论文部分内容阅读
本矿区属层状浅海相沉积石灰石矿床。矿体构造复杂,断层和废石夹层多,喀斯特溶洞裂隙发育。主要矿层以纯质石灰岩为主,次为碎屑灰岩和白云质砂质灰岩。纯质石灰岩呈粗粒、细粒晶质和致密隐晶质显微粒状构造,普氏硬度f=8~10,松散系数1.54,容重2.660~2.724吨/米~3,化学成分含CaO50%以上,MgO小于2.5%以下,为优质工业原料。我矿为山坡露天机械化开采,由于存在大量夹缝土(包括裂隙土、夹层土、溶洞土),爆破后与矿石混在一起,形成“土石混合物”,呈大块片状,粘结得象年糕一样,含泥量30%左右。
The mining area is a shallow marine sedimentary limestone deposit. Complex ore body structure, fault and waste rock interlayer, karst cave fracture development. The main strata are mainly pure limestone, followed by clastic limestone and dolomitic sandy limestone. Pure limestone is coarse grain, fine grain crystal and dense cryptocrystalline microstructure, Props hardness f = 8 ~ 10, loose coefficient of 1.54, bulk density of 2.660 ~ 2.724 tons / m ~ 3, the chemical composition of CaO containing more than 50% , MgO less than 2.5% for the quality of industrial raw materials. Because of the existence of a large amount of clamped soil (including fissure soil, mezzanine soil and karst soil), my mine is mixed with ores to form a “soil-rock mixture” in the form of a large piece of sheet that adheres like a rice cake , Mud content of about 30%.