Geochronology, geochemistry and Sr-Nd-Pb-Hf isotopes of the Paleoproterozoic mafic dykes from the Wulashan area, North China Craton: Petrogenesis and geodynamic implications
The mafic dykes from the Wulashan area emplaced at ca. 1770 Ma.
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The parental magmas experienced fractional crystallization and accumulation.
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The mafic dykes originated from the subcontinental lithospheric mantle.
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Post-orogenic setting may be the genetic model for these mafic dykes.
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