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Regeneration iron metallization at the Xishimen field (North-East China)

https://doi.org/10.33623/0579-9406-2020-1-28-36

Abstract

The Xishimen skarn iron deposit was confined to a deep fault and locates at the contact of small intrusions of monzodiorites with Pz–Mz carbonate rocks. It is represented by several banding and lenticular forms. The formation of ores is associated with the recycling processes of ore matter.
The process proceeded in several stages. Primary sedimentary and volcanogenic-sedimentary ores were formed in Ar–Prt1 time. Then followed several stages of tectonic-magmatic activation, among which the most significant was Anshan stage (Jurassic-Cretaceous). Monzodiorite magma in the process of recycling was enriched by siderophilic elements of early Precambrian and formed a series of Fe deposits in the zone of deep faults.

About the Author

Shi Xudong
Lomonosov Moscow State University
Russian Federation
119991, GSP-1, Leninskiye Gory, 1


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For citations:


Xudong Sh. Regeneration iron metallization at the Xishimen field (North-East China). Moscow University Bulletin. Series 4. Geology. 2020;(1):28-36. (In Russ.) https://doi.org/10.33623/0579-9406-2020-1-28-36

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