- 更多网络例句与逆坡相关的网络例句 [注：此内容来源于网络，仅供参考]
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Terrain shadow causes cooling to begin in basin before sunset. Radiative cooling and cold downslope wind development are two basic reasons for the formation of cold air lake and inversion in the basin.
地形遮蔽的影响使日落之前盆地中的冷却过程即已开始，地表辐射冷却及坡面冷迳流的发展是夜间冷湖和逆温形成的根本原因。
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The large altitude difference of the hypsography, the fragmental topography, the difference of exposure and the valley cause the difference of the part climate which make the orographic rain , the topography wind and the temperature inversion.
由于地势高差悬殊、地形破碎和坡向、谷向的不同，常引起局部气候差异，多地形雨、地形风和逆温现象，形成不同的小气候。
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The reverse fault occurring the slope break area of primary fault was formed as a result of inversion of normal fault in extension; c.
主控断层坡折带处的逆断层是在伸展作用下由正断层倒转形成的；c。
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There are three features in the minibasins induced by gravitational sliding on the slope: the firstly, feature is surface of unconformity developed by onlap on minibasin margins or surface of unconformity truncated by mass transport-complex are sequence boundary in the study area; the secondly , accommodation of gravity flow is controlled by up lift rate and sedimentation rate , and styles of filling in the minibasins are dominated by the interrelationship between the two factors; and the third , there are two stacking patterns that consists of upward of turbidite fan-hemipelagic drape mud or mass-transport complexes-turbidite fan-hemipelagic drape mud.
认为在深水陆坡重力滑动作用所形成的微盆地内，层序边界表现为微盆地边缘上超不整合面或重力流对下伏地层的侵蚀不整合；逆冲构造隆升速率与沉积速率共同控制了重力流可容空间和沉积充填样式；沉积垂向演化以块状搬运复合体一浊积扇－深海披覆泥或浊积扇－深海披覆泥为特征。
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This finding is of great significance not only to the reconstruction of paleoceanography, paleoenvironment, paleotectonics, and paleoclimate, but also to deepwater petroleum exploration in the South China Sea.
根据最新的地震资料分析发现，该牵引体实际上由一系列逆陆坡向上倾方向迁移的沉积物波组成，这一发现对于南海北部大陆边缘古海洋、古环境和古气候研究，以及南海深水油气勘探具有重要意义。
- 更多网络解释与逆坡相关的网络解释 [注：此内容来源于网络，仅供参考]
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adversary grade：逆坡
adventure 矿山企业 | adversary grade 逆坡 | adverse grade 逆坡
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aeolian soil：风积土
Adverse slope 逆坡 | Aeolian Soil 风积土 | Aerial camera 航空摄影机
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borderland slope：边缘坡
边缘逆冲断层 marginal thrust | 边缘坡 borderland slope | 边缘上冲断层 marginal upthrust
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slab：板,片
所以在地图和剖面观察上确定这些一级喜马拉雅构造之间的关系是非常关键的.中喜马拉雅出露的平面模式表明,MCT具有断坪-断坡的逆断层的几何特征.南部的逆冲断坪携带了一个GHC的板片(Slab)叠置在小喜马拉雅层序之上(LHS),
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back thrusting：反向逆冲作用,背向逆冲断层作用,倒向逆冲断层作用
后坡 back slope | 反向逆冲作用,背向逆冲断层作用,倒向逆冲断层作用 back thrusting | 回流 back wash