BUATOIS, L.A., SANTIAGO, N., PARRA, K. & STEEL, R. (2008) Animal-Substrate Interactions in an Early Miocene Wave-Dominated Tropical Delta: Delineating Environmental Stresses and Depositional Dynamics (Tácata Field, Eastern Venezuela). Journal of Sedimentary Research, 78, 458 - 478. BUCCIANTI, A. & ESPOSITO, P. (2004) Insights into Late Quaternary calcareous nannoplankton assemblages un<strong>de</strong>r the theory of statistical analysis for compositional data. Palaeogeography, Palaeoclimatology, Palaeoecology, 202, 209-227. BUCHY, M.-C., FREY, E., STINNESBECK, W. & GONZÁLEZ-GONZÁLEZ, A.H. (2007) Premiere mention du genre Dakosaurus (Crocodyliformes, Thalattosuchia) dans le Kimmeridgien (Jurassique Superoeur) du Mexique. Bulletin <strong>de</strong> la Societe Geologique <strong>de</strong> France, XXX, XXX-XXX. BUCHY, M.-C., FREY, E., STINNESBECK, W. & LÓPEZ-OLIVA, J.G. (2003) First occurrence of a gigantic pliosaurid plesiosaur in the late Jurassic (Kimmeridgian) of Mexico. Bulletin <strong>de</strong> la Societe Geologique <strong>de</strong> France, 174 (3), 271-278. BUCHY, M.-C., FREY, E., STINNESBECK, W. & LÓPEZ-OLIVA, J.G. (2006a) An annotated catalogue of the Upper Jurassic (Kimmerigdian and Tithonia) marine reptiles in the collections of the <strong>Universidad</strong> <strong>Autónoma</strong> <strong>de</strong> <strong>Nuevo</strong> Léon, Facultad <strong>de</strong> Ciencias <strong>de</strong> la Tierra, Linares, Mexico. Oryctos, 6, 1-18. BUCHY, M.-C., VIGNAUD, P., FREY, E., STINNESBECK, W. & GONZÁLEZ-GONZÁLEZ, A.H. (2006b) A new thalattosuchian crocodyloform from the Tithonian (Upper Jurassic) of northeastern Mexico. Comptes-Rendus Paleovol, 5, 785-794. BURIÁNEK, D., NĚMEČKOVÁ, M. & HANŽL, P. (2003) Petrology and geochemistry of plutonic rocks from the Polička and Zábřeh crystalline units (NE Bohemian Massif). Czech Geological Survey, 78, 9-22. BURROWS, R.H. (1909) Geology of northern Mexico. Minn. Sci. Press, 99, 290-327. BURST, J.F. 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(1983) Tectono-stratigraphic terranes and mineral resource distributions of Mexico. Canadian Journal of Earth Sciences 20, 1040–1051. CAMPA, U.M.F. & IRIONDO, A. (2003) Early Cretaceous protolith ages for metavolcanic rocks from Taxco and Taxco Viejo in Sourthern Mexico, pp. 31. 99th Anuual Meeting of the Geological Society of America Association, Cordillean Seciton. CAMPA, U.M.F. & IRIONDO, A. (2004) Significado <strong>de</strong> dataciones Cretácicas <strong>de</strong> los arcos volcánicos <strong>de</strong> Taxco, Taxco Viejo y Chapolapa, en la evolución <strong>de</strong> la plataforma Guerrero-Morelos, 4, pp. 173. Unión Geofísica Mexicana, Reunión Nacional <strong>de</strong> Ciencias <strong>de</strong> la Tierra, GEOS, v. 4. CAMPA, U.M.F. & RAMIREZ-ESPINOSA, J. (1979) La evolución geológica y la metalogénises <strong>de</strong> Guerrero. <strong>Universidad</strong> <strong>Autónoma</strong> <strong>de</strong> Guerrero, Serie Técnico-Científica, 1, 84. 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Geological Society of America Bulletin, 109, 1321-1332. CARRILLO-BRAVO, J. (1961) Geología <strong>de</strong>l Anticlinorio Huizachal-Peregrina al NW <strong>de</strong> Ciudad Victoria, Tamaulipas. Boletín <strong>de</strong> la Asociación Mexicana <strong>de</strong> Geólogos <strong>de</strong>l Petróleo, 13 (1/2), 1-98. CATTANEO, A. & STEEL, R.J. (2003) Transgressive <strong>de</strong>posits: a review of their variability. Earth-Science Reviews, 62, 187-228. CECCA, F., MARTIN GARIN, B., MARCHAND, D., LATHUILIERE, B. & BARTOLINI, A. (2005) Paleoclimatic control of biogeographic and sedimentary events in Tethyan and peri-Tethyan areas during the Oxfordian (Late Jurassic). Palaeogeography, Palaeoclimatology, Palaeoecology, 222, 10-32. CENTENO-GARCÍA, E. (2005) Review of Upper Paleozoic and Lower Mesozoic stratigraphy and <strong>de</strong>positional environments of central and west Mexico: Constraints on terrane analysis and paleogeography. 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Revista Mexicana <strong>de</strong> Ciencias Geologicas, 14 (2), 244-260. CLARK, K.F., DAMON, P.E., SCHUTTER, S.R. & SHAFIQULLAH, M. (1979) Magmatismo en el Norte <strong>de</strong> México en relación a los yacimientos metalíferos. Asociación <strong>de</strong> Ingenieros Mineros Metalurgistas y Geólogos <strong>de</strong> México, Tec. XIII, 8-57. CLIFTON, H.E. (1981) Progradational sequences in Miocene shoreline <strong>de</strong>posits, southeastern Caliente Range, California. Journal of Sedimentary Petrology, 51, 165-184. CLIFTON, H.E. (2006 ) A reexamination of facies mo<strong>de</strong>ls for clastic shorelines. In: Facies Mo<strong>de</strong>ls Revisited (Eds R.G. Walker and H. Posamentier), Special Publication 84, pp. 293-337. Society of Economic Paleontologists and Mineralogists, Tulsa, Oklahoma. COATES, L. & MACEACHERN, J.A. (1999) The ichnological signature of wave- and river-dominated <strong>de</strong>ltas: Dunvegan and Basal Belly River formations, West-central Alberta. In: Digging Deeper, Finding a Better Bottom Line (Eds B. Wrathall, G. Johnston, R. Arts, L., J.-P. Zonneveld, D. Arcuri and S. McLellan), pp. 99-114C. Canadian Society of Petroleum Geologists & Petroleum Society, Core Conference. COATES, L. & MACEACHERN, J.A. (2008) The ichnological signatures of river- and wave-dominated <strong>de</strong>lta complexes: differentiating <strong>de</strong>ltaic from non-<strong>de</strong>ltaic shallow marine successions, Lower Cretaceous Viking Formation and Upper Cretaceous Dunvegan Formation, west-central Alberta. In: Applied Ichnology (Eds J.A. MacEachern, K.L. Bann, M.K. Gingras and S.G. Pemberton), Short Course Notes, 52, pp. 227-254. Society of Economic Paleontologists and Mineralogists, Tulsa, Oklahoma. COLEMAN, J.M. & WRIGHT, L.D. (1975) Major river <strong>de</strong>ltas: variability of processes and sand bodies. In: Deltas, Mo<strong>de</strong>ls fo Exploration (Ed M.L. Broussard), pp. 99-149. Houston Geological Society, Houston, Tx. COLLINSON, J.D. & THOMPSON, D.B. (1989) Sedimentary Structures. Unwin-Hyman, Ltd, London, 207 pp. CONDIE, K.C. (1967) Geochemistry of Early Precambrian graywakes from Wyoming. Geochemical et Cosmochemical Acta, 31, 2135-2149. CONDIE, K.C. (1980) Origin and early <strong>de</strong>velopment of the earth's crust. Precambrian Research, 11, 183-197. CONDIE, K.C. (1981) Archean Greenstone Belts. Elsevier, Amsterdam, 476 pp. CONDIE, K.C. (1986) Geochemistry and tectonic settings of early Proterozoic supracrustal rocks in the south western United States. The Journal of Geology, 94, 845-864. CONDIE, K.C. (1993) Chemical composition and evolution of the upper continental crust; contrasting results from surface samples and shales. Chemical Geology, 104 (1.4), 1-37. CONDIE, K.C. 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En Memoria de Elpidea Ocampo Casta
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Agradecimientos Al pueblo de Méxic
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Índice de Tablas TABLA 3. 1: PARÁ
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Abstract Mesozoic sedimentary seque
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El presente trabajo, por medio de a
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Durante las décadas de los 70s−8
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Terreno Sierra Madre muestra un bas
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unidades 2 y 3 de la Formación La
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102° W 26° N 25° N 102° W Falla
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Los estratos de arenisca son de gra
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Miembro Arenoso Galeana como un com
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2 ANÁLISIS DE FACIES, ASOCIACIONES
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GINGRAS et al. 1998; COATES y MACEA
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Cgn de manera erosiva y concordante
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La ausencia de estructuras sediment
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La asociación de la gradación nor
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La estratificación cruzada es el r
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Fig.2. 8: Fotografías de la facies
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Fig.2. 9: Fotografías de la Clase
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2.4.2 ASOCIACIÓN DE FACIES 2: CANA
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estratos muy delgados a delgados (F
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shoreface superior, cambiando later
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distributarios. El abandono tempora
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ioturbación va de BI 1-2. Ocasiona
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debe a que el ambiente es altamente
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Fig.2. 23: Fotografías de las estr
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Comparando los icnogéneros del fre
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2.4.10 ASOCIACIONES DE FACIES 10: P
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en las estructuras relacionadas con
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Tardío muestran cambios significat
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Los sistemas mixtos desarrollados e
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3 PETROGRAFÍA Y ÁREA FUENTE 1 3.1
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con el re-trabajamiento ocasionado
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Fig. 3. 3: Microfotografía de la P
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frecuentes, siendo en cambio frecue
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Fig. 3.6: Ensambles microfotográfi
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3.3.2.1.2 Subpetrofacies A2: Cuarzo
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conformado por: líticos tobaceos c
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acida ocurren en porcentajes bajos,
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3.3.3.1 Cuarzo BASU et al. (1975) y
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Los fragmentos líticos metapelíti
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Sin embargo, MCBRIDE y PICARD (1987
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4 GEOQUÍMICA: CLASIFICACIÓN, GRAD
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4.4 RESULTADOS 4.4.1 ELEMENTOS MAYO
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Adicionalmene a la Figura 4.1 y a l
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4.4.2.2 Resultado del análisis de
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principalmente a caolinita o ilita
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fragmentos de rocas volcánicas y p
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4.4); la abundancia de estos elemen
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fuentes ígneas félsicas. La conce
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crecimiento sintaxiales; (2) la alt
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de componentes sedimentarios antigu
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4.4.3.8 Grado de Intemperismo 4.4.3
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o de componentes máficos durante e
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empírico propuesto a partir de div
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(MERINO 1975; BJØRLYKKE 1983; CHIL
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Gv-15 Gv-14 Gv-13 Gv-12 Gv-11 Gv-10
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casos, el componente principal de m
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Gv-15 Gv-14 Gv-13 Gv-12 Gv-11 Gv-10
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LREE TiO 2 HREE 120 100 80 60 40 En
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Probabilidad Relativa 0.3 0.25 0.2
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5.3.7 POBLACIÓN DE GRANOS “G”:
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5.5 DISCUSIÓN SOBRE LA LOCALIZACI
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Conteo (Corregido con el Bg) 1. la
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Los cuarzos con bordes de crecimien
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Según AUGUSTSSON (2003) y AUGUSTSS
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AITCHISON et al. 2000; WELTJE 2002)
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(Figuras 6.8 y 6.9 y Tabla 6.1), se
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6.4.1 CUARZO PLUTÓNICO (AZUL MEDIO
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Sc_19 Sc_16 Sc_12 Sc_10 Sc_7 Sc_2 R
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7 ANÁLISIS DE PROCEDENCIA El prese
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sur de la Fosa de Monterrey registr
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A B a 1 implican el reciclamiento o
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derivaron de rocas de composición
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C continentales con el 99% de confi
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de los cuarzos que presentan lumini
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San Rafael Chorros Huasteca Picacho
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C petrofacies A que comprenden a la
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Muestr a ODY Z-05- 06- 08-5 ODY Z-0
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Mues tra ODY Z- 06.06 .2005 -11 ODY
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Mues tra ODY Z- 24.02 .2005 -12 ODY
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APÉNDICES DEL CAPÍTULO 5 Análisi
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Análisis U (ppm) 206 Pb/ 204 Pb U/
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Análisis U (ppm) 206 Pb/ 204 Pb U/
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Análisis petrográfico y estadíst
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La Casita Fomation is represented b
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Madre presenta como basamento rocas
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metodología de Gazzi-Zuffa modific
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Patula (8%, “Arcosa Patula; 5%, F
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mientras que las muestras de la For
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dentro del CP2 indican procedencias
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presentan una afinidad con arcos di
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Atkinson, A.C., Riani, M., Cerioli,
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Egozcue, J. J., Pawlowsky-Glahn, V.
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Oklahoma, Society of Economic Paleo
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von Eynatten, H., Barceló-Vidal, C
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Figuras 102° W 101° W 100° W 26
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Figura 3: (Ocampo-Díaz, 2009) 27
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a 13 F b 45 Basamento Levantado Bas
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Rg Rp a Leyenda b Rs Rm Figura 7: (
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CP 2 : 20.34% CP 4 : 7.63% 1.0 0.5
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ln (Q/F) 8 6 4 2 0 -2 -2 Índice de
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Resumen La columna estratigráfica
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dentro de la Fosa de Monterrey. Est
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laminaciones onduladas. El espesor
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Los parámetros que conforman el
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cristalinas. Lo anterior se asocia
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4.4.3 Caso 3: Aplicación del InReS
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posibles procesos de reciclado y ca
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Sedimentary and Tectonic history of
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Lista de Figuras Figura 1. Columna
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102° W 101° W 100° W 26° N 25°
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Cratón interior Transicional conti
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Simbología Estratificación Flaser
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A B A InReSe 0.2 0.3 0.4 0.5 0.6 0.
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Petrografía y procedencia de las a
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This paper, is based on a rigorous
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conglomeráticas, rocas carbonatada
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divididas en tres petrofacies disti
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El soporte al área fuente de compo
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metapsamíticos/felsíticos3; (3) l
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Mexico Basin: Tectonics, Sedimentar
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Garzanti, E., Vezzoli, G., Andò, S
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Michalzik, D., 1986, Stratigraphy a
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cuarzo monocristlino (R23); (E) Arc
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Figura 2. Ocampo-Díaz et al., 2010
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Figura 4. Ocampo-Díaz et al., 2010
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Figura 6. Ocampo-Díaz et al., 2010
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Figura 8. Ocampo-Díaz et al., 2010
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Figura 10. Ocampo-Díaz et al., 201
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Figura 12. Ocampo-Díaz et al., 201
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Figura 14. Ocampo-Díaz et al., 201