A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2022; you can also visit the original URL.
The file type is
U–Pb Zircon Ages and Geochemistry of the Wuguan Complex and Liuling Group: Implications for The Late Paleozoic Tectonic Evolution of the Qinling Orogenic Belt, Central China
The tectonic evolution of the Qinling orogen is key to understanding the process of convergence between the North China Block (NCB) and the South China Block (SCB). The Wuguan Complex and Liuling Group, situated along the southern margin of the Shangnan–Danfeng suture zone (SDSZ) between the North Qinling Terrane (NQT) and the South Qinling Terrane (SQT), are important indicators of the late Paleozoic tectonic evolution of the Qinling orogen. In this paper, the detrital zircon U–Pbdoi:10.3390/min12081026 fatcat:rogfe3rkrffwbfjozttf4fzitm