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新疆红柳河鬣刺岩是我队与南京大学地质系关于“东天山构造演化及成矿规律研究”协作项目组在红柳河地区测制地质剖面中,经显微镜鉴定,发现了显微中空鬣刺结构而确认的.红柳河鬣刺岩产于新疆哈密市东南200公里,红柳河火车站东北7公里处的红柳河基性—超基性岩体北侧枕状玄武岩中,伴有基性火山碎屑岩.岩体形态、规模尚未详细工作,产出时代尚有争论(震旦系?二迭系?).鬣刺岩以枕状体形态产出,枕体间为基性玻屑凝灰岩充填,与其紧密伴生的枕状玄武岩的关系有待进一步工作.
Hongliuhe, Xinjiang malachite is our team and the Department of Geology, Nanjing University on the “East Tianshan tectonic evolution and metallogenic law” collaborative project team in the Hongliuhe area geological section, the identification of the microscope and found that the micro-hollow Structure of Hongliuhe hyaenite produced in Hami, Xinjiang 200 kilometers southeast of Hongliuhe Railway Station 7 km northeast of the Hongliuhe basic - ultramafic rocks north of pillow-like basalt, accompanied by the basic volcano Clastic rocks. The shape and size of the rock mass have not been worked out in detail yet, and the age of output still remains controversial (Sinian? Permian?). The hyponatre comes in the form of a pillow-like body with the base vitreous tuff Filling, with its closely associated pillow-basalt relationship needs further work.