Field analogues of shallow-water hydrocarbon seepages in the Pleistocene Argille Azzurre Formation

the chimneys field of Enza River, Northern Apennines, Italy

Davide Oppo, Rossella Capozzi, Enrico Dinelli, Alessandra Negri, Paolo Montagna, Vincenzo Picotti, S. Scarponi, Marco Taviani

Research output: Contribution to conferencePoster

Abstract

The geologically young Northern Apennines contain various natural seeps documenting a variability of reservoirs and fluids in terms of origin, age and evolution. Hydrocarbon and saline water seepages are controlled by the structures of the chain and the foredeep. In the geological record, the witness of these natural seepages are represented by authigenic carbonates. Their isotopic content allows to understand the carbon source and the processes of carbonate precipitation. The better known regional examples of Methane Derived Authigenic Carbonates (MDAC) and chemoherm build-ups, clustered in the Upper Miocene and Lower-Upper Pliocene successions, are formed in deep water (> 300 m) sediments. Occurrences in shallow water (shelf) settings have never been reported. Our case study describes the palisade chimneys field, recently exposed along the Enza riverbanks in the Northern Apennines in the Argille Azzurre Formation (blue mudstones) of Pleistocene age. The paleontological content (mainly bivalves) documents that this unit was deposited in an open marine muddy shelfal setting, in a bathymetric range of about 50-70 m, with local anoxic condition, documented by benthic foraminifer assemblages. The succession is biostratigraphically dated at the Early Pleistocene (Calabrian, nannoplancton zone MNN19e). A number of subvertical, metric-high columnar chimneys, ranging in diameter from 10 to 35 cm, in association with discontinuous planar carbonate concretions, intervening along the bedding planes, outcrop within the mudstones. Such concretions are clearly formed by the moderate cementation of the hosting pelitic sediments. The tubular concretions show central conduits running along the whole length, locally filled by sediments. The grain size within the concretions is homogeneous, both in the chimneys and planar concretions and irrespective of the bedding planes, suggesting a process of transport and homogenization prior to the cementation. Within the Enza river succession, some gas leakage still occurs, showing δ13C isotopic values of about -70‰, indicating a biogenic origin of the methane, generated within the Plio-Pleistocene mudstones. On the contrary, numerous hydrocarbon seepages along the same Northern Apennines foothills are characterized by thermogenic methane, generated at greater depth and presently trapped within Tertiary reservoirs. This documents the role of the different geologic context as the main control on gas generation and migration. The on-going research is focused on the petrographic, geochemical and biogeochemical characteristics of these concretions to unravel the different fluids involved in their formation, their concretioning modality and the fluid flow history.
Original languageEnglish
Publication statusPublished - Dec 2012
Event2012 AGU Fall Meeting - San Francisco, United States
Duration: 3 Dec 20127 Dec 2012

Conference

Conference2012 AGU Fall Meeting
CountryUnited States
CitySan Francisco
Period3/12/127/12/12

Fingerprint

concretion
seepage
shallow water
Pleistocene
hydrocarbon
river
mudstone
carbonate
bedding plane
methane
cementation
sediment
Calabrian
fluid
forearc basin
geological record
benthic foraminifera
gas
anoxic conditions
leakage

Cite this

Oppo, D., Capozzi, R., Dinelli, E., Negri, A., Montagna, P., Picotti, V., ... Taviani, M. (2012). Field analogues of shallow-water hydrocarbon seepages in the Pleistocene Argille Azzurre Formation: the chimneys field of Enza River, Northern Apennines, Italy. Poster session presented at 2012 AGU Fall Meeting , San Francisco, United States.

Field analogues of shallow-water hydrocarbon seepages in the Pleistocene Argille Azzurre Formation : the chimneys field of Enza River, Northern Apennines, Italy. / Oppo, Davide; Capozzi, Rossella; Dinelli, Enrico; Negri, Alessandra; Montagna, Paolo; Picotti, Vincenzo; Scarponi, S.; Taviani, Marco.

2012. Poster session presented at 2012 AGU Fall Meeting , San Francisco, United States.

Research output: Contribution to conferencePoster

Oppo, D, Capozzi, R, Dinelli, E, Negri, A, Montagna, P, Picotti, V, Scarponi, S & Taviani, M 2012, 'Field analogues of shallow-water hydrocarbon seepages in the Pleistocene Argille Azzurre Formation: the chimneys field of Enza River, Northern Apennines, Italy' 2012 AGU Fall Meeting , San Francisco, United States, 3/12/12 - 7/12/12, .
Oppo D, Capozzi R, Dinelli E, Negri A, Montagna P, Picotti V et al. Field analogues of shallow-water hydrocarbon seepages in the Pleistocene Argille Azzurre Formation: the chimneys field of Enza River, Northern Apennines, Italy. 2012. Poster session presented at 2012 AGU Fall Meeting , San Francisco, United States.
Oppo, Davide ; Capozzi, Rossella ; Dinelli, Enrico ; Negri, Alessandra ; Montagna, Paolo ; Picotti, Vincenzo ; Scarponi, S. ; Taviani, Marco. / Field analogues of shallow-water hydrocarbon seepages in the Pleistocene Argille Azzurre Formation : the chimneys field of Enza River, Northern Apennines, Italy. Poster session presented at 2012 AGU Fall Meeting , San Francisco, United States.
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abstract = "The geologically young Northern Apennines contain various natural seeps documenting a variability of reservoirs and fluids in terms of origin, age and evolution. Hydrocarbon and saline water seepages are controlled by the structures of the chain and the foredeep. In the geological record, the witness of these natural seepages are represented by authigenic carbonates. Their isotopic content allows to understand the carbon source and the processes of carbonate precipitation. The better known regional examples of Methane Derived Authigenic Carbonates (MDAC) and chemoherm build-ups, clustered in the Upper Miocene and Lower-Upper Pliocene successions, are formed in deep water (> 300 m) sediments. Occurrences in shallow water (shelf) settings have never been reported. Our case study describes the palisade chimneys field, recently exposed along the Enza riverbanks in the Northern Apennines in the Argille Azzurre Formation (blue mudstones) of Pleistocene age. The paleontological content (mainly bivalves) documents that this unit was deposited in an open marine muddy shelfal setting, in a bathymetric range of about 50-70 m, with local anoxic condition, documented by benthic foraminifer assemblages. The succession is biostratigraphically dated at the Early Pleistocene (Calabrian, nannoplancton zone MNN19e). A number of subvertical, metric-high columnar chimneys, ranging in diameter from 10 to 35 cm, in association with discontinuous planar carbonate concretions, intervening along the bedding planes, outcrop within the mudstones. Such concretions are clearly formed by the moderate cementation of the hosting pelitic sediments. The tubular concretions show central conduits running along the whole length, locally filled by sediments. The grain size within the concretions is homogeneous, both in the chimneys and planar concretions and irrespective of the bedding planes, suggesting a process of transport and homogenization prior to the cementation. Within the Enza river succession, some gas leakage still occurs, showing δ13C isotopic values of about -70‰, indicating a biogenic origin of the methane, generated within the Plio-Pleistocene mudstones. On the contrary, numerous hydrocarbon seepages along the same Northern Apennines foothills are characterized by thermogenic methane, generated at greater depth and presently trapped within Tertiary reservoirs. This documents the role of the different geologic context as the main control on gas generation and migration. The on-going research is focused on the petrographic, geochemical and biogeochemical characteristics of these concretions to unravel the different fluids involved in their formation, their concretioning modality and the fluid flow history.",
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T2 - the chimneys field of Enza River, Northern Apennines, Italy

AU - Oppo, Davide

AU - Capozzi, Rossella

AU - Dinelli, Enrico

AU - Negri, Alessandra

AU - Montagna, Paolo

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AU - Scarponi, S.

AU - Taviani, Marco

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N2 - The geologically young Northern Apennines contain various natural seeps documenting a variability of reservoirs and fluids in terms of origin, age and evolution. Hydrocarbon and saline water seepages are controlled by the structures of the chain and the foredeep. In the geological record, the witness of these natural seepages are represented by authigenic carbonates. Their isotopic content allows to understand the carbon source and the processes of carbonate precipitation. The better known regional examples of Methane Derived Authigenic Carbonates (MDAC) and chemoherm build-ups, clustered in the Upper Miocene and Lower-Upper Pliocene successions, are formed in deep water (> 300 m) sediments. Occurrences in shallow water (shelf) settings have never been reported. Our case study describes the palisade chimneys field, recently exposed along the Enza riverbanks in the Northern Apennines in the Argille Azzurre Formation (blue mudstones) of Pleistocene age. The paleontological content (mainly bivalves) documents that this unit was deposited in an open marine muddy shelfal setting, in a bathymetric range of about 50-70 m, with local anoxic condition, documented by benthic foraminifer assemblages. The succession is biostratigraphically dated at the Early Pleistocene (Calabrian, nannoplancton zone MNN19e). A number of subvertical, metric-high columnar chimneys, ranging in diameter from 10 to 35 cm, in association with discontinuous planar carbonate concretions, intervening along the bedding planes, outcrop within the mudstones. Such concretions are clearly formed by the moderate cementation of the hosting pelitic sediments. The tubular concretions show central conduits running along the whole length, locally filled by sediments. The grain size within the concretions is homogeneous, both in the chimneys and planar concretions and irrespective of the bedding planes, suggesting a process of transport and homogenization prior to the cementation. Within the Enza river succession, some gas leakage still occurs, showing δ13C isotopic values of about -70‰, indicating a biogenic origin of the methane, generated within the Plio-Pleistocene mudstones. On the contrary, numerous hydrocarbon seepages along the same Northern Apennines foothills are characterized by thermogenic methane, generated at greater depth and presently trapped within Tertiary reservoirs. This documents the role of the different geologic context as the main control on gas generation and migration. The on-going research is focused on the petrographic, geochemical and biogeochemical characteristics of these concretions to unravel the different fluids involved in their formation, their concretioning modality and the fluid flow history.

AB - The geologically young Northern Apennines contain various natural seeps documenting a variability of reservoirs and fluids in terms of origin, age and evolution. Hydrocarbon and saline water seepages are controlled by the structures of the chain and the foredeep. In the geological record, the witness of these natural seepages are represented by authigenic carbonates. Their isotopic content allows to understand the carbon source and the processes of carbonate precipitation. The better known regional examples of Methane Derived Authigenic Carbonates (MDAC) and chemoherm build-ups, clustered in the Upper Miocene and Lower-Upper Pliocene successions, are formed in deep water (> 300 m) sediments. Occurrences in shallow water (shelf) settings have never been reported. Our case study describes the palisade chimneys field, recently exposed along the Enza riverbanks in the Northern Apennines in the Argille Azzurre Formation (blue mudstones) of Pleistocene age. The paleontological content (mainly bivalves) documents that this unit was deposited in an open marine muddy shelfal setting, in a bathymetric range of about 50-70 m, with local anoxic condition, documented by benthic foraminifer assemblages. The succession is biostratigraphically dated at the Early Pleistocene (Calabrian, nannoplancton zone MNN19e). A number of subvertical, metric-high columnar chimneys, ranging in diameter from 10 to 35 cm, in association with discontinuous planar carbonate concretions, intervening along the bedding planes, outcrop within the mudstones. Such concretions are clearly formed by the moderate cementation of the hosting pelitic sediments. The tubular concretions show central conduits running along the whole length, locally filled by sediments. The grain size within the concretions is homogeneous, both in the chimneys and planar concretions and irrespective of the bedding planes, suggesting a process of transport and homogenization prior to the cementation. Within the Enza river succession, some gas leakage still occurs, showing δ13C isotopic values of about -70‰, indicating a biogenic origin of the methane, generated within the Plio-Pleistocene mudstones. On the contrary, numerous hydrocarbon seepages along the same Northern Apennines foothills are characterized by thermogenic methane, generated at greater depth and presently trapped within Tertiary reservoirs. This documents the role of the different geologic context as the main control on gas generation and migration. The on-going research is focused on the petrographic, geochemical and biogeochemical characteristics of these concretions to unravel the different fluids involved in their formation, their concretioning modality and the fluid flow history.

M3 - Poster

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