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浙闽地区地处太平洋构造火山带外带。通过对该区实地调查并与土耳其、美洲西部，尤其是安第斯山脉产硼区对比研究，认为二者在板块构造位置、构造盆地、深大断裂、火山岩岩石学、成矿期及古纬度古气候等方面具有不同程度的可比性。中生代板块运动与浙闽地区火山构造岩浆活动和成硼作用密切相关。浙闽地区某些晚侏罗－早白垩世喷发沉积相发育的火山盆地及火山洼地中膏盐发育，并有碳酸岩夹层的泥质岩、凝灰岩的硼异常区有找到火山沉积型硼矿的可能性。
Zhejiang and Fujian is located in the Pacific tectonic volcanic belt. Through the field investigation and comparison with the boron production areas in Turkey, the western America, especially in the Andes, it is considered that the two are in the position of plate tectonics, structural basins, deep faults, volcanic petrology, mineralization and paleoclimate paleoclimate Etc. have different degrees of comparability. The Mesozoic plate movement is closely related to the volcanic-tectonic-magmatic activity and boron formation in Zhejiang-Fujian region. Some late Jurassic-Early Cretaceous eruption-sedimentary facies volcanic basins and volcanic depressions in Zhejiang-Fujian area developed mudstone with carbonate intercalations, and the anomalous boron in tuffs found volcanic-sedimentary boron Mine possibilities.