For the first time, geologic features and exploitation conditions of the Ordovician graystone with reservoir strata are explored in the plain. 首次初步探索了該區奧陶系灰巖熱儲的地質(zhì)特征及開(kāi)發(fā)條件。
The genesis of Keketale Lead-Zinc Deposit is discussed by means of its geological characters and geochemical characters, providing the basis for sulfide type Lead-Zinc deposit. 通過(guò)可可塔勒鉛鋅礦床地質(zhì)特征及地球化學(xué)特征的研究，探討可可塔勒鉛鋅礦床的成因，為尋找硫化物型鉛鋅礦提供了依據。
