Back-thrusting response of continental collision: Early Cretaceous NW-directed thrusting in the Changle-Nan'ao belt (Southeast China). (15th March 2015)

• Record Type: Journal Article
• Authors: Wei, Wei; Faure, Michel; Chen, Yan; Ji, Wenbin; Lin, Wei; Wang, Qingchen; Yan, Quanren; Hou, Quanlin
• Is Part Of: Journal of Asian earth sciences. Volume 100(2015)
• Page Start: 98
• Page End: 114
• Publication Date: 2015-03-15
• Subjects: South China Block -- East Asia Continental Margin -- Changle-Nan'ao belt -- Paleo-Pacific subduction -- Cretaceous geodynamics; Earth sciences -- Asia -- Periodicals; Sciences de la terre -- Asie -- Périodiques; Earth sciences; Asia; Periodicals; 555.05
• DOI: 10.1016/j.jseaes.2015.01.005
• Languages: English
• ISSNs: 1367-9120

Abstract

Highlights: This work conducts a systematic structural and AMS investigation on CNB. This work interprets the CNB as a NW-directed thrust belt between 130 and 105 Ma. The CNB was a back thrust belt due to the collision between West Philippines and SCB. Abstract: The SE coastal area of the South China Block (SCB) is generally interpreted as a Cretaceous active continental margin due to subduction of the Paleo-Pacific plate beneath the Eurasian plate. There, the NE–SW striking Changle-Nan'ao belt was previously considered as a major strike-slip fault zone with a large displacement accommodating the northward subduction of the Paleo-Pacific plate. Our new field and laboratory investigations document a NW-directed ductile thrust zone that placed gneiss upon Early Cretaceous foliated volcanic rocks. Structural analyses and Anisotropy of Magnetic Susceptibility results indicate that the ductile fabrics in both units are represented by a NE–SW striking foliation and a NW–SE stretching lineation with top-to-the-NW shear sense. This deformation occurred at ca. 130–105 Ma, before the deposition of undeformed (ca. 104 Ma) volcanic rocks, and the intrusion of ca. 90 Ma isotropic plutons. This continent-ward structure is tentatively interpreted as a back-thrust resulting of the collision of the West Philippines microcontinent with the SCB rather than an effect of a simple oceanic subduction.