Study on Volcanoes and Maars in China
Even no fascinating volcanic eruptions occurred in China in modern time, there are many Cenozoic volcanoes and volcanic rocks almost distributed in the whole country, especially in the eastern continental margin and the southwestern Tibetan Plateau. Most volcanic activities took by central eruptions with basaltic magma and formed monogenic volcanoes and lava flows, of which the Neogene basalts usually located in high terraces and the Quaternary basalts distributed in valleys. The dominant volcanic rocks in China are continental intraplate basalts with high alkali in the eastern continental margin, and trachyte-basalt, shoshonite with high potassium in the Tibetan Plateau.
Cenozoic volcano Changbaishan maars in China
Jiaqi Liu Jing Wu Guoqiang Chu Qiang Liu Zhengfu Guo Jingtai Han Patrick Rioual Jorg F.W. Negendank Achim Brauer Jens Mingram Chunqing Sun Lei Zhang Jiali Liu Shuangshaung Chen Leilei Ding
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Aca Helmholtz Centre Potsdam, German Research Centre for Geosciences GFZ, Section 5.2 Climate Dynamics a
国际会议
The 6th International Maar Conference(IMC)(第六届国际玛珥会议)
长春
英文
61-62
2016-07-30(万方平台首次上网日期,不代表论文的发表时间)