华力西造山运动
华力西造山运动（英语：Variscan orogeny），又称海西造山运动（英语：Hercynian orogeny），是指古生代晚期欧美大陆与冈瓦纳大陆碰撞形成盘古超大陸的地质造山事件。
参考资料
- ^ Based on Matte 2001 and Ziegler 1990
更多阅读
- Matte, P. The Variscan collage and orogeny (480 ±290 Ma) and the tectonic definition of the Armorica microplate: a review. Terra Nova. 2001, 13 (2): 122–128. Bibcode:2001TeNov..13..122M. doi:10.1046/j.1365-3121.2001.00327.x.
- Ziegler, P.A. Geological Atlas of Western and Central Europe 2. Shell Internationale Petroleum Maatschappij BV. 1990. ISBN 978-90-6644-125-5.
- von Raumer, J.; Stampfli, G.M.; Borel, G.D.; Bussy, F. The organisation of pre-Variscan basement areas at the north-Gondwanan margin (PDF). International Journal of Earth Sciences. 2002, 91: 35–52. Bibcode:2002IJEaS..91...35V. doi:10.1007/s005310100200.
- von Raumer, J.; Stampfli, G.M.; Bussy, F. Gondwana-derived microcontinents - the constituents of the Variscan and Alpine collisional orogens. Tectonophysics. 2003, 365 (1–4): 7–22. Bibcode:10.1.1.430.1420 请检查
|bibcode=值 (帮助). doi:10.1016/S0040-1951(03)00015-5. - Stampfli, GM; Borel, GD. Cavazza W, Roure F, Spakman W, Stampfli GM, Ziegler P , 编. The TRANSMED Atlas: the Mediterranean Region from Crust to Mantle. Springer Verlag. 2004. ISBN 978-3-540-22181-4.
