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1984年发现的卡特杰布特铅锌矿位于西澳大利亚西金伯利地区的菲茨罗伊克罗辛东南80公里处,为一长3公里、宽50～150米、厚20米的缓倾斜矿床(5°～8°),产于泥盆纪白云岩、粉砂岩和石灰岩层内。主要金属矿物为闪锌矿(ZnS)和方铅矿(PbS),它产于厚约34米的自云岩层系的底部。大部分高品位矿化带产于两个不同的透镜体内。上部透镜体厚2～6米,下部透镜体厚2～5米,
The 1984 discovery of the Kat Jabil Pb-Zn mine is located 80km southeast of Fitzroy Croosin in the Western Kimberley region of Western Australia, a gently inclined deposit of 3 km long, 50-150 m wide and 20 m thick (5 ° ~ 8 °), occurring in the Devonian dolomite, siltstone and limestone. The main metallogenic minerals are sphalerite (ZnS) and galena (PbS), which are produced at the bottom of a dolomite formation about 34 meters thick. Most high-grade mineralized belts are produced in two different lenses. The upper lens body thickness of 2 to 6 meters, the lower lens body thickness of 2 to 5 meters,