late tectonic meaning in Chinese
晚构造期的
Examples
- The latest tectonic deformation at the growing point of a new fracture on the eastern tip of the altyn tagh fault
阿尔金断裂东端破裂生长点的最新构造变形 - 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。 - 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。