匈奴超地体
（重定向自匈奴地体）
匈奴超地体（Hunic superterrane）是一个地质史上的超地体，现在附着于欧亚大陆。 [1]
奥陶纪末志留紀初，从冈瓦纳大陆分离下来，向北移动，于石炭纪初的华西里造山运动与劳亚大陆接触、碰撞，形成了钦察弧[2]。但它并不是单一的地体，而是可分为两群：欧洲匈奴地体、亚洲匈奴地体。[3][4][5]
参见
[编辑]参考文献
[编辑]- ^ Stampfli 2000，Palaeotethys, p. 3; "it contains most of the areas devastated by Attila!"
- ^ Fielding, Frank & Isbell 2008，第11頁
- ^ Muttoni et al. 2009，Fig. 2, p. 19
- ^ Stampfli, von Raumer & Borel 2002，Middle Devonian Phase, p. 272
- ^ Stampfli, von Raumer & Borel 2002，Fig. 3, pp. 268–629
源文献
[编辑]- Muttoni, G.; Gaetani, M.; Kent, D. V.; Sciunnach, D.; Angiolini, L.; Berra, F.; Garzanti, E.; Mattei, M.; Zanchi, A. Opening of the Neo-Tethys Ocean and the Pangea B to Pangea A transformation during the Permian (PDF). GeoArabia. 2009, 14 (4): 17–48 [1 November 2015]. （原始内容存档 (PDF)于2017-08-09）.
- Stampfli, G. M. Tethyan oceans (PDF). Geological Society, London, Special Publications. 2000, 173 (1): 1–23 [30 November 2019]. Bibcode:2000GSLSP.173....1S. doi:10.1144/GSL.SP.2000.173.01.01.
- Stampfli, G. M.; von Raumer, J. F.; Borel, G. D. Paleozoic evolution of pre-Variscan terranes: From Gondwana to the Variscan collision (PDF). Catalán, M.; Hatcher, R. D., Jr.; Arenas, R.; et al (编). Variscan-Appalachian dynamics: The building of the late Paleozoic basement (PDF). Boulder, Colorado: Geological Society of America Special Paper 364. 2002: 263–280 [1 January 2017]. ISBN 9780813723648. doi:10.1130/0-8137-2364-7.263.
- Fielding, Christopher; Frank, Tracy; Isbell, John. Resolving the Late Paleozoic Ice Age in Time and Space. Geological Society of America. 1 January 2008 [4 November 2019]. ISBN 9780813724416.