Warm Subduction-Driven Formation of ~2.7 Ga TTG Gneiss in the Zhongtiao Mountains, Southern North China Craton: Constraints from Phase Equilibrium Modeling

Next article No AccessWarm Subduction-Driven Formation of ~2.7 Ga TTG Gneiss in the Zhongtiao Mountains, Southern North China Craton: Constraints from Phase Equilibrium ModelingDongchen Jiao and Junfeng QuDongchen Jiao and Junfeng QuPDFPDF PLUS Add to favoritesDownload CitationTrack CitationsPermissionsReprints Share onFacebookTwitterLinkedInRedditEmailPrint SectionsMoreDetailsFiguresReferencesCited by The Journal of Geology Just Accepted Article DOIhttps://doi.org/10.1086/727973 Views: 4Total views on this site HistoryAccepted September 18, 2023 © 2023 The University of Chicago. All Rights reserved.PDF download Crossref reports no articles citing this article.