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肯德可克铁矿区位于东昆仑西段祁曼塔格北缘,矿区面积约4Km~2。矿区及其附近显示的构造线方向为NWW至EW向,且以后者为主。矿区于1977年_开始钻探验证,三年来的资料证实,该矿为一中型铁矿,矿体主要受构造控制,成因类型虽有各种看法,但多数人认为应属矽卡岩型。本文试图根据历年所取得的资料对该矿区的控矿构造及其对矿液运移的控制进行初步探讨。由于工作性质所限,未能进行专门性的研究工作,因此所取得的资料不够完整,同时由于业务水平低,看法很不成熟,不可避免地会出现一些错误,不妥之处,敬请批评指正。
Kendakeke iron ore is located in the western part of East Kunlun Qimen Tage grid north of the mining area of about 4Km ~ 2. The tectonic lines shown in the mining area and its vicinity are in the NWW to EW direction with the latter dominated. The mine started its drilling verification in 1977. The data from the past three years confirm that the mine is a medium-sized iron ore mine and the ore body is mainly controlled by structure. Although various types of genetic types are considered, most people think that they should belong to the skarn type. This article tries to make preliminary study on the ore-controlling structure and its control over the movement of ore-bearing liquid in the mining area according to the data obtained over the years. Due to the nature of the work, the failure to carry out specialized research and the incompleteness of the information obtained and the unmanageable view due to the low level of business will inevitably lead to some mistakes and discrepancies. Please criticize Correction