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glacial period相关的网络例句

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与 glacial period 相关的网络例句 [注:此内容来源于网络,仅供参考]

Last Glacial is a crucial period for exploring the climatic mechanisms.

末次冰期是探索气候变化机制极为关键时段。

That's just before the last glacial maximum---a period when there was a sudden drop in temperature and glaciers advanced.

那是在最后一个最大冰川作用时代——那时气温突然降低而冰河上升。

Composed of glacial ice is a longer period of time pressed through the snow, freezing, re-crystallization process of the formation of a series of ice the lower body has a certain plasticity, in its own pressure and gravity Next, along the valley slope or flow slowly, thus the formation of a glacier.

组成冰川的冰体是由积雪经较长时间的压紧、冻结、重新结晶等一系列过程形成的,冰体的下部具有一定的可塑性,在其自身的压力和重力作用下,沿斜坡或谷地缓慢地流动,这样就形成了冰川。

This is not surprising, given the closer proximity of Pengyang to the Asian inland dust sources; The average content of calcium carbonateis of Pengyang section is not only higher than that of central loess plateau, but also higher the west of Chinese Loess Plateau, which reflected Pengyang loess had been deposited by near Liupanshan\'s substances that contained more calcium carbonateis; The content of diffluent element of 10m depth in the section increased fast, which indicated that the modern eluviation and the leaching depth of loess may be stronger than our guess; The soil growth index can reflect the intensity of soil forming and the climatic changes; The "abrupt chang" of glacial and interglacial period was caused by strong soil-forming processes that enlarged the discrepancy of granularity between loess and paleosol. However, the magnetic susceptibility nearly cannot reflect the existence of S_8 and the magnetic susceptibility of S_7 is highest in the whole section, which is inconsistent with other studies that S_5 has the highest magnetic susceptibility.Thin-section examination shows that the micro-texture of the soil layers is divided into both cementing texture in S_7, S_5 and S_1, and granular texture in all others.

与其它剖面相比,彭阳剖面粒度总体上要比东部的洛川、西安,甚至西部的兰州、新疆东湾要粗;CaCO_3平均含量不仅高于黄土高原中部,也高于高原西部,反映出本剖面富含碳酸盐的六盘山近源沉积起到了很重要的作用;易溶元素含量在剖面10m处快速升高,淀积特征明显,反映出黄土受现代淋溶成土作用影响较大,黄土直立、疏松、多孔特性和高温与多雨组合的气候特点,使得元素淋溶、淀积的强度和深度超出了传统的认识和判断;烧失量与其它指标相比,不仅能区分冰期、间冰期;而且能够区分出次一级的冰阶、间冰阶,有较高的分辨率;土壤发育指数、红度能够反映土壤强度差异,是反映气候波动的较好指标;然而,磁化率不能反映古土壤S_8的存在,且S_7的磁化率在全剖面中最高,这与大多剖面S_5磁化率最高的特点不一致。4。

; 3 younger Dryas Only has reflection in the hundred-year-scales climatic curve, it is not evident in the curve of long period; 4 in the hundred-year-scales climatic curve, the last glacial maximum fluctuation as frequuently and 18-28KaBP was the stage in which the frequency fluctuation was the largest.

;(3)新仙女木事件仅反映在百年尺度的气候曲线上,在较长周期的饿曲线上不明显;(4)在百年尺度的气候曲线中,末次冰盛期气候波动频繁,其中18-28KaBP 是频率波动的最大阶段,但随着周期尺度的加大,气候的波动频率逐渐趋于均匀。

10Be records in the Okinawa Trough sediment during the last glacial, the Younger Dryas cold period, and the Holocene show that the main part of the fluctuations in 10Be content in the sediment can be attributed to variations in the 1°Be production rate.

表层沉积物中的10Be,9Be和Pb三者表现出完全不同的分布特征。10Be的分布主要受黑潮及其支流黄海暖流所支配;10Be的分布受黄河陆源物质输入的影响,主要集中在南黄海泥质区;Pb则主要分布在长江口和琉球群岛附近,反映了人类活动的影响。

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