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新疆东准噶尔地区乌伦布拉克铜矿、老山口铜—铁—金矿两地皆存在花岗质岩浆隐蔽爆破作用。前者形成了与潜火山英安玢岩侵入体密切伴生的英安玢岩质隐爆角砾岩,后者形成了与潜火山闪长玢岩侵入体相伴生的闪长玢岩质隐爆角砾岩和闪斜煌斑岩质隐爆角砾岩。岩浆隐蔽爆破作用是伴随该区华力西中晚期—晚期地槽褶皱造山运动而发生的一种超浅成岩浆作用,其与铜、金等金属成矿的关系密切;与其有关形成了隐爆角砾岩筒型铜(金)矿和破碎带蚀变岩型金矿。两种类型的矿床都显示出广阔的找矿前景。
In the eastern Uzbekistan copper deposit and the Laoshankou copper-iron-gold mine, the concealed blasting of granitic magmas exists in both East and West Xinjiang. The former forms the Yingan igneous rock cryptoexplosion breccia which is closely associated with the volcanic intrusive volcanic intrusive rocks, and the latter forms the dioritic rock cryptoexplosion angle with the volcanic diorite intrusive volcano Conglomerate and flash lamprophyre cryptoexplosive breccia. The magmatic concealed blasting is an ultra-magmatic magmatism that occurs along with the late-late geosynclinal fold orogeny in the area, which is closely related to the metallogenic processes of copper, gold and other metals. Breccia barrel copper (gold) ore and crustal alteration rock type gold deposit. Both types of deposits show broad prospects for prospecting.