1) lateritic bauxite
红土型铝土矿
1.
Geological character and ore mechanism of lateritic bauxite depositsin Boke,Guinea
几内亚共和国博凯地区红土型铝土矿地质特征和成矿机理初探
2) aluminous laterite
高铝红土矿<冶>
3) lateritic gold deposit
红土型金矿
1.
Study on mechanism of elements migration and gold enrichment during weathering process: an example from critical lateritic gold deposits international;
风化作用元素迁移与金富集机制研究——以国内外典型红土型金矿床为例
2.
Recently,a batch of lateritic gold deposits had been also found in the belt.
哀牢山浅变质岩带分布于哀牢山深大断裂与九甲—安定深大断裂之间的古生界与中生界地层中,哀牢山金矿带目前已发现的主要金矿床(点)均产于其中,金矿类型以蚀变岩型和石英脉型为主,但近年来,相继发现了一批红土型金矿。
3.
Since being controlled by climate,lateritic gold deposits are mainly distributed in the south China,and dominated by weathering reformed typed.
红土型金矿床是原生金矿化遭受红土化作用改造所形成的一种表生金矿床,包括“红色粘土型”和“铁帽型”金矿床。
4) lateritic gold deposits
红土型金矿
1.
This paper analyzed the geological characters, main controlling factors, and the mechanism of dissolution, migration and precipitation of Au in lateritic gold deposits.
对红土型金矿的地质特征、主要控矿因素、金的溶解迁移与沉淀富集机理进行了分析。
2.
Lateritic gold deposits are superficial gold deposits parasite on mantle rock of laterite.
红土型金矿是以红土风化壳为寄生体的表生金矿床，具有规模大、品位低、易采、易选冶、见效快及效益高等特点。
5) laterite gold deposit
红土型金矿
1.
Some laterite gold deposits have been discovered in this area.
湘南为我国著名的有色金属成矿区,近年来相继发现了一批红土型金矿床(点)。
2.
The gold deposits are obviously different from laterite gold deposits abroad.
由于特殊的地质构造条件和气候、地貌条件 ,该类型金矿与国外的红土型金矿存在明显的差异 :红色粘土型金矿剖面发育差 ,红土化程度低 ;对源岩依存度高 ;铁铝含量低、硅含量高 ;矿石处在富粘土矿物阶段 ,少见三水铝石 ,一般为伊利石和高岭石共存。
6) lateritic deposit
红土型矿床
1.
All of the deposits which are related genetically to formation of weathering lateritic crust with a certain industrial value should fall to a category of "a lateritic deposit".
凡在风化壳红土形成过程中形成,并保留至今的具有工业价值的各类矿床,均可称其为“红土型矿床”。
补充资料：三水铝石,三水铝矿
CAS：14762-49-3
中文名称：三水铝矿；水铝矿；三水铝石,三水铝矿
英文名称：Gibbsite；alpha-aluminium hydroxide；alpha-aluminum hydroxide；hydrargilite
中文名称：三水铝矿；水铝矿；三水铝石,三水铝矿
英文名称：Gibbsite；alpha-aluminium hydroxide；alpha-aluminum hydroxide；hydrargilite
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