1) underground debris flow
井下泥石流
1.
Mechanism analysis on forming underground debris flow in Chengchao Mine;
程潮铁矿井下泥石流形成机理分析
2) subaqueous debris flow
水下泥石流
1.
,so it was determined to be dominantly subaqueous debris flow deposit due to slump.
地震剖面解释和钻井岩芯观察表明,伊通地堑古近系永一段底部发育一个面积>400km2、厚达250m的大型湖底扇,作为永一段层序的低位扇体,其主要由细-中砂岩和少量砂砾岩组成,砂岩中含较多砂岩角砾、泥岩碎块或泥砾,卷曲纹理、液化变形、球状-枕状构造、微断层等准同生变形构造十分发育,体现了湖底扇主要为滑塌型水下泥石流沉积。
3) quantity of underground slime and sand
井下泥砂量
1.
Based on the comprehensive comparison of the quantity of underground slime and sand,and the forms of depositing basins in mines that using filling method at the home and abroad,the method of treating and the quantity of underground slime and sand in Dongguashan Copper Mine are determined.
在综合比较国内外多家采用充填法采矿的井下矿山的坑内泥砂清理量和沉淀池形式的基础上 ,确定了冬瓜山铜矿井下泥砂量和坑内泥砂处理的方
4) submudline wellhead
泥线下井口
6) well-cementing cement
固井水泥石
补充资料：白银有色金属公司深部铜矿主井和副井
白银有色金属公司深部铜矿主井和副井
白银有色金属公司深部铜矿主井和副井
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条