Tectono-thermal evolution of middle-south section of the Da Hinggan Mountains

Author:

Shao Ji’an,Zhang Lüqiao,Mu Baolei

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference14 articles.

1. Shao Ji’an, Tang Kedong, Deuteric tectonic feature of Hinggan-Mongolian orogenic belt, inContributions for Chinese Continental Tectonics (ed. Ma Xingyuan) (in Chinese), Beijing:Publishing House of China University of Geosciences, 1992, 43–50.

2. Hong Dawei, Wang Shiguan, Huang Huaizeng, Preliminary study of the Late Palaeozoic-Triassic alkaline granite belt in northem territory of China and adjacent areas and its geodynamic significance, inContributions on Grantoids and Their Minerogenesis in Northern China (ed. Li Zitong) (in Chinese), Beijing:Geological Publishing House, 1991, 40–48.

3. Shao Ji’an, Mu Baolei, He Guogi, Zhang Lüqiao, Geological effects in tectonic upperposition of Paleo-Pacific domain and Paleo-Asian domain,Science in China, Ser. D, 1997, 40(6):634.

4. Deng Jinfu, Zhao Hailing, Mo Xuanxue et al.,Continental Roots-plume Tectonics of China—Key to the Continental Dynamics (in Chinese), Beijing:Geological Publishing House, 1996, 16.

5. Li Peizhong, Yu Jinsheng, The age and significance of Nianzishan vuggy alkaline granite, Hailong,Geochemistry (in Chinese), 1993, (4):389.

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