这一铜矿,分布在太行山东麓,唐、曲、完、满、涞、易、房等县都有露头可见,且均产出于下寒武系馒头统紫色页岩中的绿色层,层位稳定。在绿色层的下部为含铜的绿色砂页岩,铜矿物均为孔雀石,沿层理面产出,矿层之上为发育较稳定的绿色页岩,再上为紫色页岩及鲕状灰岩,矿层之下为砂页岩互层间夹砾石层。经光谱及化学分析结果,矿石中除含有铜外,还有磷、钛、钒、镍、铬及铍等元素。绿色页 This copper mine, located in the eastern foot of the Taihang Mountains, Tang, Qu, End, Manchu, Ehime, Yi, Fang and other counties are outcrops, and are produced in the Lower Cambrian system purple purple shale in the green layer, Stable. In the lower part of the green layer is a copper-bearing green sandstone shale. The copper minerals are malachite and are produced along the bedding plane. Above the ore layer is a relatively stable green shale, followed by purple shale and oolitic Limestone, below the seam for sand shale inter-layer gravel layer. The results of spectroscopy and chemical analysis, in addition to copper ore, there phosphorus, titanium, vanadium, nickel, chromium and beryllium and other elements. Green page