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天宇矿床(点)位于东天山地区的中天山地块北缘,阿齐库都克一沙泉子断裂带南侧,含矿岩体为一套基性—超基性杂岩,出露面积小于1km2,具有中国典型的小岩体成矿特征。在对该矿床的研究中(唐冬梅等,2009;钟富善等,2008;宋林山等,2008),多偏重于分析其含矿岩体的地质与地球化学特征,
The Tianyu deposit (point) is located in the northern margin of the Middle Tianshan Plot in the east Tianshan area and is located to the south of the Azichuoduke-Shaquanzi fault zone. The ore-bearing rock mass is a set of basic-ultramafic complexes with an exposed area of less than 1km2, with typical Chinese small rock mass mineralization characteristics. In the research on this deposit (Tang Dongmei et al., 2009; Zhong Fushan et al., 2008; Song Linshan et al., 2008), they mostly focused on analyzing the geological and geochemical characteristics of their ore-