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辽宁省营口东部是我国白硼矿床重要产区之一。白硼矿床赋存在早元古宙辽东裂谷带内。辽河群里尔峪岩组，黑云变粒岩、电气变粒岩夹含硼镁橄岩为含硼岩系。东西向、北西向断裂带为储矿构造，辽河期复式深成黑云母二长花岗岩为其成矿母岩 (热源体 )。蛇纹石化大理岩、蛇纹石化镁橄岩是重要的含硼蚀变岩带及找矿标志。
The eastern part of Yingkou in Liaoning Province is one of the important producing areas of China’s Bai-boron deposit. White boron deposits occur in the early Proterozoic Liaodong rift zone. Liaohe Group Liluyu Group, biotite granulite, electrical grained rock folder containing brimasite for boron-bearing rock series. The east-west and north-west fault zones are of ore-hosting structure. The Liaohe syncroic biotite monzogranite is the metallogenic parent rock (heat source body). Serpentinized marble and serpentinized mafic rocks are important boron-bearing altered rocks and ore prospecting markers.