Stratigraphic variations control deformation patterns in evaporite basins: Messinian examples, onshore and offshore Sicily (Italy)
Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated h...
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Gespeichert in:
| Autor*in: |
Robert WH Butler [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Rechteinformationen: |
Nutzungsrecht: © COPYRIGHT 2015 Geological Society Publishing House |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Journal of the Geological Society - London : Soc., 1971, 172(2015), 1, Seite 113-124 |
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| Übergeordnetes Werk: |
volume:172 ; year:2015 ; number:1 ; pages:113-124 |
| Links: |
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| DOI / URN: |
10.1144/jgs2014-024 |
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| 520 | |a Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated here using Messinian examples from the Maghrebian thrust system of Sicily and applied to the adjacent Ionian sea-bed. By integrating outcrop and onshore subsurface data, we demonstrate variations in evaporite stratigraphies deposited across thrust-top basins, and how these variations have controlled subsequent deformation of these basins. Gypsum and carbonate units develop broad single-layer buckle fold trains, with wavelengths reflecting layer thickness. The development of deformation appears limited by bending resistance at fold hinges, which can be overcome by syntectonic erosion. In contrast, the thick halite and K-salt accumulations in growth synclines have deformed with short-wavelength folds and distributed strain. These structures can display rapid lateral variations (on a scale of hundreds of metres). Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. Using the Sicilian outcrop as analogues, the structural styles for the Ionian may be used to infer evaporite type in these subsurface examples. | ||
| 540 | |a Nutzungsrecht: © COPYRIGHT 2015 Geological Society Publishing House | ||
| 650 | 4 | |a Sedimentary basins | |
| 650 | 4 | |a Geological research | |
| 650 | 4 | |a Environmental aspects | |
| 650 | 4 | |a Stratigraphy | |
| 650 | 4 | |a Seismology | |
| 650 | 4 | |a Sedimentary geology | |
| 650 | 4 | |a Basins | |
| 650 | 4 | |a Minerals | |
| 650 | 4 | |a Deformation | |
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| 700 | 0 | |a Giovanni Sturiale |4 oth | |
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10.1144/jgs2014-024 doi PQ20160617 (DE-627)OLC1964915058 (DE-599)GBVOLC1964915058 (PRQ)c1990-2280efd766c21a3514b6ae68e3a10dd98518421ef05a8a38498724568651a23d0 (KEY)0037806220150000172000100113stratigraphicvariationscontroldeformationpatternsi DE-627 ger DE-627 rakwb eng 550 DNB Robert WH Butler verfasserin aut Stratigraphic variations control deformation patterns in evaporite basins: Messinian examples, onshore and offshore Sicily (Italy) 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated here using Messinian examples from the Maghrebian thrust system of Sicily and applied to the adjacent Ionian sea-bed. By integrating outcrop and onshore subsurface data, we demonstrate variations in evaporite stratigraphies deposited across thrust-top basins, and how these variations have controlled subsequent deformation of these basins. Gypsum and carbonate units develop broad single-layer buckle fold trains, with wavelengths reflecting layer thickness. The development of deformation appears limited by bending resistance at fold hinges, which can be overcome by syntectonic erosion. In contrast, the thick halite and K-salt accumulations in growth synclines have deformed with short-wavelength folds and distributed strain. These structures can display rapid lateral variations (on a scale of hundreds of metres). Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. Using the Sicilian outcrop as analogues, the structural styles for the Ionian may be used to infer evaporite type in these subsurface examples. Nutzungsrecht: © COPYRIGHT 2015 Geological Society Publishing House Sedimentary basins Geological research Environmental aspects Stratigraphy Seismology Sedimentary geology Basins Minerals Deformation Rosanna Maniscalco oth Giovanni Sturiale oth Mario Grasso oth Enthalten in Journal of the Geological Society London : Soc., 1971 172(2015), 1, Seite 113-124 (DE-627)129290556 (DE-600)120368-X (DE-576)014471868 0016-7649 nnns volume:172 year:2015 number:1 pages:113-124 http://dx.doi.org/10.1144/jgs2014-024 Volltext http://search.proquest.com/docview/1648981302 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_69 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4323 AR 172 2015 1 113-124 |
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10.1144/jgs2014-024 doi PQ20160617 (DE-627)OLC1964915058 (DE-599)GBVOLC1964915058 (PRQ)c1990-2280efd766c21a3514b6ae68e3a10dd98518421ef05a8a38498724568651a23d0 (KEY)0037806220150000172000100113stratigraphicvariationscontroldeformationpatternsi DE-627 ger DE-627 rakwb eng 550 DNB Robert WH Butler verfasserin aut Stratigraphic variations control deformation patterns in evaporite basins: Messinian examples, onshore and offshore Sicily (Italy) 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated here using Messinian examples from the Maghrebian thrust system of Sicily and applied to the adjacent Ionian sea-bed. By integrating outcrop and onshore subsurface data, we demonstrate variations in evaporite stratigraphies deposited across thrust-top basins, and how these variations have controlled subsequent deformation of these basins. Gypsum and carbonate units develop broad single-layer buckle fold trains, with wavelengths reflecting layer thickness. The development of deformation appears limited by bending resistance at fold hinges, which can be overcome by syntectonic erosion. In contrast, the thick halite and K-salt accumulations in growth synclines have deformed with short-wavelength folds and distributed strain. These structures can display rapid lateral variations (on a scale of hundreds of metres). Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. Using the Sicilian outcrop as analogues, the structural styles for the Ionian may be used to infer evaporite type in these subsurface examples. Nutzungsrecht: © COPYRIGHT 2015 Geological Society Publishing House Sedimentary basins Geological research Environmental aspects Stratigraphy Seismology Sedimentary geology Basins Minerals Deformation Rosanna Maniscalco oth Giovanni Sturiale oth Mario Grasso oth Enthalten in Journal of the Geological Society London : Soc., 1971 172(2015), 1, Seite 113-124 (DE-627)129290556 (DE-600)120368-X (DE-576)014471868 0016-7649 nnns volume:172 year:2015 number:1 pages:113-124 http://dx.doi.org/10.1144/jgs2014-024 Volltext http://search.proquest.com/docview/1648981302 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_69 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4323 AR 172 2015 1 113-124 |
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10.1144/jgs2014-024 doi PQ20160617 (DE-627)OLC1964915058 (DE-599)GBVOLC1964915058 (PRQ)c1990-2280efd766c21a3514b6ae68e3a10dd98518421ef05a8a38498724568651a23d0 (KEY)0037806220150000172000100113stratigraphicvariationscontroldeformationpatternsi DE-627 ger DE-627 rakwb eng 550 DNB Robert WH Butler verfasserin aut Stratigraphic variations control deformation patterns in evaporite basins: Messinian examples, onshore and offshore Sicily (Italy) 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated here using Messinian examples from the Maghrebian thrust system of Sicily and applied to the adjacent Ionian sea-bed. By integrating outcrop and onshore subsurface data, we demonstrate variations in evaporite stratigraphies deposited across thrust-top basins, and how these variations have controlled subsequent deformation of these basins. Gypsum and carbonate units develop broad single-layer buckle fold trains, with wavelengths reflecting layer thickness. The development of deformation appears limited by bending resistance at fold hinges, which can be overcome by syntectonic erosion. In contrast, the thick halite and K-salt accumulations in growth synclines have deformed with short-wavelength folds and distributed strain. These structures can display rapid lateral variations (on a scale of hundreds of metres). Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. Using the Sicilian outcrop as analogues, the structural styles for the Ionian may be used to infer evaporite type in these subsurface examples. Nutzungsrecht: © COPYRIGHT 2015 Geological Society Publishing House Sedimentary basins Geological research Environmental aspects Stratigraphy Seismology Sedimentary geology Basins Minerals Deformation Rosanna Maniscalco oth Giovanni Sturiale oth Mario Grasso oth Enthalten in Journal of the Geological Society London : Soc., 1971 172(2015), 1, Seite 113-124 (DE-627)129290556 (DE-600)120368-X (DE-576)014471868 0016-7649 nnns volume:172 year:2015 number:1 pages:113-124 http://dx.doi.org/10.1144/jgs2014-024 Volltext http://search.proquest.com/docview/1648981302 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_69 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4323 AR 172 2015 1 113-124 |
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10.1144/jgs2014-024 doi PQ20160617 (DE-627)OLC1964915058 (DE-599)GBVOLC1964915058 (PRQ)c1990-2280efd766c21a3514b6ae68e3a10dd98518421ef05a8a38498724568651a23d0 (KEY)0037806220150000172000100113stratigraphicvariationscontroldeformationpatternsi DE-627 ger DE-627 rakwb eng 550 DNB Robert WH Butler verfasserin aut Stratigraphic variations control deformation patterns in evaporite basins: Messinian examples, onshore and offshore Sicily (Italy) 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated here using Messinian examples from the Maghrebian thrust system of Sicily and applied to the adjacent Ionian sea-bed. By integrating outcrop and onshore subsurface data, we demonstrate variations in evaporite stratigraphies deposited across thrust-top basins, and how these variations have controlled subsequent deformation of these basins. Gypsum and carbonate units develop broad single-layer buckle fold trains, with wavelengths reflecting layer thickness. The development of deformation appears limited by bending resistance at fold hinges, which can be overcome by syntectonic erosion. In contrast, the thick halite and K-salt accumulations in growth synclines have deformed with short-wavelength folds and distributed strain. These structures can display rapid lateral variations (on a scale of hundreds of metres). Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. Using the Sicilian outcrop as analogues, the structural styles for the Ionian may be used to infer evaporite type in these subsurface examples. Nutzungsrecht: © COPYRIGHT 2015 Geological Society Publishing House Sedimentary basins Geological research Environmental aspects Stratigraphy Seismology Sedimentary geology Basins Minerals Deformation Rosanna Maniscalco oth Giovanni Sturiale oth Mario Grasso oth Enthalten in Journal of the Geological Society London : Soc., 1971 172(2015), 1, Seite 113-124 (DE-627)129290556 (DE-600)120368-X (DE-576)014471868 0016-7649 nnns volume:172 year:2015 number:1 pages:113-124 http://dx.doi.org/10.1144/jgs2014-024 Volltext http://search.proquest.com/docview/1648981302 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_69 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4323 AR 172 2015 1 113-124 |
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10.1144/jgs2014-024 doi PQ20160617 (DE-627)OLC1964915058 (DE-599)GBVOLC1964915058 (PRQ)c1990-2280efd766c21a3514b6ae68e3a10dd98518421ef05a8a38498724568651a23d0 (KEY)0037806220150000172000100113stratigraphicvariationscontroldeformationpatternsi DE-627 ger DE-627 rakwb eng 550 DNB Robert WH Butler verfasserin aut Stratigraphic variations control deformation patterns in evaporite basins: Messinian examples, onshore and offshore Sicily (Italy) 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated here using Messinian examples from the Maghrebian thrust system of Sicily and applied to the adjacent Ionian sea-bed. By integrating outcrop and onshore subsurface data, we demonstrate variations in evaporite stratigraphies deposited across thrust-top basins, and how these variations have controlled subsequent deformation of these basins. Gypsum and carbonate units develop broad single-layer buckle fold trains, with wavelengths reflecting layer thickness. The development of deformation appears limited by bending resistance at fold hinges, which can be overcome by syntectonic erosion. In contrast, the thick halite and K-salt accumulations in growth synclines have deformed with short-wavelength folds and distributed strain. These structures can display rapid lateral variations (on a scale of hundreds of metres). Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. Using the Sicilian outcrop as analogues, the structural styles for the Ionian may be used to infer evaporite type in these subsurface examples. Nutzungsrecht: © COPYRIGHT 2015 Geological Society Publishing House Sedimentary basins Geological research Environmental aspects Stratigraphy Seismology Sedimentary geology Basins Minerals Deformation Rosanna Maniscalco oth Giovanni Sturiale oth Mario Grasso oth Enthalten in Journal of the Geological Society London : Soc., 1971 172(2015), 1, Seite 113-124 (DE-627)129290556 (DE-600)120368-X (DE-576)014471868 0016-7649 nnns volume:172 year:2015 number:1 pages:113-124 http://dx.doi.org/10.1144/jgs2014-024 Volltext http://search.proquest.com/docview/1648981302 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_69 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 GBV_ILN_4323 AR 172 2015 1 113-124 |
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Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. 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stratigraphic variations control deformation patterns in evaporite basins: messinian examples, onshore and offshore sicily (italy) |
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Stratigraphic variations control deformation patterns in evaporite basins: Messinian examples, onshore and offshore Sicily (Italy) |
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Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated here using Messinian examples from the Maghrebian thrust system of Sicily and applied to the adjacent Ionian sea-bed. By integrating outcrop and onshore subsurface data, we demonstrate variations in evaporite stratigraphies deposited across thrust-top basins, and how these variations have controlled subsequent deformation of these basins. Gypsum and carbonate units develop broad single-layer buckle fold trains, with wavelengths reflecting layer thickness. The development of deformation appears limited by bending resistance at fold hinges, which can be overcome by syntectonic erosion. In contrast, the thick halite and K-salt accumulations in growth synclines have deformed with short-wavelength folds and distributed strain. These structures can display rapid lateral variations (on a scale of hundreds of metres). Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. Using the Sicilian outcrop as analogues, the structural styles for the Ionian may be used to infer evaporite type in these subsurface examples. |
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Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated here using Messinian examples from the Maghrebian thrust system of Sicily and applied to the adjacent Ionian sea-bed. By integrating outcrop and onshore subsurface data, we demonstrate variations in evaporite stratigraphies deposited across thrust-top basins, and how these variations have controlled subsequent deformation of these basins. Gypsum and carbonate units develop broad single-layer buckle fold trains, with wavelengths reflecting layer thickness. The development of deformation appears limited by bending resistance at fold hinges, which can be overcome by syntectonic erosion. In contrast, the thick halite and K-salt accumulations in growth synclines have deformed with short-wavelength folds and distributed strain. These structures can display rapid lateral variations (on a scale of hundreds of metres). Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. Using the Sicilian outcrop as analogues, the structural styles for the Ionian may be used to infer evaporite type in these subsurface examples. |
| abstract_unstemmed |
Three-dimensional seismic data are increasingly resolving original compositional heterogeneity and structural complexity in evaporitic successions within sedimentary basins. The relationship between basin structure, evaporite composition and its influence on subsequent deformation are investigated here using Messinian examples from the Maghrebian thrust system of Sicily and applied to the adjacent Ionian sea-bed. By integrating outcrop and onshore subsurface data, we demonstrate variations in evaporite stratigraphies deposited across thrust-top basins, and how these variations have controlled subsequent deformation of these basins. Gypsum and carbonate units develop broad single-layer buckle fold trains, with wavelengths reflecting layer thickness. The development of deformation appears limited by bending resistance at fold hinges, which can be overcome by syntectonic erosion. In contrast, the thick halite and K-salt accumulations in growth synclines have deformed with short-wavelength folds and distributed strain. These structures can display rapid lateral variations (on a scale of hundreds of metres). Similar structural styles, with buckle fold trains passing laterally into more homogeneously shortened, short-wavelength folding, are evident on seismic data from the buried Messinian interval beneath the Ionian Sea. Using the Sicilian outcrop as analogues, the structural styles for the Ionian may be used to infer evaporite type in these subsurface examples. |
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Stratigraphic variations control deformation patterns in evaporite basins: Messinian examples, onshore and offshore Sicily (Italy) |
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