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  • Chromite Ore Mining and Associated Factors in the Muslim Bagh Ophiolite . . .
    Background: Chromite is a metallic mineral composed of chromium, iron, and oxygen (FeCr2O4) Pakistan is bestowed with numerous economic minerals and chromite is one of them It has major deposits in Muslim Bagh Ophiolites, Muslim Bagh area of Balochistan province, Pakistan Objectives: The objectives of this study are to analyze the chromite ore mining and the associated factors in the Muslim
  • Health risk assessment of chromium contamination in the nearby . . .
    The main objective of this work was to investigate the root cause(s) of the various diseases in the local population, living in the proximity of chromium mining area The analytical work was done on the samples of drinking water, soil and human blood, collected from the study area The chosen study area is known as Muslim Bagh, located in the Balochistan province of Pakistan The area is well
  • Risk assessment of radon in soil collected from chromite mines of . . .
    Average values of radium activity for Khanozai and Muslim Bagh chromite mines were found 3 02 and 3 09 Bq kg, respectively The values obtained for radon exhalation rate were found below the average value of 57 60 Bq m 2 h recommended by UNSCEAR Therefore, it is concluded that the mines understudy are safe from health hazards related to radon gas
  • Chromite from Muslim Bagh, Killa Saifullah District, Balochistan, Pakistan
    The podiform chromite deposits in comprises the Bela, Muslim Bagh, Zhob and Waziristan-Khost ophiolites in Pakistan and bordering Afghanistan Pournamdari, Mohsen, Hashim, Mazlan, Pour, Amin Beiranvand (2014) Application of ASTER and Landsat TM Data for Geological Mapping of Esfandagheh Ophiolite Complex, Southern Iran
  • Petrology of the mantle rocks from the Muslim Bagh Ophiolite . . .
    high grade chromite ore As a result, the whole Muslim Bagh ophiolite has been mapped at scales between 1: 10,000 and 1:24,000 and compiled in the excellent maps of Rossman et al (1971) This study is an initial report of the ongoing detailed work on the petrology of mantle rocks from the Muslim Bagh ophiolite and
  • GEOLOGICA v. 8, Article No. 4
    The chromite deposits were first discovered by Vredenburg 1901 during the course of regional reconnaissance mapping of Baluchistan and parts of eastern Persia The chromite mining started in 1903 on small scale and is continuing till today at very large scale Figure 1 The map showing the mines and mineral waste sites in Muslim Bagh
  • Beneficiation Studies on the Low-Grade Chromite of Muslim Bagh . . .
    Chromite is the only commercial source of chromium, which is used in metallurgical, refractory and chemical industries The most extensive deposits of chromite in Pakistan exist around Muslim Bagh in the Zhob Valley (Ahmed, 1975) These deposits may be placed in five different groups accor-ding to their locations, namely, Khanozai, Jungtogarh,
  • Comprehensive assessment of radiological hazards in chromite mines at . . .
    The concentrations of natural radioactivity in soil samples collected from chromite mines of two different towns, Khanozai and Muslim Bagh, districts of Pishin and Killa Saifullah, respectively, were measured using a high purity germanium (HPGe) detector The average values of 226Ra, 232Th and 40K in soil of Khanozai chromite mines were found to be 26 414, 37 321 and 404 561 Bq kg-1, respectively
  • Risk assessment of radon in soil collected from chromite mines of . . .
    Average values of radium activity for Khanozai and Muslim Bagh chromite mines were found 3 02 and 3 09 Bq kg, respectively The values obtained for radon exhalation rate were found below the average value of 57 60 Bq m 2 h recommended by UNSCEAR Therefore, it is concluded that the mines understudy are safe from health hazards related to radon gas
  • Risk assessment of radon in soil collected from chromite mines of
    The average values of radon concentration in Khanozai and Muslim Bagh chromite mines were found 1 23 ± 0 69 and 1 26 ± 0 08 kBq m3 , respectively The average values of radon exhalation rate and radium activity were found below the permissible limits of 57 60 Bq m2 h and 35 Bq kg, respectively (UNSCEAR, 2000) Therefore, the workers of mines





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