The heart of China revisited, I. Proterozoic tectonics of the Qin mountains in the core of supercontinent Rodinia

• Published in: Tectonics
• Main Authors: Bader, Thomas, Ratschbacher, Lothar, Franz, Leander, Yang, Zhao, Hofmann, Mandy, Linnemann, Ulf, Yuan, Honglin
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: American Geophysical Union 2013
• Subjects: East Antarctica; Antarc*; Antarctica
• Online Access: https://edoc.unibas.ch/81560/; https://doi.org/10.1002/tect.20024

The Qinling-Dabie orogenic collage, central China, constitutes the geographic, geologic, and cultural heart of China; it plays a key role in understanding the amalgamation and breakup of the Rodinia supercontinent and the subduction and exhumation of continental crust under ultrahigh-pressure conditions. Herein, we investigate the Proterozoic evolution of the Qinling-Dabie orogenic collage and surrounding segments of the bounding South China craton (SCC) and North China craton (NCC), employing published and new U/Th-Pb geochronology. The Kongling, Hong`an-Dabie, and Douling-Foping complexes constitute the nucleus of the Yangtze block, recording a common similar to 2.0Ga orogenic event that integrated the Yangtze block into the supercontinent Columbia. The similar to 1.10-0.95Ga Miaowan ophiolite-Shennongjia arc association of the Huangling dome-Shennongjia massif seems to have split and reassembled that nucleus. It formed earlier than or contemporaneously with the Sibao orogeny along the southeastern margin of the Yangtze block. The similar to 0.95-0.80Ga Mian-Lue complex comprises an oceanic accretionary wedge that formed outboard of an associated fore-arc-arc system represented by the Bikou-Hannan-Micangshan massifs along the north(western) margin of the Yangtze block. The Qinling complex, currently sandwiched between the SCC and NCC, lacks pre-Mesoproterozoic cratonal basement, and its igneous rocks intruded a similar to 1.7-1.0Ga old clastic wedge that incorporates meta-basites; it might have been part of the extended passive margin of East Antarctica and/or Australia. Neoproterozoic Qinling-complex magmatism spanned similar to 260 Myr and evolved from partial melting of the thick clastic sequence over an arc to a rift setting; most Qinling-complex paragneisses are erosional products of these igneous rocks. The similar to 1.0-0.85Ga Qinling-complex magmatism formed independently from that along the north(west)ern Yangtze-block margin, but its similar to 0.8-0.7Ga magmatism, peaking at similar to 750Ma, is ...