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- W2357639916 abstract "The vanadium-titanium magnetite deposit lies in the Panxi area,a large-scale steel and iron production base in China.It occurs in layered mafic and ultramafic pyroxenolite and gabbro rock bodies,and is confined to the paleo-uplift zones of the Panxi rift.The ore-bearing rock bodies intruded along the Anninghe deep fault,the Xigeda-Yuanmou fault and the Panzhihua fault.The ore-bearing rock body is only restricted in the Hercynian basic-ultrabasic rock.The lithological combination trinity of basic-ultrabasic rock,Dengyingzu Formation.calcareous limestone and Emei basalt are crucial for the large-sized and ultra-large-sized deposits in this region.The first-order rhythm of the ore-bearing Panzhihua ore-bearing rock body consists of upper gabbro,middle dark layered gabbro,lower course-grained melagabbro interbedded with the olive pyroxenite and the olive ore bedseam.Mastering characteristics of the vanadium-titanium magnetite deposit accurately is an effective way for searching for this kind of deposits.Currently,many mine occurrences have been found in the Hongge deposit and its surrounding areas using the geophysics method,suggesting a new idea for further prospecting in this region." @default.
- W2357639916 created "2016-06-24" @default.
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- W2357639916 date "2012-01-01" @default.
- W2357639916 modified "2023-09-25" @default.
- W2357639916 title "Geological Features of the Vanadium-Titanium Magnetite Deposit in the Hongge Area and Its Geophysical Prospecting" @default.
- W2357639916 hasPublicationYear "2012" @default.
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