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在过去二十年间,古气候学家已经充分证明了如下结论:对气候反映灵敏的沉积物的分布可能与大致平行于纬度的现气候带有关.例如:煤沉积在与现代雨带一致的古纬度区,沉积在现代赤道带和大约南、北纬55度地带内,它表明这些地带曾在地质历史中出现过.由此可推断,尽管一些气候参数有许多明显的不同,例如从赤道到极区的温度梯度,但古代的大气环流同现代的情形基本相同.然而,纬度分带的模式并不完全适用于预测对气候反映灵敏的沉积物的分布.与现代相比较,尽管古代的总的大气环流不会有根本的不同,但是,由于古、今地理的差别,使两者在某些方面仍有不同.因此,笔者制作了比较切合实际的降雨量分布图,这种图件是依据大气环流图产生的,而大气环流已被人们成功地用于预测某些生油层和磷灰岩矿床的分布.我们对预测的降雨量的分布与煤、蒸发岩的分布所分的七个时期逐一进行了比较.笔者发现对古地理把季风环流增大到最大限度的时期,用大气环流一降雨量图测蒸发岩和煤的分布比用纬度分带模式图更为成功.季风环流能十分有效地破坏总的纬度分带形式.对季风环流作用并不重要的时期,用纬度分带模式就足以能够预测这些岩石的分布了.
For the past two decades, palaeoclimate scientists have demonstrated the following conclusions: The distribution of climate-sensitive sediments may be related to the present climate roughly parallel to latitudes, for example, coal deposition in ancient Latitudes, deposited in the modern equatorial zone and about 55 degrees south and north latitude, which indicate that these areas had occurred in geological history, concluded that although there are many significant differences in some climatic parameters, such as from the equator to the extreme However, the pattern of latitudinal zonation is not entirely suitable for predicting the distribution of sediments that are sensitive to climate reflections.Compared with modern times, although the ancient total The general circulation of the atmosphere will not be fundamentally different, but due to the difference between ancient and modern geography, there are still some differences between the two. Therefore, the author has made a more realistic rainfall distribution map, which is based on Atmospheric circulation maps have been developed, and the general circulation has been successfully used to predict the distribution of some oil-bearing formations and apatite deposits. Our distribution of predicted rainfall is consistent with that of coal, evaporite The seven periods that were divided by cloth were compared one by one.The author finds that the distribution of evaporite and coal is more accurate than the latitudinal zonation pattern by using the atmospheric circulation and rainfall in the period when the paleogeography increased the monsoon circulation to the maximum As a success, the monsoon circulation can very effectively destroy the overall latitudinal zoning, which is sufficient to be able to predict the distribution of these rocks during periods where the monsoon circulation is not important.