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侵蚀基准面的英文

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"侵蚀基准面"怎么读用"侵蚀基准面"造句

英文翻译手机手机版

  • base level of corrosion
  • base level of erosion
  • baseleveloferosion
  • datum level of erosion
  • erosion datum

例句与用法

  • Planation is a combination of external agents . erosion is the primary significance in that it cuts all the strata formed previously and in the combination with transportation and accumulation , directly affects the formation of planation surface
    夷平作用是以侵蚀为先导,辅以搬运、堆积、伴随有地形的蚀低蚀退,以接近侵蚀基准面为目标的一种外力组合。
  • According to geologic basement , it can be divided into stable - floor planation surface and active - floor planation surface . according to climate zone , it can be divided into pediment and pediplain , double leveling surfaces and etchplain , peneplain and cryoplain
    夷平面理论研究与初步模拟? ?中文摘要影响夷平面形成的主要因素有前期大地构造、侵蚀基准面、气候、岩性、时间和后期构造运动等。
  • ( 5 ) by analyzing the terrace in the lacustrine sediment of the ancient barrier lake , diexi , minjiang river , forming of the terrace is not only because of the intermittent arising of the tectonic movement , but also because of descend of the eroding normal covering resulting from destroying of the barrier lake
    ( 5 )通过对岷江叠溪古堰塞湖湖相沉积中的河流阶地分析可知,阶地的形成不仅仅是由于新构造运动的间歇性抬升作用,由于堰塞湖的溃决引起洪水下泄,导致河流侵蚀基准面的下降也可以形成阶地。
  • Planation surface is a wide - ranging and undulating surface formed by planation in a long and relative stable period or in a decreacing - development period . it is near the base level and there always exists some deposits such as crust of weathering above it . planation surface is often uplifted or buried by the later tectonic activities
    夷平面是在长期的地壳相对稳定时期或地壳下降发展阶段,由广泛的夷平作用以截断面形式横切所有先成的地层和构造的接近侵蚀基准面的平缓的地表形态,其上常有风化壳等碎屑堆积,常遭到后期的抬升切割或埋藏,分布于地球的各纬度带。
  • We strengthen the investigation of natural factors such as pre - construction , erosion base level , climate , lithology , time and tectonic activities , which affect formation and preservation of planation surface . pre - constrction affects the time and degree of the planation . erosion base level is the base line for it
    前期大地构造影响夷平面发育的时间和程度;侵蚀基准面是夷平面发育的“终点站” ;气候直接和间接作用于夷平面的形成与保存;岩性影响夷平面形成的过程和时间;时间作用于夷平面发育和保存的程度;后期构造不利于夷平面的保存。
  • According to whether there are later tectonic activities or not it can be divided into mountain planation surface , lower planation surface and buried planation surface . according to active condition , it can be divided into active surface , dormant surface , exotic surface and defunct surface . taking the base level into consideration , it can be divided into sea - eroded and deposited planation surface , denudated planation surface , snowline planation surface and upper eroded planation surface
    依据夷平面形成后是否遭到后期构造变动将夷平面分为山地夷平面、原地夷平面和埋藏夷平面;依据夷平面的活动状态可分为活动面、休眠面、外来面和废止面;依据侵蚀基准面可分为海蚀-堆积夷平面、剥蚀夷平面、雪线夷平面和上部剥蚀夷平面;依据基底可分为稳定地带上的夷平面和活动地带上的夷平面;依据气候带可分为准平原、山麓面和联合山麓面、双层水平面和刻蚀平原、冻融山足面和冻融剥夷平原。
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