“…The similar ages, chemical, and isotopic signatures of enclaves and host granites have been interpreted in various ways. Some favor the cogenetic relation between the enclave and host granites (e.g., Pin et al, 1990;Shellnut et al, 2010) whereas some argue their derivation from common crustal sources (e.g., Güraslan and Altunkaynak, 2019;Lu et al, 2020); and some advocate mafic-felsic magma mixing, mingling, chemical modification, and isotopic re-equilibration at varying degrees responsible for their partial to nearly equivocal chemical and isotopic features (e.g., Holden et al, 1987;Eberz and Nicholls, 1990;Elburg, 1996;Kumar and Rino, 2006;Adam et al, 2019). The geochemical and isotopic features do not provide unambiguously a viable model of enclave origin.…”