1) Jiangshao fracture belt
江绍断裂带
1.
The foliated dioritic rocks locating in Huangrhan - Wangpaze area, Zhuji County, the mid-dlepart of Jiangshao fracture belt,Zhejiang Province, have been studied in this peper.
本文研究了浙江江绍断裂带中段诸暨县璜山至王家宅一带片理发育的闪长质岩石。
2) Jiangshan-shaoxing fracture zone
江山-绍兴断裂带
3) Jangshan-shaoxing foulted
江-绍断裂
4) Jiangshan-Shaoxing Fault
江绍断裂
1.
Volcanic Rocks of the Pingshui Group and Plagiogranite of This Period in Jiangshan-Shaoxing Fault: Petrogenesis and Its Tectonic;
江绍断裂带平水群火山岩及伴生斜长花岗岩的成因与大地构造意义
5) Jiangshan-Shaoxing fault
江山-绍兴断裂
1.
In the case study of Jiangshan-Shaoxing fault between Jinhua and Quzhou of Zhejiang Province, this paper describes the relations between LSTF and deep large faults based on the images of the Landsat 7 ETM and thermal infrared remote sense.
在江山-绍兴断裂金衢段的实际应用中,方法以Landsat7ETM+热红外遥感影像为数据源,描述了研究区地表温度场与深大断裂带之间的关系。
6) Ganjiang fault zone
赣江断裂带
1.
On the basis of an analysis of geological and geophysical data obtained by petroleum exploration in the South Poyang depression in recent years,the authors propose that the basining and tectonic evolution of the South Poyang depression were controlled by the activities of the Ganjiang fault zone under the constraint of the Yanshanian tectonic framework.
通过对近几年南鄱阳坳陷油气勘探取得的地质、地球物理资料的分析,认为该盆地形成和构造演化是在燕山期古构造格局的限制下,受控于赣江断裂带的活动,以走滑-伸展为主要特征。
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