Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/15654
Authors: Zhang, Bo* 
Chen, Siyu Y* 
Wang, Y* 
Reiners, P. W.* 
Cai, F. L.* 
Speranza, Fabio* 
Zhang, J. J.* 
Zhong, D.L.* 
Liu, K* 
Title: Crustal deformation and exhumation within the India-Eurasia oblique convergence zone: New insights from the Ailao Shan-Red River shear zone
Journal: GSA Bulletin 
Series/Report no.: 5-6/134 (2022)
Publisher: GSA
Issue Date: 2022
DOI: 10.1130/B35975.1
Abstract: During the collision of India and Eurasia, regional-scale strike-slip shear zones played a key role in accommodating lateral extru- sion of blocks, block rotation, and vertical ex- humation of metamorphic rocks as presented by deformation on the Ailao Shan-Red River shear zone (ARSZ) in the Eastern Himala- yan Syntaxis region and western Yunnan, China. We report structural, mica Ar/Ar, apatite fission-track (AFT), and apatite (U- Th)/He (AHe) data from the Diancangshan massif in the middle segment of the ARSZ. These structural data reveal that the massif forms a region-scale antiform, bordered by two branches of the ARSZ along its eastern and western margins. Structural evidence for partial melting in the horizontal mylonites in the gneiss core document that the gneiss experienced a horizontal shear deformation in the middle crust. Muscovite Ar/Ar ages of 36–29 Ma from the core represent cooling ages. Muscovite Ar/Ar ages of 25 and 17 Ma from greenschist-facies mylonites along the western and southern shear zones, respec- tively, are interpreted as recording deforma- tion in the ARSZ. The AFT ages, ranging from 15 to 5 Ma, represent a quiescent gap with a slow cooling/exhumation in the mas- sif. AHe results suggest that a rapid cooling and final exhumation episode of the massif could have started before 3.2 Ma, or likely ca. 5 Ma, and continue to the present. The high-temperature horizontal shearing layers of the core were first formed across the In- dochina Block, locally antiformed along the tectonic boundaries, and then cooled through the mica Ar-Ar closure temperature during Eocene or early Oligocene, subsequently re- worked and further exhumed by sinistral strike-slip movement along the ARSZ during the early Oligocene (ca. 29 Ma), lasting until ca. 17 Ma, then final exhumation of the mas- sif occurred by dextral normal faulting on the Weixi-Qiaohou and Red River faults along the limbs of the ARSZ since ca. 5 Ma. The formation of the antiform could indicate local crustal thickening in an early transpressional setting corresponding to India-Asia conver- gence. Large-scale sinistral ductile shear along the ARSZ in the shallow crust accom- modated lateral extrusion of the Indochina Block, and further contributed to the vertical exhumation of the metamorphic massif from the late Oligocene to the middle Miocene. Furthermore, the change of kinematic re- versal and associated cooling episodes along the ARSZ since the middle Miocene or early Pliocene imply a tectonic transfer from strain localization along the major tectonic bound- aries to continuous deformation correspond- ing to plateau growth and expansion.
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