A Middle Permian Ophiolitic Mélange Belt in the Solonker Suture Zone, Western Inner Mongolia, China: Implications for the Evolution of the Paleo-Asian Ocean
Dong Fu1 , Bo Huang1 , Timothy M. Kusky1,2 , Gangzhu Li3, Simon A. Wilde4 , Wenxiao Zhou5, and Yang Yu5
1Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan, China, 2State Key Laboratory of
Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, China, 3No.2 Gold Geological Team of
CAPF, Hohhot, China, 4The Institute for Geoscience Research, Department of Applied Geology, Curtin University, Perth,
Western Australia, Australia, 5Institute of Geological Survey, China University of Geosciences, Wuhan, China
The Solonker suture zone in the southeastern Central Asian Orogenic Belt is generally regarded as the location of the final closure of the Paleo-Asian Ocean, formed by complex and cryptic accretionary processes during late Paleozoic to early Mesozoic times. We recognize three tectonically juxtaposed lithotectonic units, including forearc basin sedimentary sequences, ophiolitic fragments, and ophiolitic mélange in the Solonker area, and here investigate the structural and kinematic features of the ophiolitic mélange in detail. The Solonker ophiolitic mélange has typical block-in-matrix fabrics with variably sized basalt, chert, sandstone, and ultramafic blocks embedded in siliceous-argillaceous and siltstone matrices. Both extensional and contractional structures are well developed within the mélange, characterized by pervasive foliation, pinch-and-swell, boudinage, and S-C fabrics. Kinematic analysis of the deformation tructures indicates top-to-the-N thrusting, correlated with the southward subduction of the southern margin of the Paleo-Asian Ocean. Zircon U-Pb ages of the matrices and a tonalite pluton intruded into the mélange constrain the formation age of the Solonker ophiolitic mélange to be middle Permian (ca. 268–260 Ma). Geochemical data from the ophiolitic rocks show subduction-related characteristics with enriched large ion lithophile elements and depleted Nb, implying formation in a forearc setting. Our study provides robust evidence for the closure time of the Paleo-Asian Ocean after the middle Permian. The late-stage evolution of the Paleo-Asian Ocean was characterized by subduction, forearc accretion with
subsequent obduction of the kilometer-scale upper plate, and soft collision, ultimately leading to the formation of the Solonker suture zone in the North China-Mongolia segment.