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moutonnee相关的网络例句

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与 moutonnee 相关的网络例句 [注:此内容来源于网络,仅供参考]

The distributive laws of roche moutonnee and whaleback form is controled by icetemperature and dynamic process at glacial bottom.

羊背石和鲸背岩的分布规律是受底部冰温和动力过程控制的。

In addition, the specific position of roche moutonnee is related with the local climate, structure and relationship between the primary trough and tributaory trough.

此外,羊背石分布的具体地点还与局部气候、构造以及主支谷之间的关系相关。

According to the uplift rate of 0.133-0.4 cm/a, the old moraine was formed in 610±50 ka, the glacial rock surface was formed in 140±9 ka and the roche moutonnee was formed in 18.6±0.2 ka.

由于终碛垄是冰盛期结束时遗留下来的,而冰川擦痕面是冰期结束过程中暴露出来的,因此不同冰川地貌面反映的冰期中的冰川事件是不同的。

On the contrary, some positions of roche moutonnee are not at the pressure-melt point, and the temperature of ice-base has cold and temperate alternately. They belong to the pluck-abrasion zone.

形成羊背石的部位与之相反,一些地方没有达到压力融点,冰底温度有冷、温的变替,是拔蚀-磨蚀作用带。

According to the idea of uplift early, it can be calculated that the old moraine was formed in 459.42 ka BP, the glacial rock surface was formed in 122.5 ka BP and the roche moutonnee was formed in 18.3 ka BP.

根据80万年来的阶段性的隆升速率介于0.133 cm/a – 0.4 cm/a之间,计算出老终碛垄的形成年代为564.96 ka-656.27 ka,取值为610±50 ka;冰蚀基岩面的形成年代为130.85 ka-149.37 ka,取值为140±9 ka;羊背石的形成年代为18.494 ka-18.790 ka,取值为18.6±0.2 ka。

The glacial rock surface on the independent hill near Laolinkou Daoban was formed in MIS6. The roche moutonnee in the north of Mountain Tuershang was formed in MIS2. Normally , the distance glacial reached is further and the height of glacial is bigger, the scale of ice age is bigger.

根据三组样品所反映的三次冰期来看,形成于倒数第三次冰期的老终垄的保存,以及形成于倒数第二次冰期的冰川擦痕面的存在,说明最近三次冰期的规模由大到小依次为倒数第三次冰期、倒数第二次冰期和末次冰期。

The distribution of glacial-erosion traces on the roche moutonnee has fair regularity, that is to say the long-straight striations were often formed on the top of stoss side and the crescentic scars, crescentic wedges, chatter marks and shorted striations on the end of stoss side and striation of many groups on the flanks, which can show the condition of glacial division-flow.

迎冰面的顶部为长度大且平直的擦痕,尾部为新月型裂纹,新月型凿口,颤痕和较短的擦痕;侧部常有多组擦痕,它可指示冰川分流的情况。

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