Delineation of podiform-type chromite mineralization using geochemical mineralization prospectivity index and staged factor analysis in Balvard area (SE Iran)

被引:42
作者
Afzal, P. [1 ]
Yousefi, M. [2 ]
Mirzaei, M. [1 ]
Ghadiri-Sufi, E. [3 ]
Ghasemzadeh, S. [4 ]
Saein, L. Daneshvar [5 ]
机构
[1] Islamic Azad Univ, Dept Petr & Min Engn, South Tehran Branch, Tehran, Iran
[2] Malayer Univ, Fac Engn, Malayer, Iran
[3] Kashan Univ, Dept Min Engn, Kashan, Iran
[4] Amirkabir Univ Technol, Dept Min & Met Engn, Tehran Polytech, Tehran, Iran
[5] Payame Noor Univ, Dept Geol, Tehran, Iran
来源
JOURNAL OF MINING AND ENVIRONMENT | 2019年 / 10卷 / 03期
关键词
Geochemical Mineralization Prospectivity Index; Staged Factor Analysis; Continuous Weighting; Fuzzy Logic; Podiform-Type Chromite; STREAM SEDIMENT DATA; TECTONIC EVOLUTION; OPHIOLITE COMPLEXES; FRACTAL MODEL; ANOMALIES; DEPOSITS; OVERLAY; SHEET; BASIN; ORES;
D O I
10.22044/jme.2019.8107.1678
中图分类号
TD [矿业工程];
学科分类号
0819 ;
摘要
The aim of this work was to delineate the prospects of podiform-type chromite by staged factor analysis and geochemical mineralization prospectivity index in Balvard area, SE Iran. The stream sediment data and fault density were used as the exploration features for prospectivity modeling in the studied area. In this regard, two continuous fuzzified evidence layers were generated and integrated using fuzzy operator. Then fractal modeling was used for defuzzification of the prospectivity model obtained. Furthermore, the prediction-area plot was used for evaluation of the predictive ability of the generated target areas. The results obtained showed that using the prospectivity model, 82% of mineral occurrences was predicted in 18% of the studied area. In addition, the target areas were correlated with the geological particulars including ultrabasic and serpentinization rocks, the host rocks of the podiform-type chromite deposit type.
引用
收藏
页码:705 / 715
页数:11
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