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- W2375749195 abstract "Recent exploration discovered marble near Jianshan ore block of Daye iron deposit with lots of melt inclusions or flow-melt inclusions.The heating experiments showed that melt inclusions and flow-melt inclusions have approximate homogenization temperatures of 880～1 055 and 645～740 ℃,indicating that the marble studied above is not ordinary marble formed by the contact metamorphism,but a new carbonatite type-crust-derived carbonatite of magmatic type.This reported marble,in which melt inclusions are discovered,represents some geological evidences with magma nature and even passive intrusion including the flow structures and vesicular structures at front edge of marble intrusion,which are similar to those of subvolcanic rocks and the marble veins passively intruding into diorite along cracks such as faults and joints formed at contact belt,and fewer diorite breccia packaged by marble.Therefore,those evidences through field work support the result of marble being crust at front edge of marble intrusion,derived carbonatite." @default.
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- W2375749195 date "2006-01-01" @default.
- W2375749195 modified "2023-09-26" @default.
- W2375749195 title "Magmatogenic marble discovered in contact zone of Daye iron deposit" @default.
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