Abstract
A test of deep seismic reflection profiling across the central uplift or metamorphic belt of the Qiangtang (羌塘) terrane, Tibetan plateau, provides a first image of the crustal structure. Complex reflection patterns in the upper crust are interpreted as a series of folds and thrusts, and bivergent reflections in the lower crust may represent a convergence between the Indian and the Eurasian plates.
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This study was financially supported by the National Natural Science Foundation of China (Nos. 40830316, 40874045 and 40704016), the Ministry of Science and Technology of China (Nos. SinoProbe-02, 2006DFA21340), the Ministry of Land and Resources of China (Nos. 2004-06, 200811021), and the Open Fund of Key Laboratory of Geo-detection of China University of Geosciences (Beijing) (No. GDL0603).
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Lu, Z., Gao, R., Li, Q. et al. Test of deep seismic reflection profiling across central uplift of Qiangtang terrane in Tibetan plateau. J. Earth Sci. 20, 438–447 (2009). https://doi.org/10.1007/s12583-009-0036-x
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DOI: https://doi.org/10.1007/s12583-009-0036-x