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最近十几年,越来越多的人注意到若干金属、非金属矿床在空间位置上和成因上与生物礁有关,在矿床研究中开始运用碳酸盐沉积学和石油地质学的一些成果.在国内,这一问题也引起了不少同志的注意. 生物礁是一个常用术语,但1950年W.H.童豪富曾引述许多人对它的解释,说明对这一概念的理解各人并不一致,并由此产生了生物丘(bioherm)、生物层(biostrome)、碳酸盐岩隆(carbonate buildup)等同义或近义的词.根据最近30年来沉积学资料,可以认为生物礁是由于造礁生物的活动形成的、原地生长的抗浪构
In the recent decade or so, more and more people have noticed that a number of metallic and non-metallic mineral deposits are spatially and genetically related to reefs. Some achievements in carbonate sedimentology and petroleum geology began to be applied in deposit studies. In China, this issue has also attracted the attention of many comrades. Reefs are a common term, but 1950’s WHR has quoted many interpretations of it, indicating that the concept of understanding is not the same for everyone, and As a result, synonymous or near-synonymous terms such as bioherm, biostrome, carbonate buildup, etc. Based on the sedimentology data over the last three decades, reefs are thought to be due to reef creatures The formation of activities, the growth of anti-wave structure