Title: Geochemical Data Analysis of Irankouh (Isfahan) Pb- Zn Mine, Using Exploratory Data Analysis (EDA) and Fractal Methods

Title: ØªØ¬Ø²Û Ù Ù ØªØ­Ù Û Ù Ø¯Ø§Ø¯Ù â Ù Ø§Û Ú Ø¦Ù Ø´Û Ù Û Ø§Ú©ØªØ´Ø§Ù Û Ø¯Ø± ٠حد٠د٠٠عد٠سرب Ù Ø±Ù Û Ø§Û Ø±Ø§Ù Ú©Ù Ù Ø§ØµÙ Ù Ø§Ù Ø¨Ø§ است٠اد٠از ر٠شâ Ù Ø§Û ØªØ­Ù Û Ù Ø§Ú©ØªØ´Ø§Ù Û Ø¯Ø§Ø¯Ù â ٠ا (EDA) ٠٠٠دس٠٠رکتاÙ
Author(s): Seyed Hossein Mojtahedzadeh,Mahdi Bemani,Saeede Malekzade,Ø³Û Ø¯ Ø­Ø³Û Ù Ù Ø¬ØªÙ Ø¯Ø²Ø§Ø¯Ù ,Ù Ù Ø¯Û Ø¨Ù Ø§Ù Û ,Ø³Ø¹Û Ø¯Ù Ù Ù Ú© زادÙ

منبع: روش های تحلیلی و عددی در مهندسی معدن : Volume 7, Issue 13, 2017 , Pages 71-90
نمایه شده در: Iranian Journals Crossref

شناسه دیجیتال: DOI:10.29252/anm.7.13.71
شناسه اختصاصی:
IRDOI
269-275-613-317
[برای لینک دادن به این صفحه]
لینک دانلود: [دانلود مستقیم]

Summary Anomaly and lead-zinc index recognition of an area between Tappeh-Sorkh and Gushfil, in Irankouh Pb- Zn mine, near Isfahan, was investigated.  Interpretation for 12 elements, using 804 soil samples, was conducted. After early activities for censored data correction and transforming data for preparing normal distribution, anomalies recognition and separation were done using classical statistics, fractal and EDA (Exploratory Data Analysis) methods. Plotted anomalies maps prepared by three methods, show good conformity. Therefore, further studies in the regions showed overlapping resulted anomalies by three methods. Also detailed exploration by using geophysical IP methods was proposed.   Introduction Irankouh mine is located in Irankouh Mountains, 25 km southwest of the Isfahan city. Four mining area, including Tappeh-Sorkh, Gushfil, Khane â Gorgi are distinguished and their ore reserve has been determined separately. The aim of this research was anomaly and lead-zinc index recognition in the area between Tappeh-Sorkh and Gushfil.  In this research 804 soil samples were taken and analyzed for 35 elements, but for interpretation only 12 elements were used. Anomalies recognition and separation were conducted using classical statistics, fractal and EDA (Exploratory Data Analysis) methods.   Methodology and Approaches In the first step censored values were corrected, then the normality test on corrected datasets accomplished and showed that Ca, Mg and S have normal distribution. Other elements, which did not show normal distribution, were normalized by Log â normal and 3-parameters log distribution methods. Based on the parameters obtained from classical statistics and standard formula the anomaly and the background values were separated, using area- concentration model of fractal method. Also separation of anomaly from background in EDA method, was done with boxplot. Then the anomaly maps of elements for 3 methods were plotted.   Results and Conclusions Comparison of the maps prepared by three methods, showed a good conformity. Since fractal is a structural method, it is more reliable. Further studies in the regions showed overlapping resulted anomalies by three methods. Pb, Zn and Cd were expanded in North-west, center and South-east. For more confirmation, detailed exploration by using geophysical IP methods is suggested in this area.٠عاد٠سرب Ù Ø±Ù Û Ø§Û Ø±Ø§Ù Ú©Ù Ù Ø¯Ø± رشت٠â Ú©Ù Ù Û Ø¨Ù Ù Ù Û Ù Ù Ø§Ù Ø¯Ø± 20 Ú©Û Ù Ù Ù ØªØ±Û Ø¬Ù Ù Ø¨ غرب اص٠٠ا٠٠ا٠ع شد٠است. بخشâ Ù Ø§Û Ù Ø¹Ø¯Ù Û ØªÙ¾Ù Ø³Ø±Ø®Ø Ú¯Ù Ø´Ù Û Ù Ø Ø®Ø§Ù Ù Ú¯Ø±Ú¯Û Ù ... در Ø§Û Ù Ù Ù Ø·Ù Ù Ø´Ù Ø§Ø³Ø§Û Û Ø´Ø¯Ù Ú©Ù Ø¬Ø¯Ø§Ú¯Ø§Ù Ù ØªØ¹Û Û Ù Ø°Ø®Û Ø±Ù Ø´Ø¯Ù Ù Ø¨Ø¹Ø¶Ø§Ù Ù Ù Ø±Ø¯ Ø¨Ù Ø±Ù â Ø¨Ø±Ø¯Ø§Ø±Û ٠رار گر٠ت٠است. Ø§Û Ù Ù Ø·Ø§Ù Ø¹Ù Ø¨Ù Ù Ù Ø¸Ù Ø± Ø´Ù Ø§Ø³Ø§Û Û Ø¢Ù Ù Ù Ø§Ù Û â ٠ا Ù Ø§Ù Ø¯Û Ø³â Ù Ø§Û Ø³Ø±Ø¨ Ù Ø±Ù Û Ø¯Ø± Ø¨Û Ù Ø¯Ù Ù Ù Ø·Ù Ù Ù Ø¹Ø¯Ù Û ØªÙ¾Ù Ø³Ø±Ø® Ù Ú¯Ù Ø´Ù Û Ù Ø§Ù Ø¬Ø§Ù Ú¯Ø±Ø¯Û Ø¯Ù Ø§Ø³Øª. در Ø§Û Ù Ù Ø·Ø§Ù Ø¹Ù 804 ٠٠٠٠٠خاک Ø¨Ù â Ø·Ù ر Ø³Û Ø³ØªÙ Ø§ØªÛ Ú© در د٠٠رح٠٠برداشت شد٠٠٠٠٠٠٠â ٠ا پس از Ø¢Ù Ø§Ø¯Ù â Ø³Ø§Ø²Û â Ù Ø§Û Ù Ø§Ø²Ù Ø¨Ø±Ø§Û 35 ع٠صر Ø¢Ù Ø§Ù Û Ø² Ø´Ø¯Ù â Ø§Ù د. در Ø§Û Ù Ù Ø·Ø§Ù Ø¹Ù Ø§Ø² 12 ع٠صر Ø¨Ø±Ø§Û ØªØ¬Ø²Û Ù Ù ØªØ­Ù Û Ù Ø§Ø³ØªÙ Ø§Ø¯Ù Ø´Ø¯Ù Ø§Ø³Øª. Ø¨Ø±Ø§Û Ø´Ù Ø§Ø³Ø§Û Û Ù ØªÙ Ú©Û Ú© Ø¢Ù Ù Ù Ø§Ù Û â ٠ا در Ø§Û Ù Ù Ø·Ø§Ù Ø¹Ù Ø§Ø² س٠ر٠ش آ٠ار Ú©Ù Ø§Ø³Û Ú©Ø Ù Ù Ø¯Ø³Ù Ù Ø±Ú©ØªØ§Ù Ù EDA (ØªØ­Ù Û Ù Ø§Ú©ØªØ´Ø§Ù Û Ø¯Ø§Ø¯Ù â ٠ا) است٠اد٠شد٠است. ٠ب٠از Ø§Ù Ø¬Ø§Ù ØªØ¬Ø²Û Ù Ù ØªØ­Ù Û Ù Ø§ØµÙ Û Ø¨Ø§ ر٠شâ Ù Ø§Û Ù Ù Ù â Ø§Ù Ø°Ú©Ø±Ø Ø§Ø¨ØªØ¯Ø§ پردازش Ø§Ù Ù Û Ù Ø¯Ø§Ø¯Ù â ٠ا شا٠٠اص٠اح داد٠â Ù Ø§Û Ø³Ù Ø³Ù Ø±Ø¯ Ù Ø¬Ø¯Ø§Ø³Ø§Ø²Û Ø¯Ø§Ø¯Ù â Ù Ø§Û Ø®Ø§Ø±Ø¬ از Ø±Ø¯Ù Ø§Ù Ø¬Ø§Ù Ú¯Ø±Ø¯Û Ø¯. سپس ٠ر٠ا٠ب٠د٠داد٠â ٠ا Ø¨Ø±Ø±Ø³Û Ø´Ø¯. داد٠â Ù Ø§Û Ø§Ù Ù Û Ù Ø¹Ù Ø§ØµØ± CaØ Mg Ù S ٠ر٠ا٠ب٠د٠د Ù Ù Û Ø¨Ù Û Ù Ø¹Ù Ø§ØµØ± با ØªØ¨Ø¯Û Ù Ù Ú¯Ø§Ø±Û ØªÙ Û Ø³Ø§Ø¯Ù Ù Û Ø§ Ø³Ù Ù¾Ø§Ø±Ø§Ù ØªØ±Û Ù Ø±Ù Ø§Ù â Ø³Ø§Ø²Û شد٠د. ر٠ش آ٠ار Ú©Ù Ø§Ø³Û Ú© با ØªÙ Ø¬Ù Ø¨Ù Ù¾Ø§Ø±Ø§Ù ØªØ±Ù Ø§Û Ø¢Ù Ø§Ø±Û Ø¨Ù Ø¯Ø³Øª آ٠د٠٠٠ر٠٠٠â Ù Ø§Û Ø§Ø³ØªØ§Ù Ø¯Ø§Ø±Ø¯Ø Ù Ù Ø§Ø¯Û Ø± Ø¢Ù Ù Ù Ø§Ù Û Ù Ø²Ù Û Ù Ù Ø¯Ø± ٠٠رد ٠ر ع٠صر Ø¬Ø¯Ø§Ø³Ø§Ø²Û Ú¯Ø±Ø¯Û Ø¯. Ø¨Ø±Ø§Û Ø¬Ø¯Ø§Ø³Ø§Ø²Û Ø²Ù Û Ù Ù Ø§Ø² Ø¢Ù Ù Ù Ø§Ù Û Ø¨Ø§ ر٠ش ٠رکتا٠از Ù Ø¯Ù Ø¹Û Ø§Ø± â ٠ساحت در Ù Ø­Û Ø· GIS است٠اد٠شد. Ø¬Ø¯Ø§Ø³Ø§Ø²Û Ø¢Ù Ù Ù Ø§Ù Û Ø§Ø² Ø²Ù Û Ù Ù Ø¨Ø§ ر٠ش EDA Ù Û Ø² ب٠ک٠ک ٠٠٠دار Ø¬Ø¹Ø¨Ù â Ø§Û Ø§Ù Ø¬Ø§Ù Ú¯Ø±Ø¯Û Ø¯. سپس Ù Ù Ø´Ù â Ù Ø§Û Ù Ø±Ø¨Ù Ø· ب٠٠ر ع٠صر با کاربرد س٠ر٠ش ٠ا٠برد٠رس٠شد٠د. Ø¨Ù â Ø·Ù Ø±Ú©Ù Û Ù Ù Ø´Ù â Ù Ø§Û ØªÙ Û Ù Ø´Ø¯Ù Ø§Ù Ø·Ø¨Ø§Ù Ø®Ù Ø¨Û Ø¨Ø§ ٠٠دار٠د Ù Ù Û Ø±Ù Ø´ Ù Ø±Ú©ØªØ§Ù Û Ø¨Ù Ø¹Ù Øª Ø³Ø§Ø®ØªØ§Ø±Û Ø¨Ù Ø¯Ù Ø¯Ø§Ø±Ø§Û Ù Ø§Ø¨Ù Û Øª اعت٠اد Ø¨Û Ø´ØªØ±Û Ø§Ø³Øª. Ù Ù Ø§Ø·Ù Û Ú©Ù Ø¯Ø± س٠ر٠ش Ø¢Ù Ù Ù Ø§Ù Û Ù Ø´Ø§Ù Ø¯Ø§Ø¯Ù Ø¯Ø Ø¯Ø§Ø±Ø§Û Ø§Ù Ù Ù Û Øª Ø¨Ø§Ù Ø§ØªØ±Û Ø¬Ù Øª ٠طا٠عات Ø¨Ø¹Ø¯Û Ù Û â Ø¨Ø§Ø´Ù د. ع٠اصر Ø§ØµÙ Û Ø´Ø§Ù Ù PbØ Zn Ù Cd در Ø´Ù Ø§Ù â ØºØ±Ø¨Ø ٠رکز ٠ج٠٠ب Ø´Ø±Ù Ø¢Ù Ù Ù Ø§Ù Û Ù Ø´Ø§Ù Ù Û â Ø¯Ù ٠د. Ø¢Ù Ù Ù Ø§Ù Û â Ù Ø§Û Ø¨Ù Ø¯Ø³Øª آ٠د٠با Ù ØªØ§Û Ø¬Û Ú©Ù Ø§Ø² ٠طا٠عات Ø³Ø·Ø­Û Ø¨Ù Ø¯Ø³Øª Ø¢Ù Ø¯Ù Ø§Ù Ø·Ø¨Ø§Ù Ø®Ù Ø¨Û Ù Ø´Ø§Ù Ù Û â Ø¯Ù ٠د. ج٠ت Ø§Ù Ø¬Ø§Ù Ù Ø±Ø§Ø­Ù Ø¨Ø¹Ø¯Û Ø§Ú©ØªØ´Ø§Ù Ù Ø¨Ø±Ø±Ø³Û â Ù Ø§Û Ø¨Û Ø´ØªØ± Ø¢Ù Ù Ù Ø§Ù Û â Ù Ø§Ø Ø§Ø³ØªÙ Ø§Ø¯Ù Ø§Ø² ر٠ش Ú Ø¦Ù Ù Û Ø²Û Ú©Û IP Ù¾Û Ø´Ù Ù Ø§Ø¯ Ú¯Ø±Ø¯Û Ø¯.

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