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超大型矿床的出现、形成与其所在的地质背景有关。在全新构造观的指导下论证了大型－超大型硼矿床形成时的构造环境及其它基本特点，把矿床的成生与地壳演化结合起来，并重视了深断裂对成矿的控制作用。通过幔壳长期作用，使深部巨量成矿物质以三种方式带入成矿热卤水盆地，在一定的自然地理与物理化学条件下矿质沉淀、富集形成大型与超大型硼矿床。在上述成矿条件研究的基础上，建立了矿床的地质成因模式。
The emergence and formation of superlarge deposits are related to the geological background of the deposit. Under the new tectonic concept, the tectonic setting and other basic characteristics of the large-superlarge boron deposits are demonstrated. The mineralization of the deposits combined with the evolution of the crust, and the importance of the control of deep fractures to the mineralization. Through the long-term action of the mantle crust, deep massive ore-forming materials are brought into the metallogenic thermal brine basin by three ways, and the minerals are precipitated and enriched to form large and super-large boron deposits under certain natural geophysical and chemical conditions. Based on the above research on metallogenic conditions, the geologic genetic model of the deposit is established.