1) convergence strike slipping
会聚走滑
2) dextral convergent strike slip
汇聚型右行走滑
1.
When the Cenozoic tectonic system forming, the S N tectonic system joined in it, and the S N faults were re activated by forming S N dextral convergent strike slip faults zones and transformation zones.
第三纪近南北向断裂活动以汇聚型右行走滑方式为主 ,形成近南北向走滑构造和近南北向构造变换带 ,作为深部边界约束条件而影响着第三系变形。
3) strike-slip
走滑
1.
Dextral strike-slip evidence on seismic slice for Tanlu strike-slip fault
郯庐走滑断层右旋走滑的地震切片证据
2.
On the basis of geological model with older tensile deformation under continental rift and younger dextral strike-slip movement in the Liaohe Depression, Paleogene, modeling experiments with formation and evolution of fracture system on the seismic line 34.
按辽河坳陷古近纪经历过早期大陆裂谷拉张变形和后期右行走滑变形的地质模型,对其东部凹陷34。
3.
Basins related to strike-slip faults are relatively complex,and mainly controlled by the property and evolution of boundary faults.
与走滑有关的盆地一般比较复杂 ,其形成和演化主要取决于边界断裂的性质和活动演化历史。
4) slip away; disappear
滑走;滑落
5) strike-slip fault
走滑断层
1.
Discovery of strike-slip fault and its origin analysis in Biyang depression of Xinzhuang oilfield;
泌阳凹陷新庄油田走滑断层的发现及成因分析
2.
Relationship between strike-slip faults and petroleum in the central segment of the eastern subbasin of the Liaohe oilfield,China;
辽河油田东部凹陷中段走滑断层与油气的关系
3.
Relation between features of strike-slip faults and hydrocarbon accumulation in Subei basin;
苏北盆地走滑断层特征与油气聚集关系
6) Strike-slip structure
走滑构造
1.
Characteristics of strike-slip structure and rules of hydrocarbon accumulation in northern Liaodong Bay;
辽东湾北部地区走滑构造特征与油气富集规律
2.
The geometry (type, classification, assemblage) , forming period-times and genesis mechanism of the strike-slip structures in the eastern Jiyang Depression have been researched in this paper using structural analytic method to gain more knowledge of the strike-slip structures.
为了提高走滑构造的研究程度,将济阳坳陷东部作为一个整体,应用构造解析方法,研究其走滑构造的形态、分类、组合形式及形成期次并探讨了其成因机制。
3.
The weaknesses, difficulties and key points of the present study of basin tectonic dynamics are shown in the following four aspects: (1)Tectonics with complex features and complex cause of formation, such as strike-slip structure, lateral trans.
目前盆地构造动力学研究的弱点、难点及重点主要有以下4方面:(1)特征或成因复杂的构造,如走滑构造、横向(转换)构造、拆离滑覆构造、较大型断层的分段性和断裂带的结构等。
补充资料：走胡走越
成语：走胡走越
【解释】： 汉高祖 欲拿 项羽 旧将 季布 ， 朱家 因 汝阴侯 滕公 劝 高祖 曰：“臣各爲其主用， 季布 爲 项籍 用，职耳。 项氏 臣可尽诛邪？今上始得天下，独以己之私怨求一人，何示天下之不广也！且以 季布 之贤而 汉 求之急如此，此不北走 胡 即南走 越 耳。夫忌壮士以资敌国，此 伍子胥 所以鞭 荆平王 之墓也。君何不从容爲上言邪？”见《史记·季布栾布列传》。后因以“走胡走越”谓智能之士被迫逃亡，而为敌国所用。 梁启超 《论中国学术思想变迁之大势》第三章第一节：“衰 周 之际，兼并最烈，时君之求人才，载飢载渴，又不徒奬励本国之才而已，且专吸他国者而利用之。盖得之则可以爲雄，失之且恐其走 胡 走 越 ，以爲吾患也。”
汉高祖欲拿项羽旧将季布，硃家因汝阴侯滕公劝高祖曰：“臣 各为其主用，季布为项籍用，职耳。项氏臣可尽诛邪？今上始得天下，独以己之私怨求一人，何示天下之不广也！且以季布之贤而汉求之急如此，此不北走胡即南走越耳。夫忌壮士以资敌国，此伍子胥所以鞭荆平王之墓也。君何不从容为上言邪？”见《史记·季布栾布列传》。后因以“走胡走越”谓智能之士被迫逃亡，而为敌国所用。
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