作者: Yuyoung Lee , Moonsup Cho , Wonseok Cheong , Keewook Yi
DOI: 10.1111/TER.12115
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摘要: To unravel the petrogenesis of a massif-type anorthosite in terms crust-mantle geodynamics, we dated zircons separated from six samples Sancheong-Hadong (SH) complex, Korea, using sensitive high-resolution ion microprobe. The weighted mean 207Pb/206Pb age two anorthosites is 1862 ± 2 Ma, whereas ages hornblende gabbro and granitic gneiss are 1873 ± 4 Ma 1875 ± 5 Ma respectively. Zircon rims mafic granulite migmatitic yielded 1860 ± 5 Ma 1858 ± 4 Ma, respectively, implying that facies metamorphism anatexis associated with emplacement. Our results, together available Re–Os data, compatible ~1.9–1.86 Ga collisional orogeny prevalent North China Craton Korean Peninsula, suggest orogenesis was accompanied by mantle delamination beneath craton. It thus likely SH anorthositic rocks product late-orogenic magmatism during post-collisional extension-dominated phase orogeny.