Marxico summation8/15/2023 ![]() ![]() I’ve been using Stackedit for a few months now, but that was until I found Marxico. ![]() However, the biggest issue I have is that I haven’t found a good app that’ll keep all my notes together and synced across multiple platforms. 1194–1203.I’ve been getting more and more into using markdown to take notes do to the simplicity. L., Leyden, R., and Ewing, R., 1968, Newly discovered diapirs in Gulf of Mexico: Am. ![]() Wilhelm, O., and Ewing, M., 1972, Geology and history of the Gulf of Mexico: Geol. H., 1963, Nuclear Central America, hub of the Antillean transverse belt, in: Backbone of the Americas: Am. L., 1962, Upper Cretaceous and Tertiary Stratigraphy of Guatemala: Am. Age and evolution of salt basins of southeastern Mexico, Am. Tercier, J., 1932, Geological investigation in Peninsula de Yucatán. Schuchert, C., 1935, Historical Geology of the Antillean and Caribbean Region: John Wiley and Sons, New York. Sapper, K., 1937, Mittelamerika’, Handbuch der Regionalen Geologia, v. Sapper, K., 1896, Sobre la geografía física y la geología de la Península de Yucatán: Inst. Petróleos Mexicanos, 1966–69, Informes geológicos inéditos. A., 1970, Interactions among tectonics, sedimentation and hydrocarbon accumulation: Gulf Coast Assoc. New Orleans Geological Society, 1962, Guide Book, Field Trip to Peninsula de Yucatán, 120 p. Murray, G., 1961, Geology of the Atlantic and Gulf Coastal Province of North America: Harper and Row, New York, 696 p. A., 1967, Future hydrocarbon provinces of Gulf of Mexico. López Ramos, E., 1972, Geología General., Edicíon Escolar, 262 p., Mexico, D. López Ramos, E., 1969, Marine paleozoic rocks of México Am. López Ramos, E., 1969, Geología del SE de México y Norte de Guatemala, en: TrabajosPresentados en la II Reunión de Geólogos de América Central.: ICAITI, p. W., et al., 1969, Carbonate sediments and reefs, Yucatan Shelf, Mexico: Am. J., and Dengo, G., 1960, Posibilidades petrolíferas de la cuenca de Peten, Guatemala: Fac. E., 1971, Jurassic salt, Central Gulf of Mexico and its temporal relation to circum-Gulf evaporites: Am. T., 1967, Salt Domes, Gulf Region, United States and Mexico: Gulf Publ. 11–13.įlores, G., 1952, Geology of Northern British Honduras: Am. L., 1970, Deep Sea Drilling Project-Leg 10: Geotimes, v. C., 1955, Geophysical and geological investigation in the Gulf of Mexico-Part 1: Geophysics, v. Cal., Berkeley (mimeographed).Įricson, D. R., 1965, Bosquejo Geológico de la Península de Yucatán: Tesis Professional ESIA ipn México, 55 p.Įdwards, C., 1957, Quintana Roo Mexico’s Empty Quarter (Report of Field Work Carried out under Office of Naval Research, Contract 222): Dept. de la U.N.A.M., 18 p.ĭengo, G., and Bohnenberger, H., 1970, Structural development of northern Central America: Am. 80, 192 p.īonis, S., Bohnenberger, H., and Dengo, G., 1970, Mapa Geológico de la Republica de Guatemala, la Edición: Instituto Geográfico Nacional.īutterlin, J., and Bonet, F., 1960, Microfauna del Eoceno Inferior de la Península de Yucatán: Paleontología Mexicana, No. See also: Bonet, F., 1967, Biogeología Subsuperficial del Arrecife Alacranes, Yucatán, Inst. 1204–1228.īonet, F., 1956, Nota Preliminar Sobre la Constitution de los Arrecifes Coralinos de la Sonda de Campeche, México, Resumen XX, Congreso Geol. R., Antoine, J., Ewing, M., and Jones, B., 1968, Structure of the Mexican continental shelf and slope, Gulf of Mexico: Am. H., 1972, New interpretation of geology of Maya Mountains, British Honduras: Am. This process is experimental and the keywords may be updated as the learning algorithm improves.Īlvarez, M., 1954, Exploración geologica preliminar del Rio Hondo, Quintana Roo: Assoc. These keywords were added by machine and not by the authors. The western boundary is formed by the coastal plains of the Gulf of Mexico in southwestern Campeche and eastern Tabasco. 2), a positive feature including the Guatemalan Peten and the Maya Mountains of British Honduras. The southern margin is formed by the Arco de la Libertad (Fig. To the east the continental slope also bounds the area, but there descends into the Caribbean Sea. On the north and northeast the continental slope at the edge of Campeche bank forms a natural boundary for the region. This is an area of approximately 300,000 km 2. The study covers the Yucatan Shelf from 16°–22° north and from 86°–91° west, including the eastern parts of the states of Yucatan and Campeche, the territory of Quintana Roo, the northern part of Guatemala, and the northeastern part of British Honduras (Belice) (Fig. This paper presents an integrated, though generalized, study of the Geology of the Yucatán Peninsula based upon what the writer believes to be the most adequate available information. ![]()
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