MELTING OF ACCRETIONARY WEDGE AND BUILDING MATURE CONTINENTAL CRUST: INSIGHTS FROM THE MAGMATIC EVOLUTION OF THE CHINESE ALTAI OROGEN, CENTRAL ASIA
Tectonic-magmatic reworking of accretionary wedges is a key process responsible for differentiation and stabilization of continental crustal in accretionary orogens. This generic problem can be exemplified by magmatic evolution of the Chinese Altai which represents a high-grade core of the world...
Saved in:
| Main Authors: | , , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2017-09-01
|
| Series: | Геодинамика и тектонофизика |
| Online Access: | https://www.gt-crust.ru/jour/article/view/409 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| _version_ | 1849338653812195328 |
|---|---|
| author | Yingde Jiang Karel Schulmann Min Sun Pavla Štípská Alexandra Guy Ondrej Lexa Vojetch Janoušek Chao Yuan |
| author_facet | Yingde Jiang Karel Schulmann Min Sun Pavla Štípská Alexandra Guy Ondrej Lexa Vojetch Janoušek Chao Yuan |
| author_sort | Yingde Jiang |
| collection | DOAJ |
| description | Tectonic-magmatic reworking of accretionary wedges is a key process responsible for differentiation and stabilization of continental crustal in accretionary orogens. This generic problem can be exemplified by magmatic evolution of the Chinese Altai which represents a high-grade core of the world's largest accretionary system, namely the Central Asian Orogenic Belt (CAOB). In the Chinese Altai, voluminous SilurianDevonian granitoids intruding a greywacke-dominated Ordovician flysch sequence. These intrusions are classically interpreted to originate from predominant (70‒90 %) juvenile (depleted mantle-derived) magma. However, their close temporal and spatial relationship with the regional anatexis of flysch rocks, allows us to examine the possibility that they were mainly derived from flysch rocks. |
| format | Article |
| id | doaj-art-75dc957ec726418aa8a6690adaa52f3f |
| institution | Kabale University |
| issn | 2078-502X |
| language | English |
| publishDate | 2017-09-01 |
| publisher | Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust |
| record_format | Article |
| series | Геодинамика и тектонофизика |
| spelling | doaj-art-75dc957ec726418aa8a6690adaa52f3f2025-08-20T03:44:20ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2017-09-018348148210.5800/GT-2017-8-3-0268268MELTING OF ACCRETIONARY WEDGE AND BUILDING MATURE CONTINENTAL CRUST: INSIGHTS FROM THE MAGMATIC EVOLUTION OF THE CHINESE ALTAI OROGEN, CENTRAL ASIAYingde Jiang0Karel Schulmann1Min Sun2Pavla Štípská3Alexandra Guy4Ondrej Lexa5Vojetch Janoušek6Chao Yuan7Guangzhou Institute of Geochemistry, Chinese Academy of SciencesCenter of Lithospheric Research, Czech Geological SurveyThe University of Hong KongCenter of Lithospheric Research, Czech Geological SurveyCenter of Lithospheric Research, Czech Geological SurveyInstitute of Petrology and Structural Geology, Charles UniversityCenter of Lithospheric Research, Czech Geological SurveyGuangzhou Institute of Geochemistry, Chinese Academy of SciencesTectonic-magmatic reworking of accretionary wedges is a key process responsible for differentiation and stabilization of continental crustal in accretionary orogens. This generic problem can be exemplified by magmatic evolution of the Chinese Altai which represents a high-grade core of the world's largest accretionary system, namely the Central Asian Orogenic Belt (CAOB). In the Chinese Altai, voluminous SilurianDevonian granitoids intruding a greywacke-dominated Ordovician flysch sequence. These intrusions are classically interpreted to originate from predominant (70‒90 %) juvenile (depleted mantle-derived) magma. However, their close temporal and spatial relationship with the regional anatexis of flysch rocks, allows us to examine the possibility that they were mainly derived from flysch rocks.https://www.gt-crust.ru/jour/article/view/409 |
| spellingShingle | Yingde Jiang Karel Schulmann Min Sun Pavla Štípská Alexandra Guy Ondrej Lexa Vojetch Janoušek Chao Yuan MELTING OF ACCRETIONARY WEDGE AND BUILDING MATURE CONTINENTAL CRUST: INSIGHTS FROM THE MAGMATIC EVOLUTION OF THE CHINESE ALTAI OROGEN, CENTRAL ASIA Геодинамика и тектонофизика |
| title | MELTING OF ACCRETIONARY WEDGE AND BUILDING MATURE CONTINENTAL CRUST: INSIGHTS FROM THE MAGMATIC EVOLUTION OF THE CHINESE ALTAI OROGEN, CENTRAL ASIA |
| title_full | MELTING OF ACCRETIONARY WEDGE AND BUILDING MATURE CONTINENTAL CRUST: INSIGHTS FROM THE MAGMATIC EVOLUTION OF THE CHINESE ALTAI OROGEN, CENTRAL ASIA |
| title_fullStr | MELTING OF ACCRETIONARY WEDGE AND BUILDING MATURE CONTINENTAL CRUST: INSIGHTS FROM THE MAGMATIC EVOLUTION OF THE CHINESE ALTAI OROGEN, CENTRAL ASIA |
| title_full_unstemmed | MELTING OF ACCRETIONARY WEDGE AND BUILDING MATURE CONTINENTAL CRUST: INSIGHTS FROM THE MAGMATIC EVOLUTION OF THE CHINESE ALTAI OROGEN, CENTRAL ASIA |
| title_short | MELTING OF ACCRETIONARY WEDGE AND BUILDING MATURE CONTINENTAL CRUST: INSIGHTS FROM THE MAGMATIC EVOLUTION OF THE CHINESE ALTAI OROGEN, CENTRAL ASIA |
| title_sort | melting of accretionary wedge and building mature continental crust insights from the magmatic evolution of the chinese altai orogen central asia |
| url | https://www.gt-crust.ru/jour/article/view/409 |
| work_keys_str_mv | AT yingdejiang meltingofaccretionarywedgeandbuildingmaturecontinentalcrustinsightsfromthemagmaticevolutionofthechinesealtaiorogencentralasia AT karelschulmann meltingofaccretionarywedgeandbuildingmaturecontinentalcrustinsightsfromthemagmaticevolutionofthechinesealtaiorogencentralasia AT minsun meltingofaccretionarywedgeandbuildingmaturecontinentalcrustinsightsfromthemagmaticevolutionofthechinesealtaiorogencentralasia AT pavlastipska meltingofaccretionarywedgeandbuildingmaturecontinentalcrustinsightsfromthemagmaticevolutionofthechinesealtaiorogencentralasia AT alexandraguy meltingofaccretionarywedgeandbuildingmaturecontinentalcrustinsightsfromthemagmaticevolutionofthechinesealtaiorogencentralasia AT ondrejlexa meltingofaccretionarywedgeandbuildingmaturecontinentalcrustinsightsfromthemagmaticevolutionofthechinesealtaiorogencentralasia AT vojetchjanousek meltingofaccretionarywedgeandbuildingmaturecontinentalcrustinsightsfromthemagmaticevolutionofthechinesealtaiorogencentralasia AT chaoyuan meltingofaccretionarywedgeandbuildingmaturecontinentalcrustinsightsfromthemagmaticevolutionofthechinesealtaiorogencentralasia |