新疆库木库里盆地砂(砾)岩型铜矿地质特征及其控矿条件分析
Geological features and ore-controlling conditions of sand stone (conglomerate)copper deposit in Kumukuli basin, Xinjiang
-
摘要: 新疆库木库里盆地砂(砾)岩型铜矿位于东昆仑造山带西段,含矿地层为古近系渐新统石马沟组、新近系中新统石壁梁组与上新统红石梁组。铜矿带东西长约170km,南北宽10～60km。已发现铜矿体20多条,矿化体70多条。铜矿化主要受构造、岩性、岩相古地理、古气候等因素控制。矿床属陆相砂砾岩型铜矿。Abstract: The Kumukuli sandst one (conglomerate) copper deposit is located in western segment of East Kunlun orogenic belt,Xinjiang.The strata of ore-bearing are composed of Oligocene Shimagou Formation,Miocene Shibiliang Formation and Pliocene Hong shiliang Formation.The orebelt is 170 km in length of EW and 10-60 km in width of SN.The mineralization was controlled by structures,lithology,lithofacies and paleog eography and paleoclimate.The mineralization type is continental sandstone (conglomerate) copper deposit.
-
-
新疆地质矿产局.新疆维吾尔自治区区域地质志[M].北京:地质出版社,1993.
新疆地质矿产局.新疆维吾尔自治区多重地层划分对比[M].北京:地质出版社,1998.
中科院青藏高原科考队.喀喇昆仑山-昆仑山地区地质演化[M].北京:科学出版社,1990.
崔军文,等.阿尔金断裂系统[M].北京:地质出版社,1999.
樊晶,等.新疆库木库里盆地铜矿化特征及找矿前景[A].昆仑-秦岭-大别山系地质构造与资源环境学术研讨会论文集[C].西安:西安地图出版社,2002.
肖爱芳,等.新疆库木库里盆地渐新-上新统孢粉组合特征与古气候演变[J].陕西地质,2003(1):21.
黄崇轲,等.中国铜矿床[M].北京:地质出版社,2001.
计量
- 文章访问数: 2343
- HTML全文浏览量: 0
- PDF下载量: 3314
下载:
