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本文通过对５１２、５１１矿床及其它矿点的铀源、地质构造、含矿主岩岩性、古气候、层间氧化带发育条件、成矿水文地质条件等方面的研究，提出了伊犁盆地层间氧化带砂岩型铀矿的成矿模式。
Based on the study of uranium source, geological structure, host rock lithology, palaeoclimate, developmental conditions of interlayer oxidation zone and hydrogeological conditions in the 512,511 deposits and other ore deposits, METALLOGENIC MODEL OF INTER-OXIDATIVE SANDSTONE-TYPE URANIUM DEPOSITS.