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. 2021 Jul 21;11:14882. doi: 10.1038/s41598-021-94492-y

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© The Author(s) 2021

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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(A) Simplified tectonic framework of the southern margin of the Lhasa block showing the location of the study area. (B) Regional geological map showing the study area, modified from the China Geological Survey (www.cgs.gov.cn) based on our field observations. The maps were generated by Zongyao Yang, using CorelDRAW X8 version 18.0.0.448. Yellow diamonds represent literature data of Paleocene S-type magma^9–12. Blue dashed circles represent the approximate extent of the s-type granitic rocks. LMF Luobadui–Milashan Fault.