Structural evolution and geodynamic position of the Gonzha Block, Upper Amur region
Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbai...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kotov, A. B. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Inc. 2013 |
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| Übergeordnetes Werk: |
Enthalten in: Geotectonics - Springer US, 1967, 47(2013), 5 vom: Sept., Seite 351-361 |
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| Übergeordnetes Werk: |
volume:47 ; year:2013 ; number:5 ; month:09 ; pages:351-361 |
| Links: |
|---|
| DOI / URN: |
10.1134/S0016852113050026 |
|---|
| Katalog-ID: |
OLC2026596603 |
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| 520 | |a Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbaikalia. Exhumation of metamorphic rocks of the Gonzha Block resulted from a collapse of the Late Mesozoic orogen after accrecionary and collisional events related to closure of the Mongolia-Okhotsk paleooceanic basin. The structural elements that determine the main geological features of this block formed over the course of at least three deformation stages. By the onset of the third stage responsible for exhumation of metamorphic rocks pertaining to the Gonzha Group, they had already undergone complex structural transformation and metamorphism related to growth of the Amur microcontinent and its subsequent collision with the Dzhugzur-Stanovoi and Selenga-Stanovoi supperterranes of the Central Asian Foldbelt. This distinguishes the Gonzha Block from complexes of metamorphic cores in western Transbaikalia, whose structural transformation and metamorphism are directly related to their origin. | ||
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| 700 | 1 | |a Sorokin, A. P. |4 aut | |
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10.1134/S0016852113050026 doi (DE-627)OLC2026596603 (DE-He213)S0016852113050026-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Kotov, A. B. verfasserin aut Structural evolution and geodynamic position of the Gonzha Block, Upper Amur region 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2013 Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbaikalia. Exhumation of metamorphic rocks of the Gonzha Block resulted from a collapse of the Late Mesozoic orogen after accrecionary and collisional events related to closure of the Mongolia-Okhotsk paleooceanic basin. The structural elements that determine the main geological features of this block formed over the course of at least three deformation stages. By the onset of the third stage responsible for exhumation of metamorphic rocks pertaining to the Gonzha Group, they had already undergone complex structural transformation and metamorphism related to growth of the Amur microcontinent and its subsequent collision with the Dzhugzur-Stanovoi and Selenga-Stanovoi supperterranes of the Central Asian Foldbelt. This distinguishes the Gonzha Block from complexes of metamorphic cores in western Transbaikalia, whose structural transformation and metamorphism are directly related to their origin. Metamorphic Rock Metavolcanic Rock Argun Tectonic Transport Main Geological Feature Mazukabzov, A. M. aut Skovitina, T. M. aut Velikoslavinsky, S. D. aut Sorokin, A. A. aut Sorokin, A. P. aut Enthalten in Geotectonics Springer US, 1967 47(2013), 5 vom: Sept., Seite 351-361 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:47 year:2013 number:5 month:09 pages:351-361 https://doi.org/10.1134/S0016852113050026 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_2027 AR 47 2013 5 09 351-361 |
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10.1134/S0016852113050026 doi (DE-627)OLC2026596603 (DE-He213)S0016852113050026-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Kotov, A. B. verfasserin aut Structural evolution and geodynamic position of the Gonzha Block, Upper Amur region 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2013 Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbaikalia. Exhumation of metamorphic rocks of the Gonzha Block resulted from a collapse of the Late Mesozoic orogen after accrecionary and collisional events related to closure of the Mongolia-Okhotsk paleooceanic basin. The structural elements that determine the main geological features of this block formed over the course of at least three deformation stages. By the onset of the third stage responsible for exhumation of metamorphic rocks pertaining to the Gonzha Group, they had already undergone complex structural transformation and metamorphism related to growth of the Amur microcontinent and its subsequent collision with the Dzhugzur-Stanovoi and Selenga-Stanovoi supperterranes of the Central Asian Foldbelt. This distinguishes the Gonzha Block from complexes of metamorphic cores in western Transbaikalia, whose structural transformation and metamorphism are directly related to their origin. Metamorphic Rock Metavolcanic Rock Argun Tectonic Transport Main Geological Feature Mazukabzov, A. M. aut Skovitina, T. M. aut Velikoslavinsky, S. D. aut Sorokin, A. A. aut Sorokin, A. P. aut Enthalten in Geotectonics Springer US, 1967 47(2013), 5 vom: Sept., Seite 351-361 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:47 year:2013 number:5 month:09 pages:351-361 https://doi.org/10.1134/S0016852113050026 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_2027 AR 47 2013 5 09 351-361 |
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10.1134/S0016852113050026 doi (DE-627)OLC2026596603 (DE-He213)S0016852113050026-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Kotov, A. B. verfasserin aut Structural evolution and geodynamic position of the Gonzha Block, Upper Amur region 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2013 Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbaikalia. Exhumation of metamorphic rocks of the Gonzha Block resulted from a collapse of the Late Mesozoic orogen after accrecionary and collisional events related to closure of the Mongolia-Okhotsk paleooceanic basin. The structural elements that determine the main geological features of this block formed over the course of at least three deformation stages. By the onset of the third stage responsible for exhumation of metamorphic rocks pertaining to the Gonzha Group, they had already undergone complex structural transformation and metamorphism related to growth of the Amur microcontinent and its subsequent collision with the Dzhugzur-Stanovoi and Selenga-Stanovoi supperterranes of the Central Asian Foldbelt. This distinguishes the Gonzha Block from complexes of metamorphic cores in western Transbaikalia, whose structural transformation and metamorphism are directly related to their origin. Metamorphic Rock Metavolcanic Rock Argun Tectonic Transport Main Geological Feature Mazukabzov, A. M. aut Skovitina, T. M. aut Velikoslavinsky, S. D. aut Sorokin, A. A. aut Sorokin, A. P. aut Enthalten in Geotectonics Springer US, 1967 47(2013), 5 vom: Sept., Seite 351-361 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:47 year:2013 number:5 month:09 pages:351-361 https://doi.org/10.1134/S0016852113050026 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_2027 AR 47 2013 5 09 351-361 |
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10.1134/S0016852113050026 doi (DE-627)OLC2026596603 (DE-He213)S0016852113050026-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Kotov, A. B. verfasserin aut Structural evolution and geodynamic position of the Gonzha Block, Upper Amur region 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2013 Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbaikalia. Exhumation of metamorphic rocks of the Gonzha Block resulted from a collapse of the Late Mesozoic orogen after accrecionary and collisional events related to closure of the Mongolia-Okhotsk paleooceanic basin. The structural elements that determine the main geological features of this block formed over the course of at least three deformation stages. By the onset of the third stage responsible for exhumation of metamorphic rocks pertaining to the Gonzha Group, they had already undergone complex structural transformation and metamorphism related to growth of the Amur microcontinent and its subsequent collision with the Dzhugzur-Stanovoi and Selenga-Stanovoi supperterranes of the Central Asian Foldbelt. This distinguishes the Gonzha Block from complexes of metamorphic cores in western Transbaikalia, whose structural transformation and metamorphism are directly related to their origin. Metamorphic Rock Metavolcanic Rock Argun Tectonic Transport Main Geological Feature Mazukabzov, A. M. aut Skovitina, T. M. aut Velikoslavinsky, S. D. aut Sorokin, A. A. aut Sorokin, A. P. aut Enthalten in Geotectonics Springer US, 1967 47(2013), 5 vom: Sept., Seite 351-361 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:47 year:2013 number:5 month:09 pages:351-361 https://doi.org/10.1134/S0016852113050026 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_2027 AR 47 2013 5 09 351-361 |
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10.1134/S0016852113050026 doi (DE-627)OLC2026596603 (DE-He213)S0016852113050026-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Kotov, A. B. verfasserin aut Structural evolution and geodynamic position of the Gonzha Block, Upper Amur region 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2013 Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbaikalia. Exhumation of metamorphic rocks of the Gonzha Block resulted from a collapse of the Late Mesozoic orogen after accrecionary and collisional events related to closure of the Mongolia-Okhotsk paleooceanic basin. The structural elements that determine the main geological features of this block formed over the course of at least three deformation stages. By the onset of the third stage responsible for exhumation of metamorphic rocks pertaining to the Gonzha Group, they had already undergone complex structural transformation and metamorphism related to growth of the Amur microcontinent and its subsequent collision with the Dzhugzur-Stanovoi and Selenga-Stanovoi supperterranes of the Central Asian Foldbelt. This distinguishes the Gonzha Block from complexes of metamorphic cores in western Transbaikalia, whose structural transformation and metamorphism are directly related to their origin. Metamorphic Rock Metavolcanic Rock Argun Tectonic Transport Main Geological Feature Mazukabzov, A. M. aut Skovitina, T. M. aut Velikoslavinsky, S. D. aut Sorokin, A. A. aut Sorokin, A. P. aut Enthalten in Geotectonics Springer US, 1967 47(2013), 5 vom: Sept., Seite 351-361 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:47 year:2013 number:5 month:09 pages:351-361 https://doi.org/10.1134/S0016852113050026 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_2027 AR 47 2013 5 09 351-361 |
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Kotov, A. B. Mazukabzov, A. M. Skovitina, T. M. Velikoslavinsky, S. D. Sorokin, A. A. Sorokin, A. P. |
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Kotov, A. B. |
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structural evolution and geodynamic position of the gonzha block, upper amur region |
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Structural evolution and geodynamic position of the Gonzha Block, Upper Amur region |
| abstract |
Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbaikalia. Exhumation of metamorphic rocks of the Gonzha Block resulted from a collapse of the Late Mesozoic orogen after accrecionary and collisional events related to closure of the Mongolia-Okhotsk paleooceanic basin. The structural elements that determine the main geological features of this block formed over the course of at least three deformation stages. By the onset of the third stage responsible for exhumation of metamorphic rocks pertaining to the Gonzha Group, they had already undergone complex structural transformation and metamorphism related to growth of the Amur microcontinent and its subsequent collision with the Dzhugzur-Stanovoi and Selenga-Stanovoi supperterranes of the Central Asian Foldbelt. This distinguishes the Gonzha Block from complexes of metamorphic cores in western Transbaikalia, whose structural transformation and metamorphism are directly related to their origin. © Pleiades Publishing, Inc. 2013 |
| abstractGer |
Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbaikalia. Exhumation of metamorphic rocks of the Gonzha Block resulted from a collapse of the Late Mesozoic orogen after accrecionary and collisional events related to closure of the Mongolia-Okhotsk paleooceanic basin. The structural elements that determine the main geological features of this block formed over the course of at least three deformation stages. By the onset of the third stage responsible for exhumation of metamorphic rocks pertaining to the Gonzha Group, they had already undergone complex structural transformation and metamorphism related to growth of the Amur microcontinent and its subsequent collision with the Dzhugzur-Stanovoi and Selenga-Stanovoi supperterranes of the Central Asian Foldbelt. This distinguishes the Gonzha Block from complexes of metamorphic cores in western Transbaikalia, whose structural transformation and metamorphism are directly related to their origin. © Pleiades Publishing, Inc. 2013 |
| abstract_unstemmed |
Abstract As follows from the results of a structural study and available geochronological constraints, the Gonzha Block located in the northeastern Argun-Idermeg Superterrane of the Central Asian Foldbelt is similar to Late Mesozoic (133−119 Ma) Cordilleran-type metamorphic cores of western Transbaikalia. Exhumation of metamorphic rocks of the Gonzha Block resulted from a collapse of the Late Mesozoic orogen after accrecionary and collisional events related to closure of the Mongolia-Okhotsk paleooceanic basin. The structural elements that determine the main geological features of this block formed over the course of at least three deformation stages. By the onset of the third stage responsible for exhumation of metamorphic rocks pertaining to the Gonzha Group, they had already undergone complex structural transformation and metamorphism related to growth of the Amur microcontinent and its subsequent collision with the Dzhugzur-Stanovoi and Selenga-Stanovoi supperterranes of the Central Asian Foldbelt. This distinguishes the Gonzha Block from complexes of metamorphic cores in western Transbaikalia, whose structural transformation and metamorphism are directly related to their origin. © Pleiades Publishing, Inc. 2013 |
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Structural evolution and geodynamic position of the Gonzha Block, Upper Amur region |
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