Data for: From subduction initiation to arc–polarity reversal: Evidence from the petrology, geochemistry and geochronology of Neoarchean ophiolitic mélange in the Zunhua Structural Belt, North China Craton

Published: 9 October 2020| Version 7 | DOI: 10.17632/wkcr4wb4c4.7
Contributors:
Tim Kusky,
Wenbin Ning,
Bo Huang,
Ali Polat,
Hongtao Peng,
Junpeng Wang,
Lu Wang,
Peng Feng,
Hao Deng

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Table 1. LA–ICP–MS U–Pb data for biotite–plagioclase–quartz gneiss, metadiabase and mafic dike in the Zunhua structural belt of the Eastern Hebei Complex, North China Craton. Table 2. Geochemical composition of the ultramafic–mafic rocks in the Zunhua structural belt of the Eastern Hebei Complex, North China Craton. Table 3. Sm–Nd composition of the pyroxenite in the Zunhua structural belt of the Eastern Hebei Complex, North China Craton. Table 4. Metamorphic P–T conditions during late Neoarchean in the Eastern Hebei Province, North China Craton. Supplementary Table 1. Mineral composition of olivine, chromite, orthopyroxene in the ultramafic rocks from the Zunhua structural belt of the Eastern Hebei Complex, North China Craton.

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