1) Huangjinwa
黄金洼
1.
Geological Feature and Ore-control Factors of Huangjinwa Sn Despoit,De'an County in Jiangxi Province;
江西德安黄金洼锡矿地质特征及控矿因素
2) loess ridge and depression
黄土梁洼
1.
It causes special loess ridge and depression geomorphic feature.
西安地裂缝是西安地区与秦岭山前长安—临潼断裂有关的一组NE-NEE走向的南倾陡倾角正断面的地表反映,它形成了特有的黄土梁洼地貌。
3) DaHuangPuWa detention area
大黄堡洼
4) Buwa gold deposit
埠洼金矿
1.
Buwa gold deposit occur in mediumshallow subductile and ductilebritile shear belts which are in TTG rock series.
埠洼金矿产于泰山（岩）群ＴＴＧ岩系中，赋存于中浅层次韧性、韧脆性剪切带内，矿体呈右行侧列式透镜体分布，成矿物质及热液主要来源于泰山（岩）群绿岩地层，其δ１８Ｏ值为５。
5) Caojiawa gold deposit
曹家洼金矿
1.
Study on comprehensive information and prediction of ore formingtarget in Xiaoyingezhuang ore district of Caojiawa gold deposit;
曹家洼金矿小尹格庄矿区综合信息研究与成矿靶区预测
6) Zaiwulongwa gold mine
宰乌隆洼金矿
1.
Through analyzing the geologic characteristic and geochemical characteristic of the Zaiwulongwa gold mine in the Litang county of Sichuan province,and conclusion is drawn that the Zaiwulongwa gold mine is a low temperature and hot liquid deposit.
通过对四川省理塘县宰乌隆洼金矿矿床的地质特征和地球化学特征进行分析,认为该矿床属低温热液型金矿床。
补充资料：鼻洼
1.见"鼻洼子"。
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