摘要
广西象州县新造铅锌矿床位于大瑶山西侧铅锌铜多金属成矿带上,其铅锌矿体赋存于泥盆系下统白云岩的切层断裂及其层间破碎带中,矿化的岩性为白云岩。结合区域矿床对比,认为新造铅锌矿床属中—低温沉积—热卤水改造型铅锌矿床。该区具有良好的铅锌成矿条件和找矿远景。
The Xinzao Pb-Zn deposit in Xiangzhou County of Guangxi Autonomous Region is located in the Pb-Zn-Cu polymetallic metallogenic belt which is on the west side of Dayaoshan. The orebodies are with in the incision fracture and fault zone between the strata of Lower Devonian dolostone with the mineralizing lithology being dolostone. Combined with the comparison among the regional deposits, it has been believed that the Xinzao Pb-Zn deposit is a mid-low temperature sediment-hot brine reformed Pb-Zn deposit. The favorable ore-forming conditions for Pb-Zn deposit with the prospecting perspective in this area has also been concluded.
出处
《矿产与地质》
2009年第6期533-537,共5页
Mineral Resources and Geology
关键词
铅锌矿床
地质特征
找矿方向
广西象州
Pb-Zn deposit
geological characteristics
prospecting direction
Xiangzhou of Guangxi
