Brittle failures and vein formation in the evolution of the South Qiangtang accretionary complex in the Tibetan Plateau

Abstract

The genesis of the subduction mélange in the central Qiangtang terrane has been a long hot debate. However, little research has been conducted on the brittle failure within the accretionary wedge, which is very important to unveil the structural evolution of the mélange. In this study, based on the recognition of multiple deformational phases, we analyse the characteristics and formation history of the vein system in the Gangma Co mélange. Six groups of quartz veins are recognized. Foliation‐parallel extension veins (G1 veins), shear veins (G2 veins) and foliation‐perpendicular extension veins (G4 veins) are supposed to have formed during the subduction of oceanic crust, recording the repeated low‐angle thrust‐sense frictional sliding, tensile fracturing and stress changes generated by subduction‐related earthquakes. Subsequent vertical extension veins (G5 veins) are suggested to be related to the exhumation of the underplated mélange, while the horizontal extension veins (G6 veins) in the last phase represent the final horizontal thrusting. The temperature conditions for shear vein formation were examined by fluid inclusion analysis, ranging from 120 to 200°C, coinciding with the temperature conditions of the slow earthquake region where episodic tremors and slow slip occur. This contribution supports that the Gangma Co mélange represents an in situ subduction zone and that its internal vein system is a response to the tectonic evolution of the Longmu Co‐Shuanghu Tethys Ocean.

Advances in metallogeny and tectonics of the Eastern Tethyan Realm: Introduction

“…The tectonic veins of the accretionary complex can provide significant implications for tectonic and fluid evolution processes. Li, Li, et al (2023) recognized six groups of tectonic veins from the Gangma Co mélange in the South Qiangtang accretionary complex. The foliation‐parallel G1 extensional veins, G2 shear veins and foliation‐perpendicular G4 extensional veins were considered to have formed during the oceanic subduction process.…”