Publication details for Professor Yaoling NiuDeng, J.F., Su, S.G., Niu, Yaoling, Liu, C., Zhao, G.C., Zhou, S. & Wu, Z.X. (2007). A possible model for the lithospheric thinning of North China Craton: Evidence from the Yanshanian (Jura-Cretaceous) magmatism and tectonism. Lithos 96(1-2): 22-35.
- Publication type: Journal Article
- ISSN/ISBN: 0024-4937
- DOI: 10.1016/j.lithos.2006.09.009
- Keywords: North China Craton; Yanshanian orogenic belt; Magmatism and tectonic deformation; Delamination and lithospheric thinning
- Further publication details on publisher web site
Author(s) from Durham
It is well known that the North China Craton was largely formed in the Archean, and was reactivated and transformed during the
13 Jura-Cretaceous (Yanshanian) time into an orogenic belt, which is believed to be related to the lithospheric thinning. Recent debate
14 is centered on the mechanisms and processes of the lithospheric thinning. There are two prevailing models for the lithosphere
15 thinning: (1) thermal erosion or/and chemical metasomatism allowed the lower part of the lithospheric mantle to be transformed
16 into asthenosphere, (2) delamination of the lithospheric mantle, and perhaps also the lowermost crust.
17 In this paper, we attempt to explain how the buoyant cratonic lithosphere may be transformed into a denser one, allowing
18 delamination to take place on the basis of field observation, tectonic analysis and petrologic data on igneous rocks formed during
19 the Yanshanian. We recognize four episodes of contractional deformation that resulted in significant crustal shortening and vertical
20 thickening. The counter-clockwise Pressure–Temperature–time path of the tectonomagmatic events suggests that the underplating
21 basaltic magma may have heated and weakened the existing cold and strong crust. This crustal change in rheology may have
22 facilitated the contractional deformation and crustal thickening. Petrologic data of the contemporary igneous rocks and the lower crustal xenoliths suggest that the crust had reached ∼50–65 km in thickness. It suggests that input of large amount of asthenosphere-derived mafic magmas is required to cause crustal melting. Thus, a large amount of eclogite may be formed at the lowermost crust following the transient thickening events. The dense eclogite may trigger the lithosphere delamination.