Tectonic structure and evolution of the Hissar–Alay Mountain Domain and the Pamirs
Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Leonov, M. G. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Inc. 2017 |
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| Übergeordnetes Werk: |
Enthalten in: Geotectonics - Pleiades Publishing, 1967, 51(2017), 6 vom: Nov., Seite 566-583 |
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| Übergeordnetes Werk: |
volume:51 ; year:2017 ; number:6 ; month:11 ; pages:566-583 |
| Links: |
|---|
| DOI / URN: |
10.1134/S001685211706005X |
|---|
| Katalog-ID: |
OLC2026598118 |
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| 520 | |a Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure, geometry, tectonic style, the set of kinematic parageneses, sequence of events, and the manifestation of magmatism, metamorphism, and recent orogeny. These regions belong to different segments of the Earth’s crust. In other words, they represent two distinct historical–structural–geological provinces belonging to different mobile belts of Asia: the Hissar–Alay MD is incorporated into the structure of the Central Asian (Ural–Mongolia) Belt in contrast to the Pamirs, which is a constituent of the Alpine–Himalayan Belt. The Hissar (Gissar)–Alay MD and the Pamirs formed independently and did not reveal significant geodynamic interaction. | ||
| 650 | 4 | |a geodynamics | |
| 650 | 4 | |a Hissar (Gissar)–Alay Mountain Domain | |
| 650 | 4 | |a orogen | |
| 650 | 4 | |a collision | |
| 650 | 4 | |a morphology, Pamirs (or Pamir) | |
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| 650 | 4 | |a synform | |
| 650 | 4 | |a tectonic structure | |
| 700 | 1 | |a Rybin, A. K. |4 aut | |
| 700 | 1 | |a Batalev, V. Yu. |4 aut | |
| 700 | 1 | |a Matyukov, V. E. |4 aut | |
| 700 | 1 | |a Shchelochkov, G. G. |4 aut | |
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10.1134/S001685211706005X doi (DE-627)OLC2026598118 (DE-He213)S001685211706005X-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Leonov, M. G. verfasserin aut Tectonic structure and evolution of the Hissar–Alay Mountain Domain and the Pamirs 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2017 Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure, geometry, tectonic style, the set of kinematic parageneses, sequence of events, and the manifestation of magmatism, metamorphism, and recent orogeny. These regions belong to different segments of the Earth’s crust. In other words, they represent two distinct historical–structural–geological provinces belonging to different mobile belts of Asia: the Hissar–Alay MD is incorporated into the structure of the Central Asian (Ural–Mongolia) Belt in contrast to the Pamirs, which is a constituent of the Alpine–Himalayan Belt. The Hissar (Gissar)–Alay MD and the Pamirs formed independently and did not reveal significant geodynamic interaction. geodynamics Hissar (Gissar)–Alay Mountain Domain orogen collision morphology, Pamirs (or Pamir) mobile belt synform tectonic structure Rybin, A. K. aut Batalev, V. Yu. aut Matyukov, V. E. aut Shchelochkov, G. G. aut Enthalten in Geotectonics Pleiades Publishing, 1967 51(2017), 6 vom: Nov., Seite 566-583 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:51 year:2017 number:6 month:11 pages:566-583 https://doi.org/10.1134/S001685211706005X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO AR 51 2017 6 11 566-583 |
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10.1134/S001685211706005X doi (DE-627)OLC2026598118 (DE-He213)S001685211706005X-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Leonov, M. G. verfasserin aut Tectonic structure and evolution of the Hissar–Alay Mountain Domain and the Pamirs 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2017 Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure, geometry, tectonic style, the set of kinematic parageneses, sequence of events, and the manifestation of magmatism, metamorphism, and recent orogeny. These regions belong to different segments of the Earth’s crust. In other words, they represent two distinct historical–structural–geological provinces belonging to different mobile belts of Asia: the Hissar–Alay MD is incorporated into the structure of the Central Asian (Ural–Mongolia) Belt in contrast to the Pamirs, which is a constituent of the Alpine–Himalayan Belt. The Hissar (Gissar)–Alay MD and the Pamirs formed independently and did not reveal significant geodynamic interaction. geodynamics Hissar (Gissar)–Alay Mountain Domain orogen collision morphology, Pamirs (or Pamir) mobile belt synform tectonic structure Rybin, A. K. aut Batalev, V. Yu. aut Matyukov, V. E. aut Shchelochkov, G. G. aut Enthalten in Geotectonics Pleiades Publishing, 1967 51(2017), 6 vom: Nov., Seite 566-583 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:51 year:2017 number:6 month:11 pages:566-583 https://doi.org/10.1134/S001685211706005X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO AR 51 2017 6 11 566-583 |
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10.1134/S001685211706005X doi (DE-627)OLC2026598118 (DE-He213)S001685211706005X-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Leonov, M. G. verfasserin aut Tectonic structure and evolution of the Hissar–Alay Mountain Domain and the Pamirs 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2017 Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure, geometry, tectonic style, the set of kinematic parageneses, sequence of events, and the manifestation of magmatism, metamorphism, and recent orogeny. These regions belong to different segments of the Earth’s crust. In other words, they represent two distinct historical–structural–geological provinces belonging to different mobile belts of Asia: the Hissar–Alay MD is incorporated into the structure of the Central Asian (Ural–Mongolia) Belt in contrast to the Pamirs, which is a constituent of the Alpine–Himalayan Belt. The Hissar (Gissar)–Alay MD and the Pamirs formed independently and did not reveal significant geodynamic interaction. geodynamics Hissar (Gissar)–Alay Mountain Domain orogen collision morphology, Pamirs (or Pamir) mobile belt synform tectonic structure Rybin, A. K. aut Batalev, V. Yu. aut Matyukov, V. E. aut Shchelochkov, G. G. aut Enthalten in Geotectonics Pleiades Publishing, 1967 51(2017), 6 vom: Nov., Seite 566-583 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:51 year:2017 number:6 month:11 pages:566-583 https://doi.org/10.1134/S001685211706005X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO AR 51 2017 6 11 566-583 |
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10.1134/S001685211706005X doi (DE-627)OLC2026598118 (DE-He213)S001685211706005X-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Leonov, M. G. verfasserin aut Tectonic structure and evolution of the Hissar–Alay Mountain Domain and the Pamirs 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2017 Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure, geometry, tectonic style, the set of kinematic parageneses, sequence of events, and the manifestation of magmatism, metamorphism, and recent orogeny. These regions belong to different segments of the Earth’s crust. In other words, they represent two distinct historical–structural–geological provinces belonging to different mobile belts of Asia: the Hissar–Alay MD is incorporated into the structure of the Central Asian (Ural–Mongolia) Belt in contrast to the Pamirs, which is a constituent of the Alpine–Himalayan Belt. The Hissar (Gissar)–Alay MD and the Pamirs formed independently and did not reveal significant geodynamic interaction. geodynamics Hissar (Gissar)–Alay Mountain Domain orogen collision morphology, Pamirs (or Pamir) mobile belt synform tectonic structure Rybin, A. K. aut Batalev, V. Yu. aut Matyukov, V. E. aut Shchelochkov, G. G. aut Enthalten in Geotectonics Pleiades Publishing, 1967 51(2017), 6 vom: Nov., Seite 566-583 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:51 year:2017 number:6 month:11 pages:566-583 https://doi.org/10.1134/S001685211706005X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO AR 51 2017 6 11 566-583 |
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10.1134/S001685211706005X doi (DE-627)OLC2026598118 (DE-He213)S001685211706005X-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Leonov, M. G. verfasserin aut Tectonic structure and evolution of the Hissar–Alay Mountain Domain and the Pamirs 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2017 Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure, geometry, tectonic style, the set of kinematic parageneses, sequence of events, and the manifestation of magmatism, metamorphism, and recent orogeny. These regions belong to different segments of the Earth’s crust. In other words, they represent two distinct historical–structural–geological provinces belonging to different mobile belts of Asia: the Hissar–Alay MD is incorporated into the structure of the Central Asian (Ural–Mongolia) Belt in contrast to the Pamirs, which is a constituent of the Alpine–Himalayan Belt. The Hissar (Gissar)–Alay MD and the Pamirs formed independently and did not reveal significant geodynamic interaction. geodynamics Hissar (Gissar)–Alay Mountain Domain orogen collision morphology, Pamirs (or Pamir) mobile belt synform tectonic structure Rybin, A. K. aut Batalev, V. Yu. aut Matyukov, V. E. aut Shchelochkov, G. G. aut Enthalten in Geotectonics Pleiades Publishing, 1967 51(2017), 6 vom: Nov., Seite 566-583 (DE-627)129594733 (DE-600)240564-7 (DE-576)01508762X 0016-8521 nnns volume:51 year:2017 number:6 month:11 pages:566-583 https://doi.org/10.1134/S001685211706005X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO AR 51 2017 6 11 566-583 |
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10.1134/S001685211706005X |
| dewey-full |
550 |
| title_sort |
tectonic structure and evolution of the hissar–alay mountain domain and the pamirs |
| title_auth |
Tectonic structure and evolution of the Hissar–Alay Mountain Domain and the Pamirs |
| abstract |
Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure, geometry, tectonic style, the set of kinematic parageneses, sequence of events, and the manifestation of magmatism, metamorphism, and recent orogeny. These regions belong to different segments of the Earth’s crust. In other words, they represent two distinct historical–structural–geological provinces belonging to different mobile belts of Asia: the Hissar–Alay MD is incorporated into the structure of the Central Asian (Ural–Mongolia) Belt in contrast to the Pamirs, which is a constituent of the Alpine–Himalayan Belt. The Hissar (Gissar)–Alay MD and the Pamirs formed independently and did not reveal significant geodynamic interaction. © Pleiades Publishing, Inc. 2017 |
| abstractGer |
Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure, geometry, tectonic style, the set of kinematic parageneses, sequence of events, and the manifestation of magmatism, metamorphism, and recent orogeny. These regions belong to different segments of the Earth’s crust. In other words, they represent two distinct historical–structural–geological provinces belonging to different mobile belts of Asia: the Hissar–Alay MD is incorporated into the structure of the Central Asian (Ural–Mongolia) Belt in contrast to the Pamirs, which is a constituent of the Alpine–Himalayan Belt. The Hissar (Gissar)–Alay MD and the Pamirs formed independently and did not reveal significant geodynamic interaction. © Pleiades Publishing, Inc. 2017 |
| abstract_unstemmed |
Abstract The paper presents a comparative description of two large mountain systems in the intracontinental Eurasian Orogen: the Hissar (Gissar)–Alay Mountain Domain (MD) and the Pamirs (or Pamir). It has been established that the Hissar–Alay MD and the Pamirs substantially differ in morphostructure, geometry, tectonic style, the set of kinematic parageneses, sequence of events, and the manifestation of magmatism, metamorphism, and recent orogeny. These regions belong to different segments of the Earth’s crust. In other words, they represent two distinct historical–structural–geological provinces belonging to different mobile belts of Asia: the Hissar–Alay MD is incorporated into the structure of the Central Asian (Ural–Mongolia) Belt in contrast to the Pamirs, which is a constituent of the Alpine–Himalayan Belt. The Hissar (Gissar)–Alay MD and the Pamirs formed independently and did not reveal significant geodynamic interaction. © Pleiades Publishing, Inc. 2017 |
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| title_short |
Tectonic structure and evolution of the Hissar–Alay Mountain Domain and the Pamirs |
| url |
https://doi.org/10.1134/S001685211706005X |
| remote_bool |
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| author2 |
Rybin, A. K. Batalev, V. Yu Matyukov, V. E. Shchelochkov, G. G. |
| author2Str |
Rybin, A. K. Batalev, V. Yu Matyukov, V. E. Shchelochkov, G. G. |
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