992 resultados para Signoret, Gabriel (1878-1937)
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Fecha: >1970 reproducción / Unidad de instalación: Carpeta 45 - Expediente 1-4 / Nº de pág.: 3 (mecanografiadas)
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Fecha: >1970 / Unidad de instalación: Carpeta 48 - Expediente 7-2 / Nº de pág.: 2 (1 mecanografiada, 1 manuscrita)
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Fecha: s.f. (>1970 copia) / Unidad de instalación: Carpeta 45 - Expediente 2-17 / Nº de pág.: 2 (mecanografiadas)
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Fecha: >1970 / Unidad de instalación: Carpeta 48 - Expediente 7-20-1 / Nº de pág.: 6 (3 mecanografiadas, 3 manuscritas)
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Parte 1 - Atos do Poder Executivo
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Parte 1 - Atos do Poder Legislativo
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Charles M. Breder Jr. “hypothesis” diary is a deviation from the field diaries that form part of the Breder collection housed at the Arthur Vining Davis Library, Mote Marine Laboratory. There are no notes or observations from specific scientific expeditions in the document. Instead, the contents provide an insight into the early meticulous scientific thoughts of this biologist, and how he examines and develops these ideas. It is apparent that among Dr. Breder’s passions was his continual search for knowledge about questions that still besieged many scientists. Topics discussed include symmetry, origin of the atmosphere, origin of life, mechanical analogies of organisms, aquaria as an organism, astrobiology, entropy, evolution of species, and other topics. The diary was transcribed as part of the Coastal Estuarine Data/Document Rescue and Archeology effort for South Florida. (PDF contains 33 pages)
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8 cartas y 1 tarjeta postal (manuscritas y mecanografiadas) ; entre 335x227mm y 135x90mm. Ubicación: Caja 1 - Carpeta 33
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1 nota y 3 cartas (manuscritas) ; entre 155x047mm y 210x295mm. Caja 1 - Carpeta 47
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Anais do Parlamento Brasileiro, 1878.
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Anais do Parlamento Brasileiro, 1878.
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Anais do Parlamento Brasileiro, 1878.
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Anais do Parlamento Brasileiro, 1878.
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An area of about 25 square miles in the western part of the San Gabriel Mountains was mapped on a scale of 1000 feet to the inch. Special attention was given to the structural geology, particularly the relations between the different systems of faults, of which the San Gabriel fault system and the Sierra Madre fault system are the most important ones. The present distribution and relations of the rocks suggests that the southern block has tilted northward against a more stable mass of old rocks which was raised up during a Pliocene or post-Pliocene orogeny. It is suggested that this northward tilting of the block resulted in the group of thrust faults which comprise the Sierra Madre fault system. It is show that this hypothesis fits the present distribution of the rocks and occupies a logical place in the geologic history of the region as well or better than any other hypothesis previously offered to explain the geology of the region.