Research Paper GEOSPHERE Geologic framework of the northern Indo-Burma Ranges and lateral correlation of Himalayan-Tibetan lithologic units across the GEOSPHERE, v. 15, no. 3 eastern Himalayan syntaxis https://doi.org/10.1130/GES02054.1 Peter J. Haproff1,2, Andrew V. Zuza3, An Yin2, T. Mark Harrison2, Craig E. Manning2, Chandra S. Dubey4, Lin Ding5, Chen Wu6, and Jianlin Chen7 1Department of Earth and Ocean Sciences, University of North Carolina, Wilmington, North Carolina 28403, USA 17 figures; 3 tables; 1 set of supplemental files 2Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, California 90095, USA 3Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA 4 CORRESPONDENCE:
[email protected] Department of Geology, Delhi University, Delhi 110007, India 5Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China 6Structural Geology Group, China University of Geosciences, Beijing 100083, China CITATION: Haproff, P.J., Zuza, A.V., Yin, A., Harrison, 7State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China T.M., Manning, C.E., Dubey, C.S., Ding, L., Wu, C., and Chen, J.L., 2019, Geologic framework of the north- ern Indo-Burma Ranges and lateral correlation of ■ ABSTRACT the northern Indo-Burma Ranges, including the Mesozoic–Cenozoic southern Himalayan-Tibetan lithologic units across the eastern Himalayan syntaxis: Geosphere, v. 15, no. 3, p. 856– Gangdese batholith belt and its cover sequence of the Linzizong volcanic 881, https:// doi.org /10.1130 /GES02054.1. The Cenozoic India-Asia collision generated both the east-trending Hi- rocks, Xigaze forearc basin, Tethyan Himalayan Sequence, and Greater Hi- malayan orogen and the north-trending Eastern and Western Flanking Belts malayan Crystalline Complex of south-central Tibet and the central Himalaya.