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Zircon–monazite geochronology and zircon Hf–O isotopes of Ediacaran–Cambrian paragneiss from the Mashan Complex, Jiamusi Block, NE China: implications for sedimentary–metamorphic–tectonic evolution
ABSTRACT Intense debate has surrounded the tectonic placement of microcontinents in the eastern Central Asian Orogenic Belt of NE China, with particular focus on the Jiamusi Block. The oldest basement rocks within the Jiamusi Block belong to the Mashan Complex, which preserves evidence of the Late Pan-African granulite-facies metamorphic overprinting. Characterizing this complex is therefore essential for elucidating the tectonic affinity of the Jiamusi Block.
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