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、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次发现了液成因的和砷锑、碱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.

分析粉石英、绿泥石晶体结构和表面性油酸作阴离子捕收剂时溶液化学。

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硫锰矿和硫砷锑矿、碱性火山灰成胶态锐钛矿和陆源碎屑成绿泥石。

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的硫锰矿和硫砷锑矿、碱性火山灰的胶态锐钛矿和陆源碎的斜绿泥石。

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.

在西区晚二叠世煤中首次发现了液成因的硫锰矿和硫砷锑矿、山灰成因的胶态锐钛矿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、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.

在西南地区晚二叠首次发现了液成因的硫硫砷锑、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。

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的硫锰矿和硫砷锑矿、碱性火山的胶态锐钛矿和陆源碎屑的斜绿泥石。