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Геодинамика и тектонофизика

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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

https://doi.org/10.5800/GT-2017-8-3-0282

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Аннотация

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).

Об авторах

Peng Peng
Institute of Geology and Geophysics, Chinese Academy of Sciences
Китай

State Key Laboratory of Lithospheric Evolution,

Beijing 100029



Mingguo Zhai
Institute of Geology and Geophysics, Chinese Academy of Sciences
Китай

State Key Laboratory of Lithospheric Evolution,

Beijing 100029



Xiangdong Su
Institute of Geology and Geophysics, Chinese Academy of Sciences
Китай

State Key Laboratory of Lithospheric Evolution,

Beijing 100029



Taiping Zhao
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences
Китай
Guangzhou 510640


Yanyan Zhou
Institute of Geology and Geophysics, Chinese Academy of Sciences
Китай

State Key Laboratory of Lithospheric Evolution,

Beijing 100029



Для цитирования:


Peng P., Zhai M., Su X., Zhao T., Zhou Y. 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. 2017;8(3):531-532. https://doi.org/10.5800/GT-2017-8-3-0282

For citation:


Peng P., Zhai M., Su X., Zhao T., Zhou Y. 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. Geodynamics & Tectonophysics. 2017;8(3):531-532. https://doi.org/10.5800/GT-2017-8-3-0282

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ISSN 2078-502X (Online)