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O. Capitan (illustrateur 18..-18..) : signature “O. Capitan” [1884]
No full textO. Capitan (illustrateur 18..-18..) : signature “O. Capitan” [1884] ; illustrateur actif dans l’édition musicale décennies 1880-1890, absent des ouvrages spécialisés, aucun renseignement biographique, plusieurs notices d’autorité BNF. 18 illustrations sur la banque de données de Frank Lateur “Illustrated Sheet Music” https://www.imagesmusicales.be/search/illustrator/O.-Capitan/6023/ShowData/8/Submit/ [Notice actualisée 04/11/2018
O. Capitan (illustrateur 18..-18..) : signature “O. Capitan” [1884]
No full textO. Capitan (illustrateur 18..-18..) : signature “O. Capitan” [1884] ; illustrateur actif dans l’édition musicale décennies 1880-1890, absent des ouvrages spécialisés, aucun renseignement biographique, plusieurs notices d’autorité BNF. 18 illustrations sur la banque de données de Frank Lateur “Illustrated Sheet Music” https://www.imagesmusicales.be/search/illustrator/O.-Capitan/6023/ShowData/8/Submit/ [Notice actualisée 04/11/2018
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A letter from Capitan Rendon to Dr. Hector P. Garcia.
No full textA handwritten letter from Capitan Rendon to Dr. Hector P. Garcia, thanking him for attending his mothers funeral
Geology of El Capitan, Sonora, Mexico
No full textScale of accompanying maps 1:4,000 ; Transverse Mercator projection spheroidCenter coordinates of accompanying maps in decimal degrees [longitude/latitude]: -114.406945?? and 32.310278??Title of map on Plate 1: Geologic maps of El Capitan, Sonora, Mexico.Title of diagram on Plate 2: Geologic cross sections.Title of diagram on Plate 3: Crustal - scale cross section.Three folded plates in pocket.Las Adelitas - I11D78, scale 1:50,000.No geographic names are shown on the geological map or cross section [Plates 1 and 2]. From the topographic maps: Las Adelitas I11D78 and Ejido Aquiles Serdan I11D79, there are no geographic names associated with the hills that form the mapped outcrops by Gregory Leveille. The use of, ???El Capitan???, to describe these hills is commented about by Diane Fitts in her thesis. Diane uses, ??? Ejidio Serdan??? to describe the same area. ???Ejido Aquilles Serdan??? is about nine kilometers to the northeast along Mexican Highway 2. Ejido el Sinaloenes, also along Mexican Highway 2, is three kilometers west of Ejido Aquilles Serdan and about two kilometers closer to the mapped outcrops.Plate 3, which is a regional cross section, has the following geographic names: Algodones Fault, Chocolate Mountains, Mule Mountains, McCoy Mountains, Big Maria Mountains.Carta topografica Las Adelites I11D78. Instituto Nacional de Estadistica Geografica e Informatica [INEGI]. Esferoide - Clarke 1866. Proyeccion Transversa de Mercator. Cuadricula UTM cada 1000m. Datum Horizontal Northamericano de 1927. Refencia de cotas nivel medio del mar. Procedimiento de compilacion fotogrametrico. Primera edicion 1981. Primera Impresion 1981. Autoridad -- Direccion General de Geografica del Torritorio Nacional. Segunda Impresion 1994. Equidistancia entre curves de nivel: 10 metros.Topographic map Las Adelites. National Institute of Statistics, Geography and Information INEGI]. Spheroid - Clarke 1866. Projection Transverse Mercator. Quadrangle 1000m grid UTM. Horizontal datum, NAD27 [North American Datum 1927]. Reference to mean sea level. Topography from aerial photography by photogrammetric methods. First edition 1981. First printing 1981. Published by General Director of Geography of the National Territory. Second printing 1994. Contour interval: 10 meters.Bibliography: leaves 108-119El Capitan, located 50 km southeast of Yuma, Arizona, consists of complexly deformed and moderately metamorphosed carbonate, clastic, and volcanic strata, granitic and granodioritic plutonic rocks, and mylonitic plutonic gneiss. The metamorphosed carbonate and clastic rocks can be subdivided into formations correlative with the upper Paleozoic-lower Mesozoic cratona1 section of the Colorado Plateau, northwestern Arizona. Metamorphosed lithologic equivalents of the Pennsylvanian-Permian Supai Group, Permian Coconino Sandstone, Permian Toroweap and Kaibab Limestones,\ud
Triassic Moenkopi Formation, and Upper Triassic-Lower Jurassic Aztec Sandstone are present. A sequence of metasedimentary rocks overlying the metamorphosed Aztec Sandstone may be correlative with Jurassic strata on the Colorado Plateau; however, the exact correlation is not understood. The metavolcanic rocks at El Capitan are believed to be Jurassic in age based on stratigraphic relationships observed within the study area. A Late Jurassic emplacement age for the granodioritic plutonic rocks is suggested from radiometric studies. \ud
All of the rocks at El Capitan were deformed and metamorphosed at upper greenschist-lower amphibolite facies subsequent to the emplacement of the plutonic rocks. Deformation was due to top-to-the northeast simple shear, although a component of pure shear may have been present. Deformation resulted in the formation of thrust faults, mylonitic shear zones, large- and smale-scale folds, and a pervasive axial-planar foliation. The age of this deformational event can be bracketed between Middle Jurassic and earliest Late Cretaceous time. \ud
Because the cratonic strata at El Capitan appear to be in place relative to Paleozoic-lower Mesozoic depositional trends, it seems probable that the Mojave-Sonora megashear cannot extend across the eastern Mojave Desert, California, but if it exists, must instead be located west of this area. However, this reconstruction creates distinct problems with the definition of the megashear as separating Precambrian terranes whose boundary is well-documented to be 50 km east of El Capitan. Alternately, the Paleozoic hingeline and miogeoclinal belt may swing around the southwestern United States and northwestern Mexico unbroken by major left-lateral faults. \ud
The Mesozoic deformational history recorded in the rocks at El Capitan appears to be remarkably similar to the deformational history of Mesozoic compressional terranes exposed to the north of this area. The similarities in the style and timing of deformation in these areas could be merely coincidental, but more likely, are related by some large-scale tectonic process
Teobert Maler
No full textCapitan . Teobert Maler. In: Journal de la Société des Américanistes. Tome 11, 1919. pp. 636-637
Teobert Maler
No full textCapitan . Teobert Maler. In: Journal de la Société des Américanistes. Tome 11, 1919. pp. 636-637
Claude-Joseph-Désiré Charnay
No full textCapitan . Claude-Joseph-Désiré Charnay. In: Journal de la Société des Américanistes. Tome 11, 1919. pp. 629-631
Emile Levasseur
No full textCapitan . Emile Levasseur. In: Journal de la Société des Américanistes. Tome 8, 1911. pp. 283-284
G. Maspero
No full textCapitan . G. Maspero. In: Journal de la Société des Américanistes. Tome 11, 1919. pp. 639-640
P. Berthon
No full textCapitan . P. Berthon. In: Journal de la Société des Américanistes. Tome 11, 1919. pp. 618-619
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