CO-EVOLUTION OF PROTEROZOIC CRATONIC FRAGMENTS IN WESTERN AND NORTHERN MONGOLIA
CAOB occupies a vast area that extends from the Urals to the Far East Asia and from the Siberian craton to the North China and Tarim cratons (Fig. 1, A). In order to better constrain Precambrian tectonic evolution of the CAOB, it is important to revisit Precambrian terranes of Mongolia as outlined i...
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| Format: | Article |
| Language: | English |
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Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2017-09-01
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| Series: | Геодинамика и тектонофизика |
| Online Access: | https://www.gt-crust.ru/jour/article/view/392 |
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| _version_ | 1849242592009519104 |
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| author | Uyanga Bold Francis Macdonald Yukio Isozaki |
| author_facet | Uyanga Bold Francis Macdonald Yukio Isozaki |
| author_sort | Uyanga Bold |
| collection | DOAJ |
| description | CAOB occupies a vast area that extends from the Urals to the Far East Asia and from the Siberian craton to the North China and Tarim cratons (Fig. 1, A). In order to better constrain Precambrian tectonic evolution of the CAOB, it is important to revisit Precambrian terranes of Mongolia as outlined in Badarch et al. [2002] that contain Archean to Proterozoic metamorphic basement and Neoproterozoic metasedimentary and volcanic rocks. |
| format | Article |
| id | doaj-art-67af15ddbeab4c458055fbe173fdcaae |
| 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-67af15ddbeab4c458055fbe173fdcaae2025-08-20T03:59:47ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2017-09-018341742010.5800/GT-2017-8-3-0251251CO-EVOLUTION OF PROTEROZOIC CRATONIC FRAGMENTS IN WESTERN AND NORTHERN MONGOLIAUyanga Bold0Francis Macdonald1Yukio Isozaki2University of TokyoHarvard UniversityUniversity of TokyoCAOB occupies a vast area that extends from the Urals to the Far East Asia and from the Siberian craton to the North China and Tarim cratons (Fig. 1, A). In order to better constrain Precambrian tectonic evolution of the CAOB, it is important to revisit Precambrian terranes of Mongolia as outlined in Badarch et al. [2002] that contain Archean to Proterozoic metamorphic basement and Neoproterozoic metasedimentary and volcanic rocks.https://www.gt-crust.ru/jour/article/view/392 |
| spellingShingle | Uyanga Bold Francis Macdonald Yukio Isozaki CO-EVOLUTION OF PROTEROZOIC CRATONIC FRAGMENTS IN WESTERN AND NORTHERN MONGOLIA Геодинамика и тектонофизика |
| title | CO-EVOLUTION OF PROTEROZOIC CRATONIC FRAGMENTS IN WESTERN AND NORTHERN MONGOLIA |
| title_full | CO-EVOLUTION OF PROTEROZOIC CRATONIC FRAGMENTS IN WESTERN AND NORTHERN MONGOLIA |
| title_fullStr | CO-EVOLUTION OF PROTEROZOIC CRATONIC FRAGMENTS IN WESTERN AND NORTHERN MONGOLIA |
| title_full_unstemmed | CO-EVOLUTION OF PROTEROZOIC CRATONIC FRAGMENTS IN WESTERN AND NORTHERN MONGOLIA |
| title_short | CO-EVOLUTION OF PROTEROZOIC CRATONIC FRAGMENTS IN WESTERN AND NORTHERN MONGOLIA |
| title_sort | co evolution of proterozoic cratonic fragments in western and northern mongolia |
| url | https://www.gt-crust.ru/jour/article/view/392 |
| work_keys_str_mv | AT uyangabold coevolutionofproterozoiccratonicfragmentsinwesternandnorthernmongolia AT francismacdonald coevolutionofproterozoiccratonicfragmentsinwesternandnorthernmongolia AT yukioisozaki coevolutionofproterozoiccratonicfragmentsinwesternandnorthernmongolia |