Geology, mineralogy and geochemistry of the cayeli massive sulfide ore deposit, Rize, NE Turkey

机译：土耳其东北部里泽的cayeli块状硫化物矿床的地质，矿物学和地球化学

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The Cayeli massive sulphide ore body occurs within Upper Cretaceous dacitic flows and pyroclastics and consists of a massive sulfide lens with varying ore zones and a well-developed mineralised stockwork. The main ore body strikes N30E, plunges 15 to 20 deg NE and dips 60 to 80 deg NW. It is 450 m long, 400 m wide, up to 120 m thick and has a minable reserve of 8.87 million tonnes above 880m level grading on average at 5.19

机译：Cayeli块状硫化物矿体存在于上白垩统的山洪流和火山碎屑中，并由一块块状硫化物晶状体组成，具有不同的矿区和发达的矿化储层。主矿体撞击N30E，向北倾斜15至20度，向西北倾斜60至80度。它长450 m，宽400 m，厚达120 m，可开采储量8.8百万吨，高于8.8亿吨，平均分级为5.19。

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《Biennial SGA meeting;Quadrennial IAGOD symposium》|1999年|p.459-462|共4页
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M.Akcay; M.Arar;
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Geology, mineralogy and geochemistry of the cayeli massive sulfide ore deposit, Rize, NE Turkey

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