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
Abstract
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).
About the Authors
Peng Peng
Institute of Geology and Geophysics, Chinese Academy of Sciences
China
China
State Key Laboratory of Lithospheric Evolution,
Chinese Academy of Sciences,
Mingguo Zhai
Institute of Geology and Geophysics, Chinese Academy of Sciences
China
China
State Key Laboratory of Lithospheric Evolution,
Chinese Academy of Sciences,
Xiangdong Su
Institute of Geology and Geophysics, Chinese Academy of Sciences
China
China
State Key Laboratory of Lithospheric Evolution,
Chinese Academy of Sciences,
Taiping Zhao
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences
China
Guangzhou 510640
China
Guangzhou 510640
Yanyan Zhou
Institute of Geology and Geophysics, Chinese Academy of Sciences
China
China
State Key Laboratory of Lithospheric Evolution,
Chinese Academy of Sciences,
Review
For citations:
Peng P., Zhai M., Su X., Zhao T., Zhou Ya. 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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