The problem of vortical movements in the solid earth and their role in geotectonics
Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has no...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Mirlin, E. G. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2006 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Inc. 2006 |
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| Übergeordnetes Werk: |
Enthalten in: Geotectonics - Nauka/Interperiodica, 1967, 40(2006), 4 vom: Juli, Seite 282-296 |
|---|---|
| Übergeordnetes Werk: |
volume:40 ; year:2006 ; number:4 ; month:07 ; pages:282-296 |
| Links: |
|---|
| DOI / URN: |
10.1134/S0016852106040030 |
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OLC2026594503 |
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| 520 | |a Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has not been offered. With allowance for the specific character of vortical movement, the evolution of the structural geometry of the North Atlantic basins and different segments of the global system of mid-ocean ridges is considered in this paper. It is shown that vortical movements do take place in the solid Earth during ocean formation and create scale-invariant rifting and spreading systems, where the spreading axis tends to undergo whirling. The size of these systems differs by more than two orders of magnitude. Many geotectonic phenomena that accompany the formation of oceans, including segmentation of the ocean floor and passive continental margins, folding of the sedimentary cover at these margins, and tectonic delamination of the oceanic lithosphere, may be explained by vortical movements of different ranks. In addition, the vortical structures on continents are variable in size and related to lithotectonic complexes of different ages. The vortical structural units of the Mediterranean Belt are considered as an example. Being driven by the same physical mechanism, the vortical movements depend on the dynamics of different geospheres. These movements are realized only in a nonlinear, nonequilibrium medium. Hence, only nonlinear and nonequilibrium thermodynamics will serve as a theoretical basis for a new concept, which is coming currently to take the place of plate tectonics. | ||
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10.1134/S0016852106040030 doi (DE-627)OLC2026594503 (DE-He213)S0016852106040030-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Mirlin, E. G. verfasserin aut The problem of vortical movements in the solid earth and their role in geotectonics 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has not been offered. With allowance for the specific character of vortical movement, the evolution of the structural geometry of the North Atlantic basins and different segments of the global system of mid-ocean ridges is considered in this paper. It is shown that vortical movements do take place in the solid Earth during ocean formation and create scale-invariant rifting and spreading systems, where the spreading axis tends to undergo whirling. The size of these systems differs by more than two orders of magnitude. Many geotectonic phenomena that accompany the formation of oceans, including segmentation of the ocean floor and passive continental margins, folding of the sedimentary cover at these margins, and tectonic delamination of the oceanic lithosphere, may be explained by vortical movements of different ranks. In addition, the vortical structures on continents are variable in size and related to lithotectonic complexes of different ages. The vortical structural units of the Mediterranean Belt are considered as an example. Being driven by the same physical mechanism, the vortical movements depend on the dynamics of different geospheres. These movements are realized only in a nonlinear, nonequilibrium medium. Hence, only nonlinear and nonequilibrium thermodynamics will serve as a theoretical basis for a new concept, which is coming currently to take the place of plate tectonics. Vortex Lithosphere Solid Earth Vortical Structure Oceanic Lithosphere Enthalten in Geotectonics Nauka/Interperiodica, 1967 40(2006), 4 vom: Juli, Seite 282-296 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:40 year:2006 number:4 month:07 pages:282-296 https://doi.org/10.1134/S0016852106040030 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 AR 40 2006 4 07 282-296 |
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10.1134/S0016852106040030 doi (DE-627)OLC2026594503 (DE-He213)S0016852106040030-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Mirlin, E. G. verfasserin aut The problem of vortical movements in the solid earth and their role in geotectonics 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has not been offered. With allowance for the specific character of vortical movement, the evolution of the structural geometry of the North Atlantic basins and different segments of the global system of mid-ocean ridges is considered in this paper. It is shown that vortical movements do take place in the solid Earth during ocean formation and create scale-invariant rifting and spreading systems, where the spreading axis tends to undergo whirling. The size of these systems differs by more than two orders of magnitude. Many geotectonic phenomena that accompany the formation of oceans, including segmentation of the ocean floor and passive continental margins, folding of the sedimentary cover at these margins, and tectonic delamination of the oceanic lithosphere, may be explained by vortical movements of different ranks. In addition, the vortical structures on continents are variable in size and related to lithotectonic complexes of different ages. The vortical structural units of the Mediterranean Belt are considered as an example. Being driven by the same physical mechanism, the vortical movements depend on the dynamics of different geospheres. These movements are realized only in a nonlinear, nonequilibrium medium. Hence, only nonlinear and nonequilibrium thermodynamics will serve as a theoretical basis for a new concept, which is coming currently to take the place of plate tectonics. Vortex Lithosphere Solid Earth Vortical Structure Oceanic Lithosphere Enthalten in Geotectonics Nauka/Interperiodica, 1967 40(2006), 4 vom: Juli, Seite 282-296 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:40 year:2006 number:4 month:07 pages:282-296 https://doi.org/10.1134/S0016852106040030 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 AR 40 2006 4 07 282-296 |
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10.1134/S0016852106040030 doi (DE-627)OLC2026594503 (DE-He213)S0016852106040030-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Mirlin, E. G. verfasserin aut The problem of vortical movements in the solid earth and their role in geotectonics 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has not been offered. With allowance for the specific character of vortical movement, the evolution of the structural geometry of the North Atlantic basins and different segments of the global system of mid-ocean ridges is considered in this paper. It is shown that vortical movements do take place in the solid Earth during ocean formation and create scale-invariant rifting and spreading systems, where the spreading axis tends to undergo whirling. The size of these systems differs by more than two orders of magnitude. Many geotectonic phenomena that accompany the formation of oceans, including segmentation of the ocean floor and passive continental margins, folding of the sedimentary cover at these margins, and tectonic delamination of the oceanic lithosphere, may be explained by vortical movements of different ranks. In addition, the vortical structures on continents are variable in size and related to lithotectonic complexes of different ages. The vortical structural units of the Mediterranean Belt are considered as an example. Being driven by the same physical mechanism, the vortical movements depend on the dynamics of different geospheres. These movements are realized only in a nonlinear, nonequilibrium medium. Hence, only nonlinear and nonequilibrium thermodynamics will serve as a theoretical basis for a new concept, which is coming currently to take the place of plate tectonics. Vortex Lithosphere Solid Earth Vortical Structure Oceanic Lithosphere Enthalten in Geotectonics Nauka/Interperiodica, 1967 40(2006), 4 vom: Juli, Seite 282-296 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:40 year:2006 number:4 month:07 pages:282-296 https://doi.org/10.1134/S0016852106040030 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 AR 40 2006 4 07 282-296 |
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10.1134/S0016852106040030 doi (DE-627)OLC2026594503 (DE-He213)S0016852106040030-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Mirlin, E. G. verfasserin aut The problem of vortical movements in the solid earth and their role in geotectonics 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has not been offered. With allowance for the specific character of vortical movement, the evolution of the structural geometry of the North Atlantic basins and different segments of the global system of mid-ocean ridges is considered in this paper. It is shown that vortical movements do take place in the solid Earth during ocean formation and create scale-invariant rifting and spreading systems, where the spreading axis tends to undergo whirling. The size of these systems differs by more than two orders of magnitude. Many geotectonic phenomena that accompany the formation of oceans, including segmentation of the ocean floor and passive continental margins, folding of the sedimentary cover at these margins, and tectonic delamination of the oceanic lithosphere, may be explained by vortical movements of different ranks. In addition, the vortical structures on continents are variable in size and related to lithotectonic complexes of different ages. The vortical structural units of the Mediterranean Belt are considered as an example. Being driven by the same physical mechanism, the vortical movements depend on the dynamics of different geospheres. These movements are realized only in a nonlinear, nonequilibrium medium. Hence, only nonlinear and nonequilibrium thermodynamics will serve as a theoretical basis for a new concept, which is coming currently to take the place of plate tectonics. Vortex Lithosphere Solid Earth Vortical Structure Oceanic Lithosphere Enthalten in Geotectonics Nauka/Interperiodica, 1967 40(2006), 4 vom: Juli, Seite 282-296 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:40 year:2006 number:4 month:07 pages:282-296 https://doi.org/10.1134/S0016852106040030 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 AR 40 2006 4 07 282-296 |
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10.1134/S0016852106040030 doi (DE-627)OLC2026594503 (DE-He213)S0016852106040030-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Mirlin, E. G. verfasserin aut The problem of vortical movements in the solid earth and their role in geotectonics 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has not been offered. With allowance for the specific character of vortical movement, the evolution of the structural geometry of the North Atlantic basins and different segments of the global system of mid-ocean ridges is considered in this paper. It is shown that vortical movements do take place in the solid Earth during ocean formation and create scale-invariant rifting and spreading systems, where the spreading axis tends to undergo whirling. The size of these systems differs by more than two orders of magnitude. Many geotectonic phenomena that accompany the formation of oceans, including segmentation of the ocean floor and passive continental margins, folding of the sedimentary cover at these margins, and tectonic delamination of the oceanic lithosphere, may be explained by vortical movements of different ranks. In addition, the vortical structures on continents are variable in size and related to lithotectonic complexes of different ages. The vortical structural units of the Mediterranean Belt are considered as an example. Being driven by the same physical mechanism, the vortical movements depend on the dynamics of different geospheres. These movements are realized only in a nonlinear, nonequilibrium medium. Hence, only nonlinear and nonequilibrium thermodynamics will serve as a theoretical basis for a new concept, which is coming currently to take the place of plate tectonics. Vortex Lithosphere Solid Earth Vortical Structure Oceanic Lithosphere Enthalten in Geotectonics Nauka/Interperiodica, 1967 40(2006), 4 vom: Juli, Seite 282-296 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:40 year:2006 number:4 month:07 pages:282-296 https://doi.org/10.1134/S0016852106040030 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 AR 40 2006 4 07 282-296 |
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The problem of vortical movements in the solid earth and their role in geotectonics |
| abstract |
Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has not been offered. With allowance for the specific character of vortical movement, the evolution of the structural geometry of the North Atlantic basins and different segments of the global system of mid-ocean ridges is considered in this paper. It is shown that vortical movements do take place in the solid Earth during ocean formation and create scale-invariant rifting and spreading systems, where the spreading axis tends to undergo whirling. The size of these systems differs by more than two orders of magnitude. Many geotectonic phenomena that accompany the formation of oceans, including segmentation of the ocean floor and passive continental margins, folding of the sedimentary cover at these margins, and tectonic delamination of the oceanic lithosphere, may be explained by vortical movements of different ranks. In addition, the vortical structures on continents are variable in size and related to lithotectonic complexes of different ages. The vortical structural units of the Mediterranean Belt are considered as an example. Being driven by the same physical mechanism, the vortical movements depend on the dynamics of different geospheres. These movements are realized only in a nonlinear, nonequilibrium medium. Hence, only nonlinear and nonequilibrium thermodynamics will serve as a theoretical basis for a new concept, which is coming currently to take the place of plate tectonics. © Pleiades Publishing, Inc. 2006 |
| abstractGer |
Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has not been offered. With allowance for the specific character of vortical movement, the evolution of the structural geometry of the North Atlantic basins and different segments of the global system of mid-ocean ridges is considered in this paper. It is shown that vortical movements do take place in the solid Earth during ocean formation and create scale-invariant rifting and spreading systems, where the spreading axis tends to undergo whirling. The size of these systems differs by more than two orders of magnitude. Many geotectonic phenomena that accompany the formation of oceans, including segmentation of the ocean floor and passive continental margins, folding of the sedimentary cover at these margins, and tectonic delamination of the oceanic lithosphere, may be explained by vortical movements of different ranks. In addition, the vortical structures on continents are variable in size and related to lithotectonic complexes of different ages. The vortical structural units of the Mediterranean Belt are considered as an example. Being driven by the same physical mechanism, the vortical movements depend on the dynamics of different geospheres. These movements are realized only in a nonlinear, nonequilibrium medium. Hence, only nonlinear and nonequilibrium thermodynamics will serve as a theoretical basis for a new concept, which is coming currently to take the place of plate tectonics. © Pleiades Publishing, Inc. 2006 |
| abstract_unstemmed |
Abstract Crustal structural features having a vortical or spiral shape were discovered in the first third of the 20th century. Since then, such features of various ranks, but similar appearance, have been revealed in different geotectonic settings; however, an adequate tectonic interpretation has not been offered. With allowance for the specific character of vortical movement, the evolution of the structural geometry of the North Atlantic basins and different segments of the global system of mid-ocean ridges is considered in this paper. It is shown that vortical movements do take place in the solid Earth during ocean formation and create scale-invariant rifting and spreading systems, where the spreading axis tends to undergo whirling. The size of these systems differs by more than two orders of magnitude. Many geotectonic phenomena that accompany the formation of oceans, including segmentation of the ocean floor and passive continental margins, folding of the sedimentary cover at these margins, and tectonic delamination of the oceanic lithosphere, may be explained by vortical movements of different ranks. In addition, the vortical structures on continents are variable in size and related to lithotectonic complexes of different ages. The vortical structural units of the Mediterranean Belt are considered as an example. Being driven by the same physical mechanism, the vortical movements depend on the dynamics of different geospheres. These movements are realized only in a nonlinear, nonequilibrium medium. Hence, only nonlinear and nonequilibrium thermodynamics will serve as a theoretical basis for a new concept, which is coming currently to take the place of plate tectonics. © Pleiades Publishing, Inc. 2006 |
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| title_short |
The problem of vortical movements in the solid earth and their role in geotectonics |
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https://doi.org/10.1134/S0016852106040030 |
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