Conclusions
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1.
The eclogite dikes in low-greenschist facies epi-metamorphic volcaniclastic rocks in the Dabie Mountains areas show magma origin rather than tectonic melange or metamorphic origin.
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2.
Coesite and quartz pseudomorphs in the eclogite show that they were formed at the pressure of over 2.8 GPa and belong to ultrahigh pressure type. Therefore, there were high-pressure eclogite magma at deep crust depth.
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3.
From the country rock age of the low-grade metamorphic volcaniclastic rocks, we infer that the eclogite dikes were formed after the Sinian.
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Gao, T., Tang, J., Zhou, C. et al. The discovery of eclogite dikes in low-greenschist facies volcaniclastic rocks of the Dabie Mountains. Chin.Sci.Bull. 42, 1726–1729 (1997). https://doi.org/10.1007/BF02882676
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DOI: https://doi.org/10.1007/BF02882676