Zircon and monazite U-Pb ages of the Mashan Complex of the Jiamusi Block of NE China: a link to Gondwana?

ABSTRACT

The tectonic affinities of the microcontinents in the eastern Central Asian Orogenic Belt of NE China, particularly the Jiamusi Block, have been hotly debated in the last decade. The Mashan Complex, which is the oldest exposed basement of the Jiamusi Block and consists of khondalitic rocks (felsic granulite, marble, and graphite schist) and orthogneisses, is the key geological unit to look into the tectonic affinity of the Jiamusi Block. In this study, we carried out LA-ICP-MS U-Pb dating on zircon and monazite minerals from the granitic gneisses in the Mashan Complex, to constrain the affinity of the Jiamusi Block. Magmatic zircons from two granitic gneisses yielded weighted mean ²⁰⁶Pb/²³⁸U ages of 517 ± 7 Ma and 527 ± 4 Ma, respectively, which are interpreted as the protolith ages. These age data verify a late Pan-African magmatic event in the Jiamusi Block. Metamorphic zircons from one granitic gneiss gave a weighted mean ²⁰⁶Pb/²³⁸U age of 510 ± 3 Ma, which constrained the metamorphic time of the Mashan Complex. This metamorphic age is further supported by monazite dating results – the monazites from three granitic gneiss samples yielded weighted mean ²⁰⁶Pb/²³⁸U ages of 489 ± 3 Ma, 498 ± 3 Ma, and 500 ± 3 Ma, respectively, which represented the metamorphic recrystallization ages of these monazites. These data consistently indicate a regional metamorphic event immediately after the late Pan-African magmatism in the Jiamusi Block. Our new data, combined with previously published late Pan-African geochronological data from the Jiamusi Block, support that the Jiamusi Block has an affinity to the Gondwana.

KEYWORDS:

• Monazite
• Zircon
• ;late Pan-African
• Mashan Complex
• Jiamusi Block
• Gondwana

Acknowledgments

We would like to thank Chao Yu and Xia Teng from the Institute of Geology, Chinese Academy of Geological Sciences for zircon U-Pb isotopic analyses and TIMA mineral maps. The manuscript benefited from constructive comments from Editor Robert J. Stern and two anonymous reviewers. This work was supported by the National Natural Science Foundation of China (grant number 41902240 and 41730210) and the National Key Research and Development Project of China (grant number 2017YFC0601301).

Highlight

1. Zircon U-Pb data show that the granitic gneisses were formed during 527-517 Ma and metamorphosed during 510 Ma.

2. Monazite U-Pb analyses also show that the metamorphism of the Mashan Complex occurred during 510-489 Ma.

3. The Jiamusi Block has an affinity to the Gondwanaland.

Supplementary material

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Disclosure Statement

No potential conflict of interest was reported by the author(s).

Additional information

Funding

This work was supported by the National Natural Science Foundation of China [41730210,41902240]; National Key Research and Development Project of China [2017YFC0601301].