1) faults of the Taihang moutain front
太行山山前断裂带
2) Taihang mountain-front fault
太行山山前断裂
1.
The southwestern system of the Taihang mountain-front fault includes Shijiazhuang city and its adjacent area,which is located in the southwestern Capital Circle and in the cross area between Taihang Uplift and North China Basin,the geological structure is complicated in the area.
根据太行山山前断裂西南端,包括石家庄及其周边地区的位于太行隆起与华北盆地两大地质构造单元交汇处的构造环境复杂情况。
3) Taihang piedmont fault depression belt
太行山前断陷带
1.
A carbon dioxide gas reservoir containing methane and high yield geothermal mineral spring resources were found in well Here 2 located at Hebishi gravity high in Tangying Depression of Taihang piedmont fault depression belt,thus causing people to have a new understanding about the geological structure and mineral resources in this region.
在太行山前断陷带汤阴断陷鹤壁市重力高上钻探的鹤热 2井发现了含甲烷的二氧化碳气藏和高产的地热矿泉水资源 ,从而使我们对该区的地质结构和矿产资源有了新认识。
4) Southern marginal fault zone of Taihangshan Mountains
太行山南缘断裂带
5) Taiyangshan fault zone
太阳山断裂带
6) ancient Taihangshan fault
古太行山断裂
补充资料：断裂带
亦称“断层带”。有主断层面及其两侧破碎岩块以及若干次级断层或破裂面组成的地带。在靠近主断层面附近发育有构造岩，以主断层面附近为轴线向两侧扩散，一般依次出现断层泥或糜棱岩、断层角砾岩、碎裂岩等，再向外即过渡为断层带以外的完整岩石。断层带的宽度以及带内岩石的破碎程度，决定于断层的规模、活动历史、活动方式和力学性质，从几米至几百米甚至上千米不等。一般压性活压扭性断层带比单纯剪切性质的断层带宽。在一些大型的断层带中，由于被后期不同方向的断层切错，和夹有一些未破碎的大型岩块，只是断层带的结构趋于复杂化，从而在近代的断层活动中容易形成运动的阻抗，是应力易于积累和发生地震的场所。
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