peneplanation
- peneplanation的基本解释
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准平原作用
- 更多网络例句与peneplanation相关的网络例句 [注：此内容来源于网络，仅供参考]
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Finally, we conclude that the factors controlling the geomorphic characteristic of low relief in our study area is rock types, sedimentation, weathering and high-altitude peneplanation.
此外，研究区内的条带分析和地层年代划分表明控制研究区低坡度、低起伏地形特征的因素为：岩石的岩性、沉积作用、侵蚀作用及高山夷平面。
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But there are no many tectonic events during this period. From middle Miocene to late Miocene there is a stage of peneplanation in the South China Sea and there are many tectonic events in this area, such as stratum unconformable contact, faults, deformation and magmatism.
而符合南海地区准平原化阶段的时代是在中中新世末至晚中新世(N21/N31)之间，在此时段普遍存在区域构造不整合接触和地层缺失、断裂、变形及火山活动等构造变动事件。
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Level of vast lakes had been base surface for incision in Early Miocene from (24.1±0.6)Ma to(14.5±0.5) Ma, and lakes and top lacustrine deposits of Wudaoliang Group became base surface for erosion and peneplanation since Late Miocene, which formed planation surface or peneplain of the Tibetan Plateau.
中新世早期(24.1±0.6~(14.5±0.5Ma)以古大湖的湖面为侵蚀基准面，经过隆起区剥蚀夷平和长期湖相沉积，在高海拔环境下形成早期夷平面。
- 更多网络解释与peneplanation相关的网络解释 [注：此内容来源于网络，仅供参考]
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peneplanation：准平原酌
peneplain 准平原 | peneplanation 准平原酌 | penetrability 贯穿性
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peneplanation：准平原作用
peneplainpeneplane 准平原 | peneplanation 准平原作用 | penetrability 透彻性
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peneplanation：准平原化作用
准平原|peneplain | 准平原化作用|peneplanation | 准同生作用|penesyndiagenesis, penecontemporaneous diagenesis
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peneplanation：准平原作用;蚀原作用
准同时变形 penecontemporaneous deformation | 准平原作用;蚀原作用 peneplanation | 准平原 peneplane