Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps
The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the I...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Gianni Balestro [verfasserIn] Andrea Festa [verfasserIn] Sara De Caroli [verfasserIn] Edoardo Barbero [verfasserIn] Alessandro Borghi [verfasserIn] Franco Gianotti [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Übergeordnetes Werk: |
In: Geoscience Frontiers - Elsevier, 2016, 13(2022), 6, Seite 101448- |
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| Übergeordnetes Werk: |
volume:13 ; year:2022 ; number:6 ; pages:101448- |
| Links: |
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| DOI / URN: |
10.1016/j.gsf.2022.101448 |
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DOAJ007821689 |
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| 520 | |a The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations. | ||
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10.1016/j.gsf.2022.101448 doi (DE-627)DOAJ007821689 (DE-599)DOAJ8e1bd92adceb4cacab0409ee58dc538f DE-627 ger DE-627 rakwb eng QE1-996.5 Gianni Balestro verfasserin aut Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations. Suture zone Western Alps Structural inheritance Tectonics and sedimentation Multistage tectonic evolution Geology Andrea Festa verfasserin aut Sara De Caroli verfasserin aut Edoardo Barbero verfasserin aut Alessandro Borghi verfasserin aut Franco Gianotti verfasserin aut In Geoscience Frontiers Elsevier, 2016 13(2022), 6, Seite 101448- (DE-627)DOAJ000091189 25889192 nnns volume:13 year:2022 number:6 pages:101448- https://doi.org/10.1016/j.gsf.2022.101448 kostenfrei https://doaj.org/article/8e1bd92adceb4cacab0409ee58dc538f kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987122001013 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ AR 13 2022 6 101448- |
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10.1016/j.gsf.2022.101448 doi (DE-627)DOAJ007821689 (DE-599)DOAJ8e1bd92adceb4cacab0409ee58dc538f DE-627 ger DE-627 rakwb eng QE1-996.5 Gianni Balestro verfasserin aut Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations. Suture zone Western Alps Structural inheritance Tectonics and sedimentation Multistage tectonic evolution Geology Andrea Festa verfasserin aut Sara De Caroli verfasserin aut Edoardo Barbero verfasserin aut Alessandro Borghi verfasserin aut Franco Gianotti verfasserin aut In Geoscience Frontiers Elsevier, 2016 13(2022), 6, Seite 101448- (DE-627)DOAJ000091189 25889192 nnns volume:13 year:2022 number:6 pages:101448- https://doi.org/10.1016/j.gsf.2022.101448 kostenfrei https://doaj.org/article/8e1bd92adceb4cacab0409ee58dc538f kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987122001013 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ AR 13 2022 6 101448- |
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10.1016/j.gsf.2022.101448 doi (DE-627)DOAJ007821689 (DE-599)DOAJ8e1bd92adceb4cacab0409ee58dc538f DE-627 ger DE-627 rakwb eng QE1-996.5 Gianni Balestro verfasserin aut Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations. Suture zone Western Alps Structural inheritance Tectonics and sedimentation Multistage tectonic evolution Geology Andrea Festa verfasserin aut Sara De Caroli verfasserin aut Edoardo Barbero verfasserin aut Alessandro Borghi verfasserin aut Franco Gianotti verfasserin aut In Geoscience Frontiers Elsevier, 2016 13(2022), 6, Seite 101448- (DE-627)DOAJ000091189 25889192 nnns volume:13 year:2022 number:6 pages:101448- https://doi.org/10.1016/j.gsf.2022.101448 kostenfrei https://doaj.org/article/8e1bd92adceb4cacab0409ee58dc538f kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987122001013 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ AR 13 2022 6 101448- |
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10.1016/j.gsf.2022.101448 doi (DE-627)DOAJ007821689 (DE-599)DOAJ8e1bd92adceb4cacab0409ee58dc538f DE-627 ger DE-627 rakwb eng QE1-996.5 Gianni Balestro verfasserin aut Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations. Suture zone Western Alps Structural inheritance Tectonics and sedimentation Multistage tectonic evolution Geology Andrea Festa verfasserin aut Sara De Caroli verfasserin aut Edoardo Barbero verfasserin aut Alessandro Borghi verfasserin aut Franco Gianotti verfasserin aut In Geoscience Frontiers Elsevier, 2016 13(2022), 6, Seite 101448- (DE-627)DOAJ000091189 25889192 nnns volume:13 year:2022 number:6 pages:101448- https://doi.org/10.1016/j.gsf.2022.101448 kostenfrei https://doaj.org/article/8e1bd92adceb4cacab0409ee58dc538f kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987122001013 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ AR 13 2022 6 101448- |
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10.1016/j.gsf.2022.101448 doi (DE-627)DOAJ007821689 (DE-599)DOAJ8e1bd92adceb4cacab0409ee58dc538f DE-627 ger DE-627 rakwb eng QE1-996.5 Gianni Balestro verfasserin aut Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations. Suture zone Western Alps Structural inheritance Tectonics and sedimentation Multistage tectonic evolution Geology Andrea Festa verfasserin aut Sara De Caroli verfasserin aut Edoardo Barbero verfasserin aut Alessandro Borghi verfasserin aut Franco Gianotti verfasserin aut In Geoscience Frontiers Elsevier, 2016 13(2022), 6, Seite 101448- (DE-627)DOAJ000091189 25889192 nnns volume:13 year:2022 number:6 pages:101448- https://doi.org/10.1016/j.gsf.2022.101448 kostenfrei https://doaj.org/article/8e1bd92adceb4cacab0409ee58dc538f kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987122001013 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ AR 13 2022 6 101448- |
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multistage tectono-stratigraphic evolution of the canavese intracontinental suture zone: new constraints on the tectonics of the inner western alps |
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Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps |
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The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations. |
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The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations. |
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The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations. |
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