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Exploration and its results of placer type titanium deposits in Kokpektinskaya area, the Republic of Kazakhstan

机译:哈萨克斯坦共和国Kokpektinskaya地区砂矿型钛矿床的勘探及其成果

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An exploration and geological investigation program was carried out from fiscal years 2000 to 2002 in Kokpektinskaya area (120km to south of Ust-Kamenogorsk) in order to increase ore reserves and clarify the resource potential of ilmenite placer deposits. The ilmenite placer deposits in the area are embedded in sandy clay sediment of the Aral Formation of Neogene and hosted within clayey sand above an unconformable surface of weathered basement rocks. They are covered by thick Neo-gene and Quarternary sediments up to 54m in thickness and totally concealed. The program consists mainly of drilling exploration, petrological and magnetic susceptibility study of source granitoids and paleogeomorphology of the pre-Neogene basement. Japan International Cooperation Agency (JICA) and Metal Mining Agency of Japan (MMAJ) conducted the program under the request of the Kazakhstan Government. Drilling exploration in the southern extension of the Bektimir No. 1 deposit showed that it has a strike length of 2.5km, width up to 2km and average thickness of 4.8m. The calculated ore reserves are 13.3 million m~3, average grade is 126.7 kg ilmenite/m~3 (cut-off grade: 100 kg ilmenite/m~3) and ilmenite contained is 1,686,000 tonnes in total. Investigations of source granitoids concluded that the high ilmenite content rock type is little-differentiated granitoids such as gabbro, diorite and monzonite with low magnetic susceptibility. Paleogeomorphological structure contour maps show that the deposits occupy structural channels, which are interpreted as river valleys of the pre-Neogene basement. An area east of the Bektimir No. 1 deposit was selected as an exploration target, which is corresponds to the above conditions. After the area was selected, drilling survey followed, and intercepts of ilmenite concentration were encountered as a new discovery. The showing has a strike length of 2.5km, width of 200 to 600m and thickness of 0.7 to 4.5m. The calculated potential reserves are 1.05 million m~3, average grade is 30.9 kg ilmenite/m~3 and ilmenite contained is 32,500 tonnes (cut-off grade: 20kg ilmenite/m~3). Due to the perception that the deposit enlarges and becomes richer toward the downstream, it is a prospective target for further exploration.
机译:从2000到2002财政年度,在Kokpektinskaya地区(乌斯季卡梅诺戈尔斯克以南120公里)实施了勘探和地质调查计划,以增加矿石储量并阐明钛铁矿砂矿的资源潜力。该地区的钛铁矿砂矿床被埋在新近纪咸水层的砂质粘土沉积物中,并被风化的基底岩石的不整合面之上的黏土砂所包裹。它们被厚厚的新近纪和第四纪沉积物所覆盖,厚度高达54m,并且被完全隐藏。该计划主要包括钻探勘探,源花岗岩类的岩石和磁化率研究以及新近纪前基底的古地貌。日本国际合作局(JICA)和日本金属矿山局(MMAJ)在哈萨克斯坦政府的要求下进行了该计划。在Bektimir 1号矿床南部延伸段的钻探表明,该矿床的走向长度为2.5 km,宽度最大为2 km,平均厚度为4.8 m。计算出的矿石储量为1330万立方米-3,平均品位为126.7千克钛铁矿/ m〜3(最低品位:100千克钛铁矿/ m〜3),所含钛铁矿总量为168.6万吨。对源花岗岩类的研究得出结论,高钛铁矿含量的岩石类型是低分化的花岗岩类,如辉长岩,闪长岩和绿柱石,磁化率低。古地貌构造等高线图表明该矿床占据构造通道,被解释为新近纪前基底的河谷。与上述条件相对应,选择了Bektimir 1号矿床以东的地区作为勘探目标。选择区域后,进行钻孔勘测,并发现钛铁矿浓度的截距是新发现。该显示的罢工长度为2.5公里,宽度为200至600m,厚度为0.7至4.5m。计算出的潜在储量为105万立方米3,平均品位为30.9千克钛铁矿/ m〜3,所含钛铁矿为32,500吨(临界品位:20千克钛铁矿/ m〜3)。由于人们认为该矿床会扩大并向下游富集,因此它是进一步勘探的潜在目标。

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