Journal
GONDWANA RESEARCH
Volume 26, Issue 2, Pages 475-491Publisher
ELSEVIER
DOI: 10.1016/j.gr.2013.07.023
Keywords
Triassic bimodal volcanic rocks; Slab break-off; Collisional orogenesis; Jiangda-Deqen-Weixi continental margin arc (DWCA); Paleo-Tethys
Categories
Funding
- National Key Project for Basic Research of China [2009CB421003]
- Chinese National Natural Science Foundation [41073033, 41373030]
- Program of the China Geological Survey [1212011121262, 1212011085119]
Ask authors/readers for more resources
Triassic volcanic rocks in the Jiangda-Deqen-Weixi continental margin arc (DWCA) in the Sanjiang area of SW China formed as a result of the closure of the Paleo-Tethys and associated continental collision, and are therefore important for reconstructing the evolution of the Paleo-Tethys. Representative samples of rhyolite and basalt from the Jijiading-Luchun-Yezhi area yield weighted mean Pb-206/U-238 ages of 245-249 Ma and 245 Ma, respectively, and exhibit the features of bimodal volcanic rocks. The mafic rocks are enriched in large ion lithophile elements (e.g., Rb, Ba, U), are depleted in high field strength elements (e.g., Nb,Ta, Ti), and have low epsilon(Nd)(t) values (-3.55 to -3.69) and high initial Sr-87/Sr-86 values (0.70788-0.70804). The mafic rocks were formed by partial melting of an enriched lithospheric mantle source that had been metasomatized by fluids derived from subducted sediments. The felsic rocks are characterized by high K2O (K2O/Na2O = 2.16-71.33) and A/CNK (>1.1), and low Mg# (20-45) and epsilon(Nd)(t) values (-9.61 to -10.66), with zircon epsilon(Hf)(t) values of -8.1 to -16.6. Their old Nd model ages are similar to those of ancient Yangtze basement, indicating that they formed by partial melting of this ancient crust as a result of underplating by basaltic magma. We suggest that the bimodal volcanic rocks in the DWCA formed in an extensional setting as a result of slab break-off during a margin of arc-continent collision. The present results, combined with previous data, reveal three stages of collision in the Paleo-Tethys: early collision convergence (similar to 255-250 Ma), syn-collision extension (249-237 Ma), and late collision orogenesis (236-212 Ma). (C) 2013 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available