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本文讨论了我国各地质时代中的碳酸岩的发育、演化及其中的层控矿床。碳酸岩的时空分布具太古代和中新生代较少,元古代和古生代多;西部褶皱带少,东部陆台区多的特点。它们主要是在浅水环境下沉积的,太古代碳酸岩为化学沉积;元古代多与藻类的生命活动有关,白云岩占绝对优势;古生代及部分中生代主要是生物及生物化学沉积,灰岩多于白云岩。元古代以后,生物礁滩开始发育。
This paper discusses the development and evolution of carbonate rocks and the stratabound ore deposits in various geologic times in China. Carbonatite spatial and temporal distribution of the Archean and Mesozoic Cenozoic less, more Proterozoic and Paleozoic; western fold less, the eastern part of the land area more. They are mainly deposited in shallow water environment. Archean carbonates are chemical deposition. Proterozoic and algae are mostly related to the life activities of algae. Dolomite has the absolute advantage. Paleozoic and some Mesozoic are mainly biologic and biochemical sediments, with more limestone Dolomites. Proterozoic, bio reef beach began to develop.