Fractal structure formation at various stages of the evolution of the oceanic lithosphere: Premises, examples, and problems
Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and...
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: Oceanology - Nauka/Interperiodica, 1966, 46(2006), 1 vom: Jan., Seite 123-133 |
|---|---|
| Übergeordnetes Werk: |
volume:46 ; year:2006 ; number:1 ; month:01 ; pages:123-133 |
| Links: |
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| DOI / URN: |
10.1134/S0001437006010140 |
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OLC2071610059 |
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| 520 | |a Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. Within the frameworks of this line, selected problems are specified: the scales of the compressional deformations and horizontal stratification of the oceanic crust and lithosphere and the necessity for the development of a special terminological basis. | ||
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10.1134/S0001437006010140 doi (DE-627)OLC2071610059 (DE-He213)S0001437006010140-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mirlin, E. G. verfasserin aut Fractal structure formation at various stages of the evolution of the oceanic lithosphere: Premises, examples, and problems 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. Within the frameworks of this line, selected problems are specified: the scales of the compressional deformations and horizontal stratification of the oceanic crust and lithosphere and the necessity for the development of a special terminological basis. Lithosphere Continental Margin Oceanic Crust Nonlinear Dynamical System Oceanic Lithosphere Enthalten in Oceanology Nauka/Interperiodica, 1966 46(2006), 1 vom: Jan., Seite 123-133 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:46 year:2006 number:1 month:01 pages:123-133 https://doi.org/10.1134/S0001437006010140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_201 GBV_ILN_381 AR 46 2006 1 01 123-133 |
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10.1134/S0001437006010140 doi (DE-627)OLC2071610059 (DE-He213)S0001437006010140-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mirlin, E. G. verfasserin aut Fractal structure formation at various stages of the evolution of the oceanic lithosphere: Premises, examples, and problems 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. Within the frameworks of this line, selected problems are specified: the scales of the compressional deformations and horizontal stratification of the oceanic crust and lithosphere and the necessity for the development of a special terminological basis. Lithosphere Continental Margin Oceanic Crust Nonlinear Dynamical System Oceanic Lithosphere Enthalten in Oceanology Nauka/Interperiodica, 1966 46(2006), 1 vom: Jan., Seite 123-133 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:46 year:2006 number:1 month:01 pages:123-133 https://doi.org/10.1134/S0001437006010140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_201 GBV_ILN_381 AR 46 2006 1 01 123-133 |
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10.1134/S0001437006010140 doi (DE-627)OLC2071610059 (DE-He213)S0001437006010140-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mirlin, E. G. verfasserin aut Fractal structure formation at various stages of the evolution of the oceanic lithosphere: Premises, examples, and problems 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. Within the frameworks of this line, selected problems are specified: the scales of the compressional deformations and horizontal stratification of the oceanic crust and lithosphere and the necessity for the development of a special terminological basis. Lithosphere Continental Margin Oceanic Crust Nonlinear Dynamical System Oceanic Lithosphere Enthalten in Oceanology Nauka/Interperiodica, 1966 46(2006), 1 vom: Jan., Seite 123-133 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:46 year:2006 number:1 month:01 pages:123-133 https://doi.org/10.1134/S0001437006010140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_201 GBV_ILN_381 AR 46 2006 1 01 123-133 |
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10.1134/S0001437006010140 doi (DE-627)OLC2071610059 (DE-He213)S0001437006010140-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mirlin, E. G. verfasserin aut Fractal structure formation at various stages of the evolution of the oceanic lithosphere: Premises, examples, and problems 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. Within the frameworks of this line, selected problems are specified: the scales of the compressional deformations and horizontal stratification of the oceanic crust and lithosphere and the necessity for the development of a special terminological basis. Lithosphere Continental Margin Oceanic Crust Nonlinear Dynamical System Oceanic Lithosphere Enthalten in Oceanology Nauka/Interperiodica, 1966 46(2006), 1 vom: Jan., Seite 123-133 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:46 year:2006 number:1 month:01 pages:123-133 https://doi.org/10.1134/S0001437006010140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_201 GBV_ILN_381 AR 46 2006 1 01 123-133 |
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10.1134/S0001437006010140 doi (DE-627)OLC2071610059 (DE-He213)S0001437006010140-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mirlin, E. G. verfasserin aut Fractal structure formation at various stages of the evolution of the oceanic lithosphere: Premises, examples, and problems 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2006 Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. Within the frameworks of this line, selected problems are specified: the scales of the compressional deformations and horizontal stratification of the oceanic crust and lithosphere and the necessity for the development of a special terminological basis. Lithosphere Continental Margin Oceanic Crust Nonlinear Dynamical System Oceanic Lithosphere Enthalten in Oceanology Nauka/Interperiodica, 1966 46(2006), 1 vom: Jan., Seite 123-133 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:46 year:2006 number:1 month:01 pages:123-133 https://doi.org/10.1134/S0001437006010140 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_201 GBV_ILN_381 AR 46 2006 1 01 123-133 |
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Fractal structure formation at various stages of the evolution of the oceanic lithosphere: Premises, examples, and problems |
| abstract |
Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. Within the frameworks of this line, selected problems are specified: the scales of the compressional deformations and horizontal stratification of the oceanic crust and lithosphere and the necessity for the development of a special terminological basis. © Pleiades Publishing, Inc. 2006 |
| abstractGer |
Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. Within the frameworks of this line, selected problems are specified: the scales of the compressional deformations and horizontal stratification of the oceanic crust and lithosphere and the necessity for the development of a special terminological basis. © Pleiades Publishing, Inc. 2006 |
| abstract_unstemmed |
Abstract Premises according to which the lithosphere represents a nonlinear dynamical system with particular fractal objects are considered. A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. Within the frameworks of this line, selected problems are specified: the scales of the compressional deformations and horizontal stratification of the oceanic crust and lithosphere and the necessity for the development of a special terminological basis. © Pleiades Publishing, Inc. 2006 |
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Fractal structure formation at various stages of the evolution of the oceanic lithosphere: Premises, examples, and problems |
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https://doi.org/10.1134/S0001437006010140 |
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10.1134/S0001437006010140 |
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2024-07-04T03:50:13.298Z |
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A series of examples helps to show that, at the principal stages of the evolution of the lithosphere, from continental rifts to passive continental margins and spreading centers on the crests of mid-ocean ridges, scale-invariant structures are generated associated with pull-apart features under the presence of a shear component. An hypothesis is posed according to which the latter structures are formed due to vortical movements similar to those in the hydrosphere and atmosphere at their origin. The diverse properties of the geological medium, which may be referred to as fractal, together with the examples assessed, allow us to make a conclusion concerning the development of the fractal (syneregetic) line in the structural-tectonic analysis. 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