Inherited source affinity of Li and Hf isotopes for porphyry copper deposits from subduction and collisional settings

Lu, Yigan; Xiao, Yilin; Nadeau, Olivier; Yang, Xiaoyong; Wang, Yangyang; Hou, Zhiguo; Sun, He; Li, Dongyong; Gu, Hai‐Ou; Deng, Jianghong; Tong, Fengtai; Tan, Dong-Bo; Qi, Huasheng; Bute, Saleh Ibrahim

doi:10.1016/j.oregeorev.2021.104328

Cited by 5 publications

(1 citation statement)

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“…The associated Tethyan metallogenic belt is one of the most endowed metallogenic belts in China, which was formed in a continental collision setting [3][4][5]. Giant or large porphyry copper deposit (PCD) may not be solely produced by oceanic subduction [6][7][8], but might also be emplaced in the continental collision during the post-collisional extension of the intra-continental setting, which also favors large or even giant porphyry deposit [9][10][11][12]. Generally, in an arc setting, the porphyry Cu deposits are associated with a calc-alkaline suite whereas in the continental settings are associated with high-K to shoshonitic suites [13,14].…”

Section: Introductionmentioning

confidence: 99%

Origin and Geodynamic Mechanism of the Tibetan Demingding Porphyry Mo (Cu) Deposit from Oceanic Subduction to Continental Collision

Dong

Zhou

et al. 2022

Minerals

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Demingding is a promising porphyry Mo-dominated deposit recently discovered in the eastern Gangdese metallogenic belt in Tibet, China. We present zircon U-Pb-Lu-Hf isotopic studies, as well as geochemical data of the late monzogranites and the prior rhyolites from the Demingding porphyry deposit to uncover their origin and geodynamic mechanism. Zircon U–Pb dating yielded precise crystallization ages of 17.3 ± 0.6 Ma (MSWD = 2.5) and 186.5 ± 3.0 Ma (MSWD = 2.0) for monzogranite and rhyolite, respectively. The monzogranite is characterized by high-K calc-alkaline, adakitic affinities, and positive zircon εHf(t) values (+0.9∼+5.6, avg.+3.1) with TDM2 (0.73–1.04 Ga), while the rhyolite has εHf(t) values of (+2.1∼+7.3, avg.+5.2) and TDM2 of (0.76–1.09 Ga) similar to the monzogranite. Our results suggest that the Demingding porphyry Mo (Cu) deposit is related to magma generated from the Neo-Tethyan oceanic subduction. The subsequent monzogranite porphyry was likely formed by the remelting of previously subduction-modified arc lithosphere, triggered by continental collision crustal thickening in Miocene. The lower positive εHf(t) values of monzogranites suggest minor inputs from the Mo-rich ancient crust, suggesting that Mo favors the silicate melt. Such magmatic events and special metallogenesis typify intracontinental processes and porphyry copper deposits, which are normally confined to oceanic subduction and Cu-dominated style, thereby making the continental setting and Mo-dominated style of Demingding exceptional and possibly unique.

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