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本文所要阐述的是分布在干旱大陆气候带中并产在为古生代山脉所环绕的新第三纪陆相沉积洼地中的铀矿床。矿层的形成是由于铀的原始同生堆积和在成岩作用、后生作用阶段以及地表附近风化条件下铀在岩层中后来重新分布的结果。
What this article describes is uranium deposits distributed in the arid continental climate zone and deposited in the Neogene terrigenous depressions surrounding the Paleozoic range. The formation of the mine is due to the original symbiosis of uranium and the subsequent redistribution of uranium in the rock under the diagenesis, metaphysics and weathering conditions near the surface.