Artículo

Beresi, M.S.; Cabaleri, N.G.; Buitrón-Sánchez, B.E.; Cecilia Rodríguez, M.; Heredia, S.E.; Franco Tortello, M. "Microfacies, biota y paleoambientes sedimentarios del Ordovícico temprano-medio del cerro salazar, Sonora central, México" (2012) Revista Mexicana de Ciencias Geologicas. 29(2):330-345
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Abstract:

This work shows the results of facies/microfacies and paleoenvironmental analysis of the Pozo Nuevo Formation outcropping at the Cerro Salazar, nearby the Rancho Las Norias (Central Sonora, Mexico). The Pozo Nuevo Formation represents Early-Middle Ordovician deposits of a continental carbonate shelf that developed in the southwestern tip of Laurentia. The conodonts and trilobites described from the unit indicate a late Floian-early Dapingian age. The microfacies analysis enables identifying different sub-environments within the carbonate shelf from minor to major depth: a coastal beach, represented by quartz sandstone and laminated quartzite with desiccation cracks; an inner shelf which includes a supratidal setting constituted by dolomitized wackestone and an intertidal-subtidal lagoon characterized by diffusely laminated microbialites, oncoid mudstone, pelloid packstone grading to biopelloid and bioclastic packstone containing foraminifera and ostracods; and a subtidal setting composed of grainstone and packstone with crinoids and algae (Nuia) and detritic quartz and bioclastic packstone with bryozoans. In the lagoon as well as in the subtidal platform, there are intercalated intraclastic - bioclastic packstone levels, which are interpreted as proximal stormy events. The vertical variation of facies indicates a marked trend toward shallowing. At the base of the section fine micritic sediments deposited in a quiet, low energy lagoon, whereas a deeper subtidal environment with diverse faunas was developed in the middle part. On the other hand, at the top of the succession there is an increased participation of detrital quartz with deposition of coastal quartz sandstone culminating with thick dolomite levels of a vadose environment.

Registro:

Documento: Artículo
Título:Microfacies, biota y paleoambientes sedimentarios del Ordovícico temprano-medio del cerro salazar, Sonora central, México
Autor:Beresi, M.S.; Cabaleri, N.G.; Buitrón-Sánchez, B.E.; Cecilia Rodríguez, M.; Heredia, S.E.; Franco Tortello, M.
Filiación:Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), Consejo Nacional de Investigaciones Científicas y Tecnológicas (CONICET), Av. A. Ruiz Leal s/n, Parque Gral, San Martín, 5500, Mendoza, Argentina
Instituto de Geocronología y Geología Isotópica (INGEIS), Universidad de Buenos Aires (UBA), CONICET, Ciudad Universitaria C1428EGA, Intendente Güiraldes 2160, Ciudad Autónoma de Buenos Aires, Argentina
Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, 04510, México D.F, Mexico
CONICET- Instituto de Investigaciones Mineras, Facultad de Ingeniería, Universidad Nacional de San Juan, Urquiza y Libertador, (5400) San Juan, Argentina
CONICET - Dpto. Paleontología Invertebrados, Museo de La Plata, Paseo del Bosque (B1900FWA), La Plata, Argentina
Palabras clave:Central sonora; Mexico; Microfacies; Ordovician; Paleoenvironments
Año:2012
Volumen:29
Número:2
Página de inicio:330
Página de fin:345
Título revista:Revista Mexicana de Ciencias Geologicas
Título revista abreviado:Rev. Mex. Cienc. Geol.
ISSN:10268774
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_10268774_v29_n2_p330_Beresi

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Citas:

---------- APA ----------
Beresi, M.S., Cabaleri, N.G., Buitrón-Sánchez, B.E., Cecilia Rodríguez, M., Heredia, S.E. & Franco Tortello, M. (2012) . Microfacies, biota y paleoambientes sedimentarios del Ordovícico temprano-medio del cerro salazar, Sonora central, México. Revista Mexicana de Ciencias Geologicas, 29(2), 330-345.
Recuperado de https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_10268774_v29_n2_p330_Beresi [ ]
---------- CHICAGO ----------
Beresi, M.S., Cabaleri, N.G., Buitrón-Sánchez, B.E., Cecilia Rodríguez, M., Heredia, S.E., Franco Tortello, M. "Microfacies, biota y paleoambientes sedimentarios del Ordovícico temprano-medio del cerro salazar, Sonora central, México" . Revista Mexicana de Ciencias Geologicas 29, no. 2 (2012) : 330-345.
Recuperado de https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_10268774_v29_n2_p330_Beresi [ ]
---------- MLA ----------
Beresi, M.S., Cabaleri, N.G., Buitrón-Sánchez, B.E., Cecilia Rodríguez, M., Heredia, S.E., Franco Tortello, M. "Microfacies, biota y paleoambientes sedimentarios del Ordovícico temprano-medio del cerro salazar, Sonora central, México" . Revista Mexicana de Ciencias Geologicas, vol. 29, no. 2, 2012, pp. 330-345.
Recuperado de https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_10268774_v29_n2_p330_Beresi [ ]
---------- VANCOUVER ----------
Beresi, M.S., Cabaleri, N.G., Buitrón-Sánchez, B.E., Cecilia Rodríguez, M., Heredia, S.E., Franco Tortello, M. Microfacies, biota y paleoambientes sedimentarios del Ordovícico temprano-medio del cerro salazar, Sonora central, México. Rev. Mex. Cienc. Geol. 2012;29(2):330-345.
Available from: https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_10268774_v29_n2_p330_Beresi [ ]