1) Gubeikou fault
古北口断层
1.
The sedimentation of Tuchengzi Formation was mainly preserved in Chengde syncline and in the south part of Gubeikou fault in Chengde area, namely Chengde basin and Gubeikou basin, respectively.
承德地区土城子组的沉积地层,主要保存在两个地区,一处为承德向斜,另一处为古北口断层的南部紧邻断层地区,即分别命名的承德盆地和古北口盆地内。
2) Gubeikou
古北口
1.
Application Analysis of Water Quality and Quantity Automatic Monitoring System in Gubeikou Hydrological Station;
古北口水文站水质水量自动监测系统的应用分析
2.
Gubeikou thrust nappe structure and brittle-ductile deformation belt of the Tuchengze Formation;
古北口逆冲推覆构造及土城子组脆韧性变形带特征
3.
The changing trend on water quality of Chaohe Gubeikou provincial section,which is an important Miyun Reservoir's tributary,was discussed and analyzed.
依据水质自动监测系统数据,对密云水库重要入库支流-潮河古北口省界断面水质变化趋势、水质特性等进行了详细讨论与分析。
3) Chengbei fault
埕北断层
1.
Based on juncture re_processing and interpretation of high_quality 3D seismic data, some new knowledge has been obtained for the southern Chengbei fault in the Chengdao area, that is, a new branch fault is found south of the old fault.
通过对高品质三维地震资料的重新连片处理解释 ,对埕岛油田埕北断层南段部分取得了新的解释结果 ,即在老断层以南又发现一条新的分支断层。
4) Beichuan fault
北川断层
1.
The Beichuan fault plays an important role in the formation and evolution of Longmenshan thrust zone and Western Sichuan foreland basin, it causes difference between hanging side and heading side of the fault.
龙门山是典型的逆冲断层发育带，北川断层是龙门山逆冲断层系中的主干断层。
5) the NE trend faults
北东向断层
1.
Appalying the new theory of structural geology, the article focuses on the genesis of the NE trend faulrs and turns out the results that the NE trend faults were formed by expanding gradually because of having been multiply forced.
文中运用构造地质学新理论来研究青岛地区北东向断层的成因。
6) lamellar fracture
层状断口
补充资料：古北口
| 古北口 中国长城上关口之一，北京与东北地区往来的咽喉要道。位于北京市密云县东北部。555年，居庸关至山海关长城从此修过，古北口与长城相接。1403年朱棣称帝后迁都北京，为加强北京防务，大修长城。尤其是首都北京从居庸关到山海关这一段500多千米的长城修得特别坚固。西北居庸关，东北古北口成为明王朝首都的两个重要门户。古北口与居庸关东西对峙，是华北平原通往内蒙古高原的要道，自古称为雄险，有“地扼襟喉趋朔漠，天留锁钥枕雄关”之称。古北口的关城，跨于两山之上，建于明洪武十一年(1378)，并设有守御千户所。 |
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参考词条