Publication details for Professor Yaoling NiuSong, S.-G., Su, L., Li, X.-H., Niu, Yaoling & Zhang, L.F. (2012). Grenville-age orogenesis in the Qaidam-Qilian block: The link between South China and Tarim. Precambrian Research 220-221: 9-22.
- Publication type: Journal Article
- ISSN/ISBN: 0301-9268 (print)
- DOI: 10.1016/j.precamres.2012.07.007
- Keywords: North Qaidam UHPM belt, Grenville-age, Orogeny, Geochronology, South-West China United Continent.
- Further publication details on publisher web site
Author(s) from Durham
The link between the South China and Tarim blocks is a key issue in defining the tectonic framework of China. We report here that rocks from the Paleozoic (Caledonian) ultrahigh-pressure metamorphic (UHPM) belt also record a Grenville-age orogenic event in the Qaidam-Qilian block that lies between the South China and Tarim blocks. This event is marked by the presence of a juvenile Grenville-age continental margin that had been subducted to and exhumed from mantle depths of 100–200 km at the present-day location of northern Tibetan Plateau. The magmatic and metamorphic ages of 900–1000 Ma recorded in the gneisses provide direct evidence for this Grenville-age orogeny that extends northwestward from the Yangtze block, to the Qaidam-Qilian block, and to the Tarim block. This Grenville-age orogen along the North Qaidam UHPM belt (1) represents the link for the once South China–Qaidam-Qilian–Tarim continent, which, we name here as the “South-West China United Continent (SWCUC)”, had existed before the India–Asia collision, (2) sets a framework for precise reconstruction of Supercontinent Rodinia, and (3) presents an example of multi-epoch tectonic recycles, represented by the Neoproterozoic Grenvillian orogenesis and the Early Paleozoic Caledonian orogenesis.