The Geological Characteristics and Prospecting Direction of Ta-Nb Deposits in Laomuzhushi Mountain, Shangcheng, Henan
GUO Jun-gang1,2.3, BIAN Xiao-dong1,2.3, WANG Pan-xi1,2.3, WANG Shou-jing1,2.3
1.Zhengzhou Institute of Multipurpose Utilization of Mineral Resources, Chinese Academy of Geological Science, Zhengzhou, Henan 450006, China; 2. National Engineering Center for Multipurpose Utilization of Non-Metallic Mineral Resources, Zhengzhou, Henan 450006, China; 3. Key Laboratory for Polymetallic Ore Evaluation and Utilization, MLR, Zhengzhou, Henan 450006, China
Abstract：Laomuzhushi Ta-Nb ore field is located on the north side of the Dabie Mountains, in the core of Qinling-Dabie organic belt where east Qinling fold belt of Qinling fold system extends eastward. Here, a Ta-Nb deposit is found in K-feldspar leucogranulitite of the lower Dahongkou formation . The main Nb-and Ta-bearing minerals are niobite, ilmenorutile and titanium-rich hematite. The Ta-Nb ores there are characterized by fine grains and high level of dispersion. Laomuzhushi Ta-Nb deposit is metamorphic origin . In this paper, our focus is on the deposit geological characteristics and the ore-forming and ore-controlling factors, which are indicative of similar Ta-Nb deposits and other rare metal deposits in South Henan.
郭俊刚，卞孝东，王盘喜，王守敬. 河南商城县老母猪石山钽铌矿地质特征及找矿方向[J]. 中国地质调查, 2014, 1(1): 32-37.
GUO Jun-gang, BIAN Xiao-dong, WANG Pan-xi, WANG Shou-jing. The Geological Characteristics and Prospecting Direction of Ta-Nb Deposits in Laomuzhushi Mountain, Shangcheng, Henan. , 2014, 1(1): 32-37.
2014, Vol. 1 
