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《Journal of Changchun Institute of Technology(Natural Sciences Edition)》 2014-04
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The geological and geochemical characteristics of Molybdenum Deposit and its ore-controlling rocks in Songshutai Luanchuan County Henan Province

LIU Qin-an;No.5 Institute of Geo-exploration of Henan;  
The Songshutai hidden Molybdenum-Tungsten deposit lies in Huangbeiling metallogenic belt of the famous Nannihu molybdenum ore field.The area shows a good prospecting potential according to the widely distribution of Minor intrusions and well-developed faults.Orebodies occur in the contact zone of marble and granite porphyry of Sanchuan formation,with molybdenum ore types of marble,skarn and granite porphyry.The deposit resource of MO and W can reach medium-scale with a high grade.The respectively average grades of Mo and associated W are of 0.12%and 0.08%.Huangbeiling Porphyritic granite related closely to the mineralization,is a kind of caic-alkaline rock with high grade of silicon and K.The rock shows some features as follows:the average contents of SiO2,Na2 O + K2 O are respectively of 73.83%and8.97%,σ=2.01-3.283.3;And LREE shows relative enrichment.The elements of Ce and Eu show negative anomaly with the respectively average value ofδEu andδCe of 0.40 and 0.56-0.78.The rock is much poorer in Sr and Ba but richer in the large ion lithophile elements.These features are similar to those of Nannihu and Shangfang granite.It can conclude that Songshutai molybdenum deposit can be classified as porphyry-skarn type,being the same type with Nannihu and Shangfang molybdenum deposit.The ore bodies may extend to the endless depth and with greater prospecting potential.
【Fund】: 国土资源部整装勘查项目(2011年第10号)
【CateGory Index】: P618.6
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