980 resultados para Reinwald, C., (París)
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Mode of access: Internet.
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Vol.6.-Pars secunda, sive Opera declamatoria, etc.
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Mode of access: Internet.
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Mode of access: Internet.
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Descripción basada en CCPB.
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Mode of access: Internet.
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Mode of access: Internet.
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Contiene : M- Z.
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Sub-titles of v. 3, pt. 1-2, c. 2, vary slightly. v. 1-3, c. 2-24 cm.
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A partir del hallazgo de un tipo particular de envases: ungüentarios y perfumarios en una nueva tumba en el territorio de Arados/Amrit, observamos cómo se incrementa la presencia de estos envases en tumbas de incineración e inhumación durante el primer milenio antes de Cristo en la cuenca mediterránea. Hemos elaborado una serie de análisis y discusiones sobre su distribución, cronología, significado y uso social, tratando de establecer una periodización de sus usos y una contextualización cultural y social dentro del ritual funerario y del uso de determinadas materias primas empleadas para su elaboración.
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El presente articulo intenta determinar las razones por las que el santuario de Sant Miquel de Llíria, uno de los más importantes de la actual provincia de Valencia, se consagró al arcàngel guerrero. Se estudia para ello la historia de su culto en Occidente, haciendo hincapié en aspectos como su relación con los lugares elevados y la frecuente proximidad de sus santuarios con aquellos dedicados a la Virgen. Atenderemos también a aspectos fundamentales del contexto histórico, como los movimientos de renovación espiritual medievales, la influencia del médico y teólogo Arnau de Vilanova en la Valencia de principios del siglo XIV y las profecías escatológicas vinculadas a la llegada del Anticristo.
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Dehram group includes Faraghan, Dalan and Kangan formations. Kangan formation ages lower terias. That is one of the important reservoir rocks of southern Iran and Persian Gulf. In this research Kangan formation is studied in two A and B wells. Based on 75 studies on thin section, four carbonate litho acies association A, B, C, D with 12 subfacies are identified. A lithofacies association includes 4 subfacies: A1, A2, A3 and A4. B lithofacies association consists of 3 subfacies: B1, B2 and B3. C lithofacies association consists of 3 subfacies: C1, C2, C3 and D lithofacies association includes 2 subfacies: D1 and D2. On the base of studies lithofacies association of Kangan formations are formed in 3 environments of: Tidal Flat, Lagoon and Barrier Shore Complex in a Carbonated Platform Ramp type. Diagenetic processes have effected this formation. The most important Diagenetic processes are: Cementation, Anhydritization, Micrization, Neomorphism, Bioturbation, Dissolution, Compaction, Dolomitization and Porosity. Sequence staratigraphy studies were performed base on the vertical and horizontal relationship of lithofacies association and well logging in gamma ray and sonic type that causes the identification of two sedimentary sequences: First sedimentary sequence includes: Transgressive System Tract (TST) and High Stand System Tract (HST). The lower boundary of this sequence is in Sequence Boundary 1 (SB1) which shows unconformities of Dalan and Kangan that are Permian-terias unconformities. The upper boundary is in Sequence Boundary 2 (SB2) type that is identified by carbonate facies associated by anhydrite nodular. Second sedimentary sequence includes: TST and HST. Lower and upper boundaries of these sequences are both in SB2 type. The lower and upper boundary is made of carbonate facies with anhydrite nodular.