NATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGEN
There are two episodes of magmatism along the northern margin of the North China block during the Late Carboniferous to Late Triassic, one at 310–250 Ma (Late Carboniferous to Permian) and the other at 235–210 Ma (Late Triassic). The former group comprises plutonic rocks (gabbro-diorite-monzodiorite...
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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/423 |
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| _version_ | 1849338668977750016 |
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| author | Peng Peng Mingguo Zhai Xiangdong Su Taiping Zhao Yanyan Zhou |
| author_facet | Peng Peng Mingguo Zhai Xiangdong Su Taiping Zhao Yanyan Zhou |
| author_sort | Peng Peng |
| collection | DOAJ |
| description | There are two episodes of magmatism along the northern margin of the North China block during the Late Carboniferous to Late Triassic, one at 310–250 Ma (Late Carboniferous to Permian) and the other at 235–210 Ma (Late Triassic). The former group comprises plutonic rocks (gabbro-diorite-monzodioritemonzogranite-granite), mafic to intermediate dykes (diorite to dolerite) and a few felsic volcanics (andesite to dacite). |
| format | Article |
| id | doaj-art-b6b59f7e517a4c148725e5bca8af65cd |
| 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-b6b59f7e517a4c148725e5bca8af65cd2025-08-20T03:44:20ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2017-09-018353153210.5800/GT-2017-8-3-0282282NATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGENPeng Peng0Mingguo Zhai1Xiangdong Su2Taiping Zhao3Yanyan Zhou4Institute of Geology and Geophysics, Chinese Academy of SciencesInstitute of Geology and Geophysics, Chinese Academy of SciencesInstitute of Geology and Geophysics, Chinese Academy of SciencesGuangzhou Institute of Geochemistry, Chinese Academy of SciencesInstitute of Geology and Geophysics, Chinese Academy of SciencesThere are two episodes of magmatism along the northern margin of the North China block during the Late Carboniferous to Late Triassic, one at 310–250 Ma (Late Carboniferous to Permian) and the other at 235–210 Ma (Late Triassic). The former group comprises plutonic rocks (gabbro-diorite-monzodioritemonzogranite-granite), mafic to intermediate dykes (diorite to dolerite) and a few felsic volcanics (andesite to dacite).https://www.gt-crust.ru/jour/article/view/423 |
| spellingShingle | Peng Peng Mingguo Zhai Xiangdong Su Taiping Zhao Yanyan Zhou NATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGEN Геодинамика и тектонофизика |
| title | NATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGEN |
| title_full | NATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGEN |
| title_fullStr | NATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGEN |
| title_full_unstemmed | NATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGEN |
| title_short | NATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGEN |
| title_sort | nature of the late carboniferous to triassic magmatism along the northern margin of the north china block link with the evolution of the central asian orogen |
| url | https://www.gt-crust.ru/jour/article/view/423 |
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