Zircon Hf-O isotopic constraints on the origin of Late Mesozoic felsic volcanic rocks from the Great Xing'an Range, NE China

• Published in: Lithos Vol. 308-309; pp. 412 - 427
• Main Authors: Gong, Mingyue, Tian, Wei, Fu, Bin, Wang, Shuangyue, Dong, Jinlong
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-05-2018
• Subjects: 18O-depletion; Felsic volcanic rocks; Late Mesozoic magmatism; Northeastern China; Phanerozoic continent growth; Rift; Rift; Phanerozoic continent growth; Felsic volcanic rocks; 18O-depletion; Northeastern China; Late Mesozoic magmatism
• ISSN: 0024-4937; 1872-6143
• DOI: 10.1016/j.lithos.2018.03.023

The voluminous Late Mesozoic magmatism was related to extensive re-melting of juvenile materials that were added to the Central East Asia continent in Phanerozoic time. The most favoured magma generation mechanism of Late Mesozoic magmas is partial melting of underplated lower crust that had radiogenic Hf-Nd isotopic characteristics, but this mechanism faces difficulties when interpreting other isotopic data. The tectonic environment controlling the generation of the Late Mesozoic felsic magmas is also in dispute. In this study, we obtained new U-Pb ages, and geochemical and isotopic data of representative Jurassic (154.4 ± 1.5 Ma) and Cretaceous (140.2 ± 1.5 Ma) felsic volcanic samples. The Jurassic sample has inherited zircon cores of Permian age, with depleted mantle-like εHf(t) of +7.4 − +8.5, which is in contrast with those of the magmatic zircons (εHf(t) = +2.4 ± 0.7). Whereas the inherited cores and the magmatic zircons have identical mantle-like δ18O composition ranges (4.25–5.29‰ and 4.69–5.54‰, respectively). These Hf-O isotopic characteristics suggest a mixed source of enriched mantle materials rather than ancient crustal components and a depleted mantle source represented by the inherited Permian zircon core. This mechanism is manifested by the eruption of Jurassic alkaline basalts originated from an enriched mantle source. The Cretaceous sample has high εHf(t) of +7.0 − +10.5, suggesting re-melting of a mafic magma derived from a depleted mantle-source. However, the sub-mantle zircon δ18O values (3.70–4.58‰) suggest the depleted mantle-derived mafic source rocks had experienced high temperature hydrothermal alteration at upper crustal level. Therefore, the Cretaceous felsic magma, if not all, could be generated by re-melting of down-dropped supracrustal volcanic rocks that experienced high temperature oxygen isotope alteration. The two processes, enriched mantle-contribution and supracrustal juvenile material re-melting, are new generation mechanisms of the Late Mesozoic magmas from Central East Asia. Rift settings may have controlled these processes throughout crustal and mantle levels.
•The Jurassic felsic volcanic rocks had a mixing source derived from EM + DM.•The Cretaceous ones had a juvenile, high-T hydrothermal altered supracrustal source.•Hf-O isotopes do not support the "underplated lower crust re-melting" model.