Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

分析粉石英、斜绿泥石的晶体结构和表面性质以及油离子捕收剂时的溶液化学。

The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

在西南地区晚二叠世煤中首次发现了液成因的硫锰矿和硫砷锑矿、碱性火山灰成因的胶态锐钛矿和陆成因的斜绿泥石。

Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

析粉英、斜的晶体结构和表面质以及油酸作阴离子捕收剂时的溶液化学。

The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

在西南地区晚二叠世煤中首次发现了液成因的硫锰矿和硫砷锑矿、碱火山灰成因的胶态锐钛矿和陆源碎屑成因的斜。

Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

分析粉英、斜的晶体结构和质以及油酸作阴离子捕收剂时的溶液化学。

The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

在西南地区晚二叠世煤中首次发现了液成因的硫锰矿和硫砷锑矿、碱火山灰成因的胶态锐钛矿和陆源碎屑成因的斜。

Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

分析粉石英、斜绿泥石的晶体结构表面性质以及油酸作阴离子捕收剂时的溶液化学。

The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

在西南地区晚二中首次发现了液成因的锰砷锑、碱性火山灰成因的胶态锐钛陆源碎屑成因的斜绿泥石。

Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

分析粉石英、斜绿泥石的晶体结构和表面性质以及油酸作阴离子捕收剂时的溶液化学。

The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

在西南地区晚二叠世煤中首次发现了液因的硫锰矿和硫砷锑矿、碱性火山灰因的胶态锐钛矿和陆源碎屑因的斜绿泥石。

Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

分析粉石英、斜绿泥石的晶体结构表面性质以及油酸作阴离子捕收剂时的溶液化学。

The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

在西南地区晚煤中首次发现了液成因的锰矿锑矿、碱性火山灰成因的胶态锐钛矿陆源碎屑成因的斜绿泥石。

Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

分析粉石英、斜绿泥石的晶体结构和表面性质以及油酸作阴离子捕收剂时的溶液化学。

The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

在西南二叠世煤中首次发现了液成因的硫锰和硫砷、性火山灰成因的胶态锐钛和陆源碎屑成因的斜绿泥石。

Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

析粉石英、石的晶体结构和表面质以及油酸作阴离子捕收剂时的溶液化学。

The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

在西南地区晚二叠世煤中首次发现了液成因的硫锰矿和硫砷锑矿、碱火山灰成因的胶态锐钛矿和陆源碎屑成因的石。

Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

分析粉石英、斜绿泥石的晶体结构和表面质以及油酸作阴离子捕收剂时的溶液化学。

The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

西地区晚二叠世煤中首次发现了液成因的硫锰矿和硫砷锑矿、碱灰成因的胶态锐钛矿和陆源碎屑成因的斜绿泥石。