Zobrazeno 1 - 10 of 14 pro vyhledávání: '"Debritas"'
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Akademický článek
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Contornitas y depósitos gravitativos del drift de Faro (Golfo de Cádiz): áreas fuente
Autor: Alonso, Belén, Ercilla, Gemma, Casas, David, Stow, D. A. V., Rodríguez Tovar, Francisco J., Dorador, Javier, Hernández-Molina, Francisco J.
Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
instname
IX Congreso Geológico de España, 12-14 septiembre 2016, Huelva.-- 4 pages, 4 figures
[EN] The Pleistocene deposits of the Faro Drift at sites U1386 and U1387 with IODP 339 Exp. 339 have been examined to characterize: a) their lithofacies, b) f
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0b1cc4a64c39603324ae340fdf775037
http://hdl.handle.net/10261/160248
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3
Akademický článek
La Formación Chivillas en Tehuacán, Puebla, México: definición, análisis de facies y procedencia.
Autor: Mendoza-Rosales, Claudia Cristina1 claus@unam.mx, Silva-Romo, Gilberto1, Centeno-García, Elena2, Campos-Madrigal, Emiliano1, Rodríguez-Otero, Mónica1
Publikováno v: Boletín de la Sociedad Geológica Mexicana. 2013, Vol. 65 Issue 3, p457-480. 24p.
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5
La Formación Chivillas en Tehuacán, Puebla, México: definición, análisis de facies y procedencia
Autor: Claudia C. Mendoza-Rosales, Elena Centeno-García, Mónica Rodríguez-Otero, Emiliano Campos-Madrigal, Gilberto Silva-Romo
Publikováno v: Universidad Nacional Autónoma de México
UNAM
Redalyc-UNAM
Boletín de la Sociedad Geológica Mexicana (México) Num.3 Vol.65
Redalyc
"Se propone formalmente a la Formación Chivillas, unidad litoestratigráfica clave para descifrar el registro sedimentario de la Cuenca Cuicateca. Su localidad tipo se encuentra en la Barranca Las Salinas al noreste de Tehuacán, donde las rocas est
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d78f9acfd86efce6842a57f3a4541fc5
https://www.redalyc.org/articulo.oa?id=94329954003
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6
Tips on the SW-Gondwana margin: Ordovician conodont-graptolite biostratigraphy of allochthonous blocks in the Rinconada mélange, Argentine Precordillera
Autor: Voldman, Gustavo G., Alonso, Juan L., Fernández, Luis P., Ortega, Gladys, Albanesi, Guillermo L., Banchig, Aldo L., Cardó, Raúl
Publikováno v: Andean geology, Volume: 45, Issue: 3, Pages: 399-409, Published: 2018
The Rinconada Formation is a mélange that crops out in the eastern margin of the Argentine Precordillera, an exotic terrane accreted to Gondwana in Ordovician times. Its gravity-driven deposits have been studied by means of conodont and graptolite b
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______614::7a785bdcccfe0750700e1a26c94d6b24
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062018000300399&lng=en&tlng=en
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7
Tips on the SW-Gondwana margin: Ordovician conodont-graptolite biostratigraphy of allochthonous blocks in the Rinconada melange, Argentine Precordillera
Autor: Luis Pedro Fernández, Guillermo L. Albanesi, Aldo Lui Banchig, Gladys Ortega, Gustavo Gabriel Voldman, Raúl Cardó, Juan Luis Alonso Alonso
Publikováno v: WOS:000449464900006
Andean geology v.45 n.3 2018
SciELO Chile
CONICYT Chile
instacron:CONICYT
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
The Rinconada Formation is a mélange that crops out in the eastern margin of the Argentine Precordillera, an exotic terrane accreted to Gondwana in Ordovician times. Its gravity-driven deposits have been studied by means of conodont and graptolite b
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3e0d0776cb3b703ef69f500028076ddb
http://hdl.handle.net/10651/50760
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8
Characterization of the Ophiomorpha rudis 3D boxwork in a turbiditic succession (Oligocene of the Alicante Province, southeastern Spain)
Autor: Alice Giannetti, Santiago Falces Delgado, Paolo Monaco
Purpose: Slope-associated ichnoassemblages show great variability according to the physiography of the platform-slope system, sedimentary taxa and nutrient input. Ophiomorpha rudis uses to be common in turbiditic successions, therefore its detailed c
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::38fea392f9a439ba37d51d5cffea8f90
http://hdl.handle.net/11391/1421475
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9
Depósitos de flujos de sedimentos por densidad en la transición canal-lóbulo submarino: un ejemplo del Tortoniense superior de la Cuenca de Sorbas, SE España
Autor: Carrión Torrente, Álvaro, Puga Bernabéu, Ángel
The subaqueous sediment density flows (SDF) in Mizala (Sorbas Basin, SE Spain) were deposited during the late Tortonian in a middle submarine fan system, near the channel-lobe transition zone. Channel and lobe deposits comprise 6 facies types interpr
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______1388::f4d2c29b9c5b34eb6b2969d91cd9f6fc
https://hdl.handle.net/10272/13602
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10
Sediment density flow deposits at the channel-lobe transition zone: an example from late Tortonian of the Sorbas Basin, SE Spain
Autor: Carrión Torrente, Álvaro, Puga Bernabéu, Ángel
Publikováno v: Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
The subaqueous sediment density flows (SDF) in Mizala (Sorbas Basin, SE Spain) were deposited during the late Tortonian in a middle submarine fan system, near the channel-lobe transition zone. Channel and lobe deposits comprise 6 facies types interpr
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::f4d2c29b9c5b34eb6b2969d91cd9f6fc
http://hdl.handle.net/10272/13602
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