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1981年碳酸盐研究有无重大突破,时间将作出回答。诚然,有一些振奋人心的进展。这些进展许多是由于研究方向的改变或侧重点与以往不同所取得的。如果从这种眼前利益的观点采看,许多成果似乎都是由于把老方法应用于新情况,新观点应用于老问题以及所召开的那些有助于综合资料和总结当前研究现状的专题讨论会和学术报告会所致。 对于现代深水碳酸盐,尤其是它们在大陆坡和台地内盆地(如巴哈马地区)的沉积作用、沉积学特征及海相成岩作用,仍在进行大量的工作,通常采用的
There is no major breakthrough in carbonate research in 1981, the time will be answered. True, there are some encouraging developments. Much of this progress has been made due to changes in research direction or different priorities. Judging from this immediate interest, many of the results seem to stem from the application of the old method to new situations, the application of new ideas to old problems and the convening of symposiums that help to synthesize information and summarize the current state of research And academic report due. For modern deep-water carbonates, and in particular their sedimentation, sedimentology and marine diagenesis in the continental slope and intracontinental basins (eg, the Bahamas), extensive work is still underway and commonly used