山西科技
山西科技
산서과기
SHANXI KEJI
2014年
4期
59-61,62
,共4页
黄芮%姬丽娜%邹春林%魏庆喜
黃芮%姬麗娜%鄒春林%魏慶喜
황예%희려나%추춘림%위경희
地质特征%矿床成因%八角锌矿床%云南省
地質特徵%礦床成因%八角鋅礦床%雲南省
지질특정%광상성인%팔각자광상%운남성
geological characteristics%mineral deposit genesis%Bajiao Zinc deposit%Yunnan Province
云南省楚雄八角锌矿床位于祥云-新平多金属成矿带中南段。通过对楚雄八角锌矿床地质特征的阐述，指出矿体明显受地层岩性和构造的联合控制，矿床成因为构造及地层控制的地下水中～低温热液矿床，并总结了控矿因素和找矿标志。
雲南省楚雄八角鋅礦床位于祥雲-新平多金屬成礦帶中南段。通過對楚雄八角鋅礦床地質特徵的闡述，指齣礦體明顯受地層巖性和構造的聯閤控製，礦床成因為構造及地層控製的地下水中～低溫熱液礦床，併總結瞭控礦因素和找礦標誌。
운남성초웅팔각자광상위우상운-신평다금속성광대중남단。통과대초웅팔각자광상지질특정적천술，지출광체명현수지층암성화구조적연합공제，광상성인위구조급지층공제적지하수중～저온열액광상，병총결료공광인소화조광표지。
Chuxiong Bajiao Zinc deposit of Yunnan Province is located in south central section of Xiangyun-Xinping polymetallic metallogenic belt. Through expounding the geological characteristics of Chuxiong Bajiao Zinc deposit, this paper points out that the ore body is obviously under the joint control of stratum’s lithology and structure, and the mineral deposit genesis is groundwater low-to-moderate hydrothermal deposit controlled by the structure and stratum, and sumsup the ore-controlling factors and ore-prospecting marks.
