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Geochronological and geochemical constraints on the petrogenesis and tectonic significance of Paleozoic dolerite dykes in the southern margin of Alxa Block, North China Craton
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The dolerite dykes in the Jinchuan area, southwestern North China Craton were emplaced at ∼424 Ma.

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The parental magma of the Jinchuan dolerite dykes underwent strong crustal contamination.

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Partial melting in the source mantle was induced by asthenosphere upwelling associated with slab break-off.

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The southwestern margin of North China Craton was an active plate margin in Early Paleozoic.

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