Paleo-earthquakes in passive-margin settings, an example from the Paleocene of the Golfo San Jorge Basin, Argentina
Paleocene sedimentary rocks in the Golfo San Jorge Basin include the marine Salamanca Formation and the continental Río Chico Formation. Both units contain soft-sediment deformation features and evidence of contemporary tectonics, which include: 1) sediment-filled fissures, hosted in muddy marine se...
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| Published in: | Sedimentary geology Vol. 205; no. 1; pp. 67 - 78 |
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| Format: | Journal Article |
| Language: | English |
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30-03-2008
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| Abstract | Paleocene sedimentary rocks in the Golfo San Jorge Basin include the marine Salamanca Formation and the continental Río Chico Formation. Both units contain soft-sediment deformation features and evidence of contemporary tectonics, which include: 1) sediment-filled fissures, hosted in muddy marine sediments of the Salamanca Formation (“Fragmentosa” Section), where the sandy infill of the fissures took place from above; 2) synsedimentary normal faults in the uppermost levels of the Salamanca Formation, with vertical throws rarely exceeding 1 m; 3) fault-graded beds in the “Banco Negro Inferior” (marine–continental transition), which show a deformed sequence with small-scale normal faults at the bottom and intraformational breccias on top; and 4) liquefaction and/or fluidization pillars, “V” or funnel-shaped, with vertical extension of up to 5 m and preserved into fluvial channels of the Río Chico Formation. Deformed strata are bounded by undisturbed horizons and some of these features can be correlated along 60 km of exposures.
The suite of soft-sediment deformation structures is considered a secondary evidence of synsedimentary paleo-earthquakes (seismites) in this portion of the South American passive margin. This work shows new evidence of syndepositional tectonic activity in the lowermost Paleogene of the Golfo San Jorge Basin. |
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| AbstractList | Paleocene sedimentary rocks in the Golfo San Jorge Basin include the marine Salamanca Formation and the continental Río Chico Formation. Both units contain soft-sediment deformation features and evidence of contemporary tectonics, which include: 1) sediment-filled fissures, hosted in muddy marine sediments of the Salamanca Formation (“Fragmentosa” Section), where the sandy infill of the fissures took place from above; 2) synsedimentary normal faults in the uppermost levels of the Salamanca Formation, with vertical throws rarely exceeding 1 m; 3) fault-graded beds in the “Banco Negro Inferior” (marine–continental transition), which show a deformed sequence with small-scale normal faults at the bottom and intraformational breccias on top; and 4) liquefaction and/or fluidization pillars, “V” or funnel-shaped, with vertical extension of up to 5 m and preserved into fluvial channels of the Río Chico Formation. Deformed strata are bounded by undisturbed horizons and some of these features can be correlated along 60 km of exposures.
The suite of soft-sediment deformation structures is considered a secondary evidence of synsedimentary paleo-earthquakes (seismites) in this portion of the South American passive margin. This work shows new evidence of syndepositional tectonic activity in the lowermost Paleogene of the Golfo San Jorge Basin. Paleocene sedimentary rocks in the Golfo San Jorge Basin include the marine Salamanca Formation and the continental Rio Chico Formation. Both units contain soft-sediment deformation features and evidence of contemporary tectonics, which include: 1) sediment-filled fissures, hosted in muddy marine sediments of the Salamanca Formation (''Fragmentosa'' Section), where the sandy infill of the fissures took place from above; 2) synsedimentary normal faults in the uppermost levels of the Salamanca Formation, with vertical throws rarely exceeding 1 m; 3) fault-graded beds in the ''Banco Negro Inferior'' (marine-continental transition), which show a deformed sequence with small-scale normal faults at the bottom and intraformational breccias on top; and 4) liquefaction and/or fluidization pillars, ''V'' or funnel-shaped, with vertical extension of up to 5 m and preserved into fluvial channels of the Rio Chico Formation. Deformed strata are bounded by undisturbed horizons and some of these features can be correlated along 60 km of exposures. The suite of soft-sediment deformation structures is considered a secondary evidence of synsedimentary paleo-earthquakes (seismites) in this portion of the South American passive margin. This work shows new evidence of syndepositional tectonic activity in the lowermost Paleogene of the Golfo San Jorge Basin. |
| Author | Foix, Nicolás Paredes, José M. Giacosa, Raúl E. |
| Author_xml | – sequence: 1 givenname: Nicolás surname: Foix fullname: Foix, Nicolás email: nicofoix@unpata.edu.ar organization: Departamento de Geología, Facultad de Ciencias Naturales, Universidad Nacional de la Patagonia “San Juan Bosco”, Ruta Prov. Nº 1 Km 4 , Comodoro Rivadavia, Chubut, Argentina – sequence: 2 givenname: José M. surname: Paredes fullname: Paredes, José M. organization: Departamento de Geología, Facultad de Ciencias Naturales, Universidad Nacional de la Patagonia “San Juan Bosco”, Ruta Prov. Nº 1 Km 4 , Comodoro Rivadavia, Chubut, Argentina – sequence: 3 givenname: Raúl E. surname: Giacosa fullname: Giacosa, Raúl E. organization: Departamento de Geología, Facultad de Ciencias Naturales, Universidad Nacional de la Patagonia “San Juan Bosco”, Ruta Prov. Nº 1 Km 4 , Comodoro Rivadavia, Chubut, Argentina |
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| Keywords | Golfo San Jorge Basin South American passive margin Synsedimentary normal faults Ancient seismites Paleocene |
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| Snippet | Paleocene sedimentary rocks in the Golfo San Jorge Basin include the marine Salamanca Formation and the continental Río Chico Formation. Both units contain... Paleocene sedimentary rocks in the Golfo San Jorge Basin include the marine Salamanca Formation and the continental Rio Chico Formation. Both units contain... |
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| Title | Paleo-earthquakes in passive-margin settings, an example from the Paleocene of the Golfo San Jorge Basin, Argentina |
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