摘要
地壳上升会使岩金矿床风化剥蚀，而剥蚀程度取决于地壳上升幅度。结合呼玛西部地区岩金矿床阐明区域剥蚀程度的研究方法，从区域剥蚀程度角度提出该区今后找矿工作重点及方向。
The elevation of crust can make rock gold deposit weather and denude and the level of the denudation depends on the scale of the elevation. The research method of the level of regional denudation is clarified and the prospecting direction of rock gold deposit in western Huma is put forward.
出处
《黄金地质》
1998年第3期40-46,共7页
Gold Geology
关键词
岩金矿床
地质发展史
剥蚀程度
金矿床
rock gold deposit, history of geology, level of the denuation, Heilongjiang
