大水-红柳河地区位于东天山东部,西起大水岩体,东到红柳河的水沟子井。处于塔里木板块中的塔里木古陆内的北山古生代裂陷槽中,北临木扎尔特-红柳河板块缝合带。出露元古界、古生界和新生界。侵入岩较发育,期次频繁等特点。岩浆活动始于早古生代,华力西中、晚期达到最高潮。岩体以花岗岩为主,其次为闪长岩。脉岩发育,种类多样,分布广,单脉规模小。形成时代有加里东和华力西两期,以华力西 Great Shui - Hongliuhe area is located in the eastern Tianshan Mountains, west of the Dashui Rock, east of Hongliuhe Duguizi wells. In the Beishan Paleozoic rift trough in the Tarim ancient land in the Tarim plate, the Muzhart-Hongliuhe plate suture is located in the north. Proterozoic Proterozoic, Paleozoic and Cenozoic. Invasive rocks more development, frequent and other characteristics. Magmatic activity began in the early Paleozoic, Variscan, late to reach the climax. The main granite is granite, followed by diorite. Artefact development, species diversity, wide distribution, single-pulse size small. The formation of Caledon and Variscan period two times to Varis