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1981年的12个月中,有关蒸发岩及其构造环境,蒸发岩与其他沉积物,以及与烃聚集的关系的论文和著作的数量有了很大的增加。由于这些工作的结果,现在从其地层记录看来,已经包括大量形成于蒸发阶段(一部分为海相而另一部分为非海相成因)的沉积物。西伯利亚地质与地球物理部的Michall Zharkov撰写的《古生代盐类聚集历史》一书,着重讨论了整个古生代约350百万年间的蒸发岩聚积体的范围。进而,他把所有这些沉积物的地理位置放在板块构造和“最固定的”环境中加以比较。在关于板块构造的几个讨
In the 12 months of 1981, there has been a dramatic increase in the number of papers and writings on evaporites and their tectonic setting, evaporites and other sediments, and their relationship to hydrocarbon accumulation. As a result of these efforts, it now appears from its stratigraphic records that a large number of sediments have been formed in the evaporation phase (one part of which is marine and the other part of which is non-marine). The Paleozoic Salt Aggregation History, by Michall Zharkov, Department of Geology and Geophysics, Siberian, focuses on the range of evaporite aggregates over about 350 million years of Paleozoic. In turn, he compares the location of all these sediments to the plate tectonics and the “most stationary” environment. Several discussion on the plate structure