Geological Characteristics and Prospecting Indicators of Y Deposit in Taidulong-Kuzhuping Area,Northern Guangdon
Taidulong-Kuzhuping Y ore deposit in northern Guangdong is located at the junction of the Yangtze River Y ore field and Baishun Y ore field.The area is characterized by intense magmatic activity,developed structures,and superimposed hydrothermal activity,indicating a promising prospecting.Y ore body occurs in the fissures of silicified cataclasite and granitic cataclasite,is strictly controlled by fault structure,and is a me-dium-low temperature hydrothermal deposit associated with silicified fault zone.Small Cretaceous rock masses and basic dike rocks interspersed in complex rock masses,and the junction of different fault structures and rock alteration indicators(silicification,hematitization and limonitization,etc.)are important prospecting indica-tors.
Y depositGeological characteristicsProspecting indicatorsTaidulong-Kuzhuping area in northern Guangdong
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