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P-ISSN 0002-9599
E-ISSN 1945-452X
Science Paper
Vol. 314, Issue 2, 2014February 01, 2014 EDT

Geochronologic and Geochemical Evidence for Persistence of South-Dipping Subduction to Late Permian Time, Langshan Area, Inner Mongolia (China): Significance for Termination of Accretionary Orogenesis in the Southern Altaids

Li'na Lin, Wenjiao Xiao, Bo Wan, Brian F. Windley, Songjian Ao, Chunming Han, Jianyun Feng, Ji'en Zhang, Zhiyong Zhang,
LangshanPermianaccretionary tectonicsNorth China CratonAndean-type arc
https://doi.org/10.2475/02.2014.08
American Journal of Science
Lin, L., Xiao, W., Wan, B., Windley, B. F., Ao, S., Han, C., Feng, J., Zhang, J., & Zhang, Z. (2014). Geochronologic and Geochemical Evidence for Persistence of South-Dipping Subduction to Late Permian Time, Langshan Area, Inner Mongolia (China): Significance for Termination of Accretionary Orogenesis in the Southern Altaids. American Journal of Science, 314(2), 679–703. https:/​/​doi.org/​10.2475/​02.2014.08

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