A new age model for the middle Eocene deep-marine Ainsa Basin, Spanish Pyrenees
The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for th...
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| Autor*in: |
JI Scotchman [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Rechteinformationen: |
Nutzungsrecht: © COPYRIGHT 2015 Elsevier Science Publishers |
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| Systematik: |
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| Übergeordnetes Werk: |
Enthalten in: Earth science reviews - Amsterdam [u.a.] : Elsevier, 1966, 144(2015), Seite 10-22 |
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| Übergeordnetes Werk: |
volume:144 ; year:2015 ; pages:10-22 |
| Links: |
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| DOI / URN: |
10.1016/j.earscirev.2014.11.006 |
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| 520 | |a The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for the submarine fan and related deposits. Here, we present a new composite basin stratigraphy based upon biostratigraphic analyses of the Upper Hecho Group submarine-fan and interfan deposits. Calcareous nannofossil data suggest that deposition of the Gerbe through to Guaso systems occurred during biozones NP14-16 (42.6 and 48.9 Ma based on our age model). Additional biostratigraphic ages from the Lower Hecho Group suggest that the entire Hecho Group no older than biozone NP13 (~ 51 Ma). The improved chronostratigraphic control enables correlations between submarine canyons and submarine-fans of the Ainsa and Jaca basins to be assessed. Our new age model provides a means of comparison of stratigraphic events with regional sections allowing a better understanding of the lateral and temporal evolution of these depositional systems from source-to-sink. | ||
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10.1016/j.earscirev.2014.11.006 doi PQ20160617 (DE-627)OLC1967858551 (DE-599)GBVOLC1967858551 (PRQ)c1822-43b4817eab2a89553bbb453b28c6f64975d6229ec8fd68de702cf7888e618d460 (KEY)0080876820150000144000000010newagemodelforthemiddleeocenedeepmarineainsabasins DE-627 ger DE-627 rakwb eng 070 550 DNB RA 1000 AVZ rvk JI Scotchman verfasserin aut A new age model for the middle Eocene deep-marine Ainsa Basin, Spanish Pyrenees 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for the submarine fan and related deposits. Here, we present a new composite basin stratigraphy based upon biostratigraphic analyses of the Upper Hecho Group submarine-fan and interfan deposits. Calcareous nannofossil data suggest that deposition of the Gerbe through to Guaso systems occurred during biozones NP14-16 (42.6 and 48.9 Ma based on our age model). Additional biostratigraphic ages from the Lower Hecho Group suggest that the entire Hecho Group no older than biozone NP13 (~ 51 Ma). The improved chronostratigraphic control enables correlations between submarine canyons and submarine-fans of the Ainsa and Jaca basins to be assessed. Our new age model provides a means of comparison of stratigraphic events with regional sections allowing a better understanding of the lateral and temporal evolution of these depositional systems from source-to-sink. Nutzungsrecht: © COPYRIGHT 2015 Elsevier Science Publishers Rocks, Sedimentary Basins (Geology) Submarine valleys Analysis Stratigraphy Sedimentary geology Basins Rocks Evolution P Bown oth KT Pickering oth M BouDagher-Fadel oth NJ Bayliss oth SA Robinson oth Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 144(2015), Seite 10-22 (DE-627)129069752 (DE-600)1792-9 (DE-576)014401525 0012-8252 nnns volume:144 year:2015 pages:10-22 http://dx.doi.org/10.1016/j.earscirev.2014.11.006 Volltext http://search.proquest.com/docview/1681501022 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_4028 RA 1000 AR 144 2015 10-22 |
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10.1016/j.earscirev.2014.11.006 doi PQ20160617 (DE-627)OLC1967858551 (DE-599)GBVOLC1967858551 (PRQ)c1822-43b4817eab2a89553bbb453b28c6f64975d6229ec8fd68de702cf7888e618d460 (KEY)0080876820150000144000000010newagemodelforthemiddleeocenedeepmarineainsabasins DE-627 ger DE-627 rakwb eng 070 550 DNB RA 1000 AVZ rvk JI Scotchman verfasserin aut A new age model for the middle Eocene deep-marine Ainsa Basin, Spanish Pyrenees 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for the submarine fan and related deposits. Here, we present a new composite basin stratigraphy based upon biostratigraphic analyses of the Upper Hecho Group submarine-fan and interfan deposits. Calcareous nannofossil data suggest that deposition of the Gerbe through to Guaso systems occurred during biozones NP14-16 (42.6 and 48.9 Ma based on our age model). Additional biostratigraphic ages from the Lower Hecho Group suggest that the entire Hecho Group no older than biozone NP13 (~ 51 Ma). The improved chronostratigraphic control enables correlations between submarine canyons and submarine-fans of the Ainsa and Jaca basins to be assessed. Our new age model provides a means of comparison of stratigraphic events with regional sections allowing a better understanding of the lateral and temporal evolution of these depositional systems from source-to-sink. Nutzungsrecht: © COPYRIGHT 2015 Elsevier Science Publishers Rocks, Sedimentary Basins (Geology) Submarine valleys Analysis Stratigraphy Sedimentary geology Basins Rocks Evolution P Bown oth KT Pickering oth M BouDagher-Fadel oth NJ Bayliss oth SA Robinson oth Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 144(2015), Seite 10-22 (DE-627)129069752 (DE-600)1792-9 (DE-576)014401525 0012-8252 nnns volume:144 year:2015 pages:10-22 http://dx.doi.org/10.1016/j.earscirev.2014.11.006 Volltext http://search.proquest.com/docview/1681501022 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_4028 RA 1000 AR 144 2015 10-22 |
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10.1016/j.earscirev.2014.11.006 doi PQ20160617 (DE-627)OLC1967858551 (DE-599)GBVOLC1967858551 (PRQ)c1822-43b4817eab2a89553bbb453b28c6f64975d6229ec8fd68de702cf7888e618d460 (KEY)0080876820150000144000000010newagemodelforthemiddleeocenedeepmarineainsabasins DE-627 ger DE-627 rakwb eng 070 550 DNB RA 1000 AVZ rvk JI Scotchman verfasserin aut A new age model for the middle Eocene deep-marine Ainsa Basin, Spanish Pyrenees 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for the submarine fan and related deposits. Here, we present a new composite basin stratigraphy based upon biostratigraphic analyses of the Upper Hecho Group submarine-fan and interfan deposits. Calcareous nannofossil data suggest that deposition of the Gerbe through to Guaso systems occurred during biozones NP14-16 (42.6 and 48.9 Ma based on our age model). Additional biostratigraphic ages from the Lower Hecho Group suggest that the entire Hecho Group no older than biozone NP13 (~ 51 Ma). The improved chronostratigraphic control enables correlations between submarine canyons and submarine-fans of the Ainsa and Jaca basins to be assessed. Our new age model provides a means of comparison of stratigraphic events with regional sections allowing a better understanding of the lateral and temporal evolution of these depositional systems from source-to-sink. Nutzungsrecht: © COPYRIGHT 2015 Elsevier Science Publishers Rocks, Sedimentary Basins (Geology) Submarine valleys Analysis Stratigraphy Sedimentary geology Basins Rocks Evolution P Bown oth KT Pickering oth M BouDagher-Fadel oth NJ Bayliss oth SA Robinson oth Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 144(2015), Seite 10-22 (DE-627)129069752 (DE-600)1792-9 (DE-576)014401525 0012-8252 nnns volume:144 year:2015 pages:10-22 http://dx.doi.org/10.1016/j.earscirev.2014.11.006 Volltext http://search.proquest.com/docview/1681501022 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_4028 RA 1000 AR 144 2015 10-22 |
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10.1016/j.earscirev.2014.11.006 doi PQ20160617 (DE-627)OLC1967858551 (DE-599)GBVOLC1967858551 (PRQ)c1822-43b4817eab2a89553bbb453b28c6f64975d6229ec8fd68de702cf7888e618d460 (KEY)0080876820150000144000000010newagemodelforthemiddleeocenedeepmarineainsabasins DE-627 ger DE-627 rakwb eng 070 550 DNB RA 1000 AVZ rvk JI Scotchman verfasserin aut A new age model for the middle Eocene deep-marine Ainsa Basin, Spanish Pyrenees 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for the submarine fan and related deposits. Here, we present a new composite basin stratigraphy based upon biostratigraphic analyses of the Upper Hecho Group submarine-fan and interfan deposits. Calcareous nannofossil data suggest that deposition of the Gerbe through to Guaso systems occurred during biozones NP14-16 (42.6 and 48.9 Ma based on our age model). Additional biostratigraphic ages from the Lower Hecho Group suggest that the entire Hecho Group no older than biozone NP13 (~ 51 Ma). The improved chronostratigraphic control enables correlations between submarine canyons and submarine-fans of the Ainsa and Jaca basins to be assessed. Our new age model provides a means of comparison of stratigraphic events with regional sections allowing a better understanding of the lateral and temporal evolution of these depositional systems from source-to-sink. Nutzungsrecht: © COPYRIGHT 2015 Elsevier Science Publishers Rocks, Sedimentary Basins (Geology) Submarine valleys Analysis Stratigraphy Sedimentary geology Basins Rocks Evolution P Bown oth KT Pickering oth M BouDagher-Fadel oth NJ Bayliss oth SA Robinson oth Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 144(2015), Seite 10-22 (DE-627)129069752 (DE-600)1792-9 (DE-576)014401525 0012-8252 nnns volume:144 year:2015 pages:10-22 http://dx.doi.org/10.1016/j.earscirev.2014.11.006 Volltext http://search.proquest.com/docview/1681501022 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_4028 RA 1000 AR 144 2015 10-22 |
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10.1016/j.earscirev.2014.11.006 doi PQ20160617 (DE-627)OLC1967858551 (DE-599)GBVOLC1967858551 (PRQ)c1822-43b4817eab2a89553bbb453b28c6f64975d6229ec8fd68de702cf7888e618d460 (KEY)0080876820150000144000000010newagemodelforthemiddleeocenedeepmarineainsabasins DE-627 ger DE-627 rakwb eng 070 550 DNB RA 1000 AVZ rvk JI Scotchman verfasserin aut A new age model for the middle Eocene deep-marine Ainsa Basin, Spanish Pyrenees 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for the submarine fan and related deposits. Here, we present a new composite basin stratigraphy based upon biostratigraphic analyses of the Upper Hecho Group submarine-fan and interfan deposits. Calcareous nannofossil data suggest that deposition of the Gerbe through to Guaso systems occurred during biozones NP14-16 (42.6 and 48.9 Ma based on our age model). Additional biostratigraphic ages from the Lower Hecho Group suggest that the entire Hecho Group no older than biozone NP13 (~ 51 Ma). The improved chronostratigraphic control enables correlations between submarine canyons and submarine-fans of the Ainsa and Jaca basins to be assessed. Our new age model provides a means of comparison of stratigraphic events with regional sections allowing a better understanding of the lateral and temporal evolution of these depositional systems from source-to-sink. Nutzungsrecht: © COPYRIGHT 2015 Elsevier Science Publishers Rocks, Sedimentary Basins (Geology) Submarine valleys Analysis Stratigraphy Sedimentary geology Basins Rocks Evolution P Bown oth KT Pickering oth M BouDagher-Fadel oth NJ Bayliss oth SA Robinson oth Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 144(2015), Seite 10-22 (DE-627)129069752 (DE-600)1792-9 (DE-576)014401525 0012-8252 nnns volume:144 year:2015 pages:10-22 http://dx.doi.org/10.1016/j.earscirev.2014.11.006 Volltext http://search.proquest.com/docview/1681501022 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_4028 RA 1000 AR 144 2015 10-22 |
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new age model for the middle eocene deep-marine ainsa basin, spanish pyrenees |
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A new age model for the middle Eocene deep-marine Ainsa Basin, Spanish Pyrenees |
| abstract |
The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for the submarine fan and related deposits. Here, we present a new composite basin stratigraphy based upon biostratigraphic analyses of the Upper Hecho Group submarine-fan and interfan deposits. Calcareous nannofossil data suggest that deposition of the Gerbe through to Guaso systems occurred during biozones NP14-16 (42.6 and 48.9 Ma based on our age model). Additional biostratigraphic ages from the Lower Hecho Group suggest that the entire Hecho Group no older than biozone NP13 (~ 51 Ma). The improved chronostratigraphic control enables correlations between submarine canyons and submarine-fans of the Ainsa and Jaca basins to be assessed. Our new age model provides a means of comparison of stratigraphic events with regional sections allowing a better understanding of the lateral and temporal evolution of these depositional systems from source-to-sink. |
| abstractGer |
The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for the submarine fan and related deposits. Here, we present a new composite basin stratigraphy based upon biostratigraphic analyses of the Upper Hecho Group submarine-fan and interfan deposits. Calcareous nannofossil data suggest that deposition of the Gerbe through to Guaso systems occurred during biozones NP14-16 (42.6 and 48.9 Ma based on our age model). Additional biostratigraphic ages from the Lower Hecho Group suggest that the entire Hecho Group no older than biozone NP13 (~ 51 Ma). The improved chronostratigraphic control enables correlations between submarine canyons and submarine-fans of the Ainsa and Jaca basins to be assessed. Our new age model provides a means of comparison of stratigraphic events with regional sections allowing a better understanding of the lateral and temporal evolution of these depositional systems from source-to-sink. |
| abstract_unstemmed |
The middle Eocene Ainsa Basin, Spanish Pyrenees, comprises ~ 4 km of deep-marine sedimentary rocks belonging to the Hecho Group. Despite extensive study of these exemplary deep-marine clastic successions, there has been no comprehensive chronostratigraphic framework that provides primary ages for the submarine fan and related deposits. Here, we present a new composite basin stratigraphy based upon biostratigraphic analyses of the Upper Hecho Group submarine-fan and interfan deposits. Calcareous nannofossil data suggest that deposition of the Gerbe through to Guaso systems occurred during biozones NP14-16 (42.6 and 48.9 Ma based on our age model). Additional biostratigraphic ages from the Lower Hecho Group suggest that the entire Hecho Group no older than biozone NP13 (~ 51 Ma). The improved chronostratigraphic control enables correlations between submarine canyons and submarine-fans of the Ainsa and Jaca basins to be assessed. Our new age model provides a means of comparison of stratigraphic events with regional sections allowing a better understanding of the lateral and temporal evolution of these depositional systems from source-to-sink. |
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A new age model for the middle Eocene deep-marine Ainsa Basin, Spanish Pyrenees |
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