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Paleo-environmental evolution of early Paleogene in the Sanshui Basin indicated from factor analysis of main elements

机译:Sanshui盆地早期古古古古和的古环境演变,表明了主要元素的因子分析

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In this paper, factor analysis are used to study the early Paleogene paleo-environmental evolution from the Sanshui Basin, and main conclusions can be obtained as follows: stage I (89.0-73.0 m), relatively dry and relatively low temperatures; stage II (73.0-52.5 m), warm and humidity of the climate and environment; stage III (52.5-22.5 m), the ancient climate conditions change quickly, showing the alternating warm and humidity and dry; stage IV (22.5-0 m), prevailing warm and moist climatic conditions.
机译:在本文中,使用因子分析来研究Sanshui盆地的古古古环境演化,可以如下获得主要结论:阶段I(89.0-73.0 m),相对干燥且相对较低的温度;第II阶段(73.0-52.5米),气候和环境的温暖和湿度;第三阶段(52.5-22.5米),古老的气候条件迅速变化,显示出交替的温暖和湿度和干燥;第四阶段(22.5-0米),盛行温暖和潮湿的气候条件。

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