.
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t.I El jeneral Don José Manuel Borgoño. El coronel español Don José Ordoñez. Don Ignacio Domeyko.--t.II Don Andrés Bello. Don Carlos Bello. Don Francisco Bello. Don Juan Bello.--t.III. Don Manuel Antonio Tocornal i Grez. Don José Joaquín Vallejo.--t.IV. Don Vicente Carvallo i Goyeneche. Don García Hurtado de Mendoza i Don Alonso de Ercilla i Zúñiga. Don Gabriel Cano de Aponte. Don José Rodríguez Ballesteros. Don Rodulfo Amando Philippi. Don José Antonio Torres. Don Simón Rodríguez. Don Francisco Núñez de Pineda i Bascuñán. Don Bernardo de Vera i Pintado. La necrópolis de Don José Miguel Infante.
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On double leaves, oriental style.
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Contiene: t. I - t. II.
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I. Artephii, dess uhralten Philosophi von der geheimen Kunst, und Stein der Weisen, Geheimes Buch -- II. Johannis Garladii (sic), seu Hortulani Angli, Compendium Alchimiæ, oder Erklärung der Smaragdischen Tafel Hermetis Trismegisti -- III. Arnoldi de Villanova, Erklärung über den commentarium Hortulani -- IV. Bernhardi Comitis Trevis, Absonderlicher Tractat vom Stein der Weisen.
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Convention signed on 27 june 1308 (1892) [i.e. 8 July 1892]
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Comparison of initial Pb-isotope signatures of several early Archaean (3.65-3.82 Ga) lithologies (orthogneisses and metasediments) and minerals (feldspar and galena) documents the existence of substantial isotopic heterogeneity in the early Archaean, particularly in the Pb-207/Pb-204 ratio. The magnitude of isotopic variability at 3.82-3.65 Ga requires source separation between 4.3 and 4.1 Ga, depending on the extent of U/Pb fractionation possible in the early Earth. The isotopic heterogeneity could reflect the coexistence of enriched and depleted mantle domains or the separation of a terrestrial protocrust with a U-238/Pb-204 (mu) that was ca. 20-30% higher than coeval mantle. We prefer this latter explanation because the high-p signature is most evident in metasediments (that formed at the Earth's surface). This interpretation is strengthened by the fact that no straightforward mantle model can be constructed for these high-mu lithologies without violating bulk silicate Earth constraints. The Pb-isotope evidence for a long-lived protocrust complements similar Hf-isotope data from the Earth's oldest zircons, which also require an origin from an enriched (low Lu/Hf) environment. A model is developed in which greater than or equal to3.8-Ga tonalite and monzodiorite gneiss precursors (for one of which we provide zircon U-Pb data) are not mantle-derived but formed by remelting or differentiation of ancient (ca. 4.3 Ga) basaltic crust which had evolved with a higher U/Pb ratio than coeval mantle in the absence of the subduction process. With the initiation of terrestrial subduction at, we propose, ca. 3.75 Ga, most of the greater than or equal to3.8-Ga basaltic shell (and its differentiation products) was recycled into the mantle, because of the lack of a stabilising mantle lithosphere. We argue that the key event for preservation of all greater than or equal to3.8-Ga terrestrial crust was the intrusion of voluminous granitoids immediately after establishment of global subduction because of complementary creation of a lithospheric keel. Furthermore, we argue that preservation of !3.8-Ga material (in situ rocks and zircons) globally is restricted to cratons with a high U/Pb source character (North Atlantic, Slave, Zimbabwe, Yilgarn, and Wyoming), and that the Pb-isotope systematics of these provinces are ultimately explained by reworking of material that was derived from ca. 4.3 Ga (i.e. Hadean) basaltic crust.