Tectonic Boundary and Ceasing Time of Amalgamation between the North China Craton and the North Qinling BeltJingbo Liu(Ningbo University), Wen Su(Chinese Academy of Sciences), Nengsong ChenJournal of Earth ScienceJuly 13, 201810.1007/s12583-018-0847-8Cited by 10SaveCiteExport RISWatch citationsRelated PapersMineral Inclusions in Zircon from Gneisses in the Ultrahigh‐Pressure Zone of the Dabie Mountains, China|The Journal of Geology|2001|169A transitional eclogite- to high pressure granulite-facies overprint on coesite–eclogite at Taohang in the Sulu ultrahigh-pressure terrane, Eastern China|Lithos|2000|90Fluid–rock interaction and element mobilization in UHP metabasalt: Constraints from an omphacite–epidote vein and host eclogites in the Dabie orogen|Lithos|2011|90Exhumation P–T path of UHP eclogites in the Hong'an area, western Dabie Mountains, China|Lithos|2006|54Formation of multiple high-pressure veins in ultrahigh-pressure eclogite (Hualiangting, Dabie terrane, China): Fluid source, element transfer, and closed-system metamorphic veining|Chemical Geology|2015|41