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首页> 外文期刊>Resource Geology >Heavy Mineral Placer Sand Deposits of Kontiagarh Area, Ganjam District, Orissa, India
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Heavy Mineral Placer Sand Deposits of Kontiagarh Area, Ganjam District, Orissa, India

机译:印度奥里萨邦Ganjam区Kontiagarh地区的重矿物砂砂矿床

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The Kontiagarh placer deposit in the Ganjam district, Orissa, India extends in northeast direction having a width of 700-1000 m. A total of 187 samples were collected meterwise from 55 bore holes in a grid pattern from beach, frontal, intermediate and back dunes covering an area of approximately 1 km~2. Light minerals decrease in size from the beach to the back dunes, whereas the size distribution of heavy minerals in the beach and dunes is more or less uniform. The average heavy mineral content in the beach and dunes vary from 9.38 percent to 24.20 percent. The heavy minerals are ilmenite, garnet, sillimanite, rutile, monazite, and zircon with trace amounts of magnetite, hornblende, diopside, sphene, tourmaline, and epidote. Heavy minerals are mostly less than 350 urn in size, with a peak distribution in the range between 180 and 125 um. Ilmenite shows exsolution intergrowth with hematite. Mineral chemistry of ilmenite, hematite, leucoxene, magnetite, monazite and sillimanite are examined by EPMA. Leucoxene is lower in Fe and higher in Ti, Al, Cr and V than ilmenite. The litho-units of the Precambrian Eastern Ghats Mobile Belt, comprising primarily khondalite, charnockite, calc-silicate granulite and gneiss, are the source of heavy minerals for this deposit. The bulk sample has 7.30 percent ilmenite, 5.24 percent sillimanite, 9.16 percent garnet, 0.18 percent rutile, 0.14 percent monazite, 0.06 percent zircon and 0.52 percent other heavy minerals. The deposit has good potential for economic exploitation of ilmenite, rutile, sillimanite, monazite, zircon and garnet.
机译:印度奥里萨邦Ganjam区的Kontiagarh砂矿矿床向东北方向延伸,宽度为700-1000 m。从海滩,前沙丘,中沙丘和后沙丘的55个钻孔中,以网格为单位,以米为单位共收集了187个样本,覆盖面积约1 km〜2。从海滩到沙丘,轻质矿物的尺寸减小,而海滩和沙丘中重质矿物的尺寸分布或多或少均匀。海滩和沙丘中的平均重矿物质含量在9.38%至24.20%之间。重矿物包括钛铁矿,石榴石,硅线石,金红石,独居石和锆石,其中含有少量磁铁矿,角闪石,透辉石,蝶粉,电气石和附子。重矿物的大小大多小于350 n,峰值分布在180至125 um之间。钛铁矿显示与赤铁矿互溶共生。 EPMA检查了钛铁矿,赤铁矿,白二烯,磁铁矿,独居石和硅线石的矿物化学。与钛铁矿相比,白三烯的铁含量较低,而钛,铝,铬和钒的含量较高。前寒武纪东部高止山脉移动带的岩石单元主要是高岭石,方钠石,钙硅酸盐颗粒和片麻岩,是该矿床重矿物的来源。大块样品中含有7.30%的钛铁矿,5.24%的硅线石,9.16%的石榴石,0.18%的金红石,0.14%的独居石,0.06%的锆石和0.52%的其他重矿物。该矿床具有开发钛铁矿,金红石,硅线石,独居石,锆石和石榴石的良好潜力。

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