ELECTRON PROBE SPECTRUM ANALYSIS OF CHROMITE IN MENGYIN KIMBERLITES, SHANDONG PROVINCE
CHI Hui-zhong1, WANG Da-qian2, LI Jing-guo2, WU Yue2, LI Chun-ling2, ZHANG Yuan-yuan2, LIU Jin-xiu2, ZHAO Mei-jing2
1. Shenyang Laboratory of National Jewelry and Jade Quality Supervision and Inspection Center, Shenyang 110013, China; 2. Shenyang Center of China Geological Survey, Shenyang 110032, China
Abstract:Chromite is one of the main indicator minerals in kimberlite diamond deposit. Accurate content analysis of the chemical compositions such as FeO, MgO, Cr2O3, Al2O3 and TiO2 in chromite is the key for the naming of chromite, and significant indication for kimberlite diamond deposit prospecting as well. The electron probe spectroscopy is used to analyze the major chemical elements in chromite, and the micro-area chemical analysis of measured samples to infer the mineral name. The analysis results of 25 single mineral samples show that the contents of major chemical components are 15.666%-29.971% of FeO, 7.286%-11.477% of MgO and 56.421%-71.111% of Cr2O3, with minor chemical components MnO 0.012%-0.382%, Al2O3 0.871%-8.993% and TiO2 0.074%-3.375%. The total mineral chemical composition is 99.117%-100.877%. The chemical composition of single mineral is equivalent to that of chromite. According to the mineral characteristics by artificial heavy mineral identification and positions of ion groups A and B, it can be determined that the measured sample is magnochromite.
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