1) the Yumushan nappe
榆木山推覆片体
2) napping sheets
推覆片体
3) Yumushan
榆木山
1.
Gaotai railway station fault, as a part of northern faults of the Yumushan uplift being a second-order uplift in Hexi Corridor, situated about 6km northern from the northern Yumushan fault, which is related to the Yumushan uplift and actives newer than the northern Yumushan fault.
高台车站断裂属于河西走廊内次级隆起——榆木山隆起北侧断裂系的组成部分,它位于榆木山北缘断裂北侧6km、是与榆木山隆起有成生联系、活动时间比北缘断裂更新的现代活动断裂。
2.
The Yumushan Eastern Marginal Fault Zone Lies the west margin of the ZhangyeMinle basin and in the central part of the Hexi corridor.
位于甘肃河西走廊中部、张掖——民乐盆地西侧的榆木山东麓断裂带,是一条走向北北西向晚第四纪活动断裂。
4) nappe-type section of mountain front formation
山前构造推覆体
1.
If the main rock is hard granite when penetrated into nappe-type section of mountain front formation,it's often to take place down hole accidents such as drill string breaking and drill bit wearing very quickly.
在钻井中,钻遇山前构造推覆体段以花岗岩为主的岩石时,极易发生钻具断损及钻头磨损加剧的情况。
5) Wudang Mountains nappe
武当山推覆体
6) fold orogeny
推覆造山
1.
In the early Mesozoic, it began to enter into inner continental orogenic stage and changed from fold orogeny in the early stage to nappe.
由早期的褶皱造山进而转化为推覆造山。
补充资料：榆木疙瘩
1.见"榆木圪垯"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条