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
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,
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