樟岭—开库康地区
位于黑龙江省漠河县境内的二十五站、开库康、樟岭一带。
该区地处上黑龙江冒地槽褶皱带的中部。区内以侏罗系火山岩为主,并见有零星分布的第三系。燕山期黄岗岩皆是小岩体出露。西北向构造发育。
西南部为额木尔山,形成南高北低的总地势,为一低山丘陵地貌景观。黑龙江及其支流构成树枝状水系。
区内已发现砂金矿床多处,沙金矿点十几处,旧采区多处。
本区砂金地质工作程度不高。今后应在盘古河及其支流(乌里克河、塔里亚河、大头卡河、古鲁干河)开展砂金矿普查找矿工作。
Zhang Ling - kaikukang area
位于黑龙江省漠河县境内的二十五站、开库康、樟岭一带。
The twenty-five station, kaikukang, Zhang Ling area is located in Mohe County County of Heilongjiang province.
该区地处上黑龙江冒地槽褶皱带的中部。区内以侏罗系火山岩为主,并见有零星分布的第三系。燕山期黄岗岩皆是小岩体出露。西北向构造发育。
The area is located on the central Heilongjiang geosyncline fold belt. Jurassic volcanic rocks are mainly in the area, and there are third series. Yanshan is a small yellow granite outcrops. NW trending tectonic development.
西南部为额木尔山,形成南高北低的总地势,为一低山丘陵地貌景观。黑龙江及其支流构成树枝状水系。
For the southwest Emuer mountain formation, total low-lying South High North, is a hilly landscape. Heilongjiang and its tributaries form a branch stream.
区内已发现砂金矿床多处,沙金矿点十几处,旧采区多处。
The district has found sand deposit, alluvial gold ore mining area of more than a dozen old.
本区砂金地质工作程度不高。今后应在盘古河及其支流(乌里克河、塔里亚河、大头卡河、古鲁干河)开展砂金矿普查找矿工作。
The degree of geological work in the area of placer gold is not high. In the future, in the disc ancient river and its tributaries (urique River, Talia River, the big card River, the ancient Lugan River) to carry out sand prospecting for gold prospecting work should be.