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地质学报 1924
THERESULTOFAGEOLOGICALSURVEYOFTHFHONGSHANINTRUSION,NORTHHONANAbstract: Theresultssofarobtainedmaybesummarizedasfollows.TheHongshanintrusionisadome-shapedandisolatedbodyanddeep-seatednorigin.Theiatrusiontookplaceinthepost-CarboniferoustimeTheirondepositwasprobablyformedthroughmetasomatiereplacementoftheOrdovieianlimestoneandthereforeonlyextendsdownwardforaninsignifieuntdepth.Asarogoureoformodernindustry,itisabsohtelyvaluess.Thevariationinthecompositionofthedioriteisprobablydonnotsomuchtomagmaticdifferentiationbutrathertotheassimilationfotheoverlyingrocks.
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