In-situ central Qiangtang metamorphic belt in western Tibet as a typical suture zone: Evidence of crust-mantle structural footprints from P-wave receiver function analyses

地质学 地体 结壳 纤维接头 俯冲 地震学 地幔(地质学) 接收器功能 变质岩 岩石学 地球化学 构造学 岩石圈 医学 解剖
作者
Xiao Guang Niu,Rizheng He,Hongwei Zheng,Wei Wu,Zhanbo Ji
出处
期刊:Tectonophysics [Elsevier]
卷期号:838: 229484-229484
标识
DOI:10.1016/j.tecto.2022.229484
摘要

Whether the central metamorphic belt of the Qiangtang terrane in the Qinghai-Tibet Plateau should be attributed to a suture zone, is still heavily debated, due to inadequate deep structure constraints. Using the data collected from 16 stations in the northern part of the Hi-Climb profile and 16 broadband seismic stations recently arranged in the northern part of Gaize County, this study developed a broadband seismic profile running through the in-situ Central Qiangtang Metamorphic Belt (CQMB) roughly along 84.5°E. Significantly characteristics of the crust and mantle structure beneath the profile were obtained through P-wave receiver function analyses: (i) The south Qiangtang terrane has a complex Moho structure at depth 56–82 km, while the north Qiangtang terrane has a nearly horizontal Moho at depth approximately 62 km. Moreover, the northward-inclining Moho is noticeably dislocated with a maximum offset of approximately 18 km under the CQMB. (ii) The crustal low-velocity zones on both sides of the CQMB are transversely discontinuous and are also distinct from each other. (iii) A northward-subducting interface occurs beneath the in-situ CQMB (34.0°N–34.5° N). Based on the geological outcrops and their petrological analysis, the structural characteristics beneath the CQMB are interpreted as the traces of the Longmucuo-Shuanghu suture zone, which was formed by the northward subduction-collision of the south Qiangtang terrane left after the closure of the Paleo-Tethys Ocean at the end of the Triassic. • Obvious difference in the crust-mantle structure along the Profile 84.5°E in the western Qiangtang through P-wave receiver function analyses. • The northward-inclining Moho structure under the in-situ CQMB is noticeably dislocated, with a maximum offset of approximately 18 km. • The in-situ CQMB is interpreted as the traces of the Longmucuo-Shuanghu suture zone.
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