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1)  Bolokenu Aqikekuduke Fault
博阿断裂
1.
The Bolokenu Aqikekuduke Fault extends over 700km and obliquely cuts the North Tian Shan.
利用遥感资料 ,通过野外实地考察并结合气候地貌事件的分析 ,对斜切北天山、长逾70 0km的博阿断裂 (博罗科努 -阿齐克库都克断裂 )的右旋走滑运动进行了定量研究。
2)  Bogd Fault
博格德断裂
3)  Aerjin fault
阿尔金断裂
1.
Status of the research of Aerjin Fault and its control effect of petroleum;
阿尔金断裂的研究现状及其控油意义
2.
Results show that western basins and eastern basins which takes Aerjin fault as dividing line, have obvious difference in geo thermal gradient.
以阿尔金断裂为界 ,东部盆地与西部盆地地热梯度存在明显差异。
4)  Altun Fault
阿尔金断裂
1.
Adverse impact of Altun Fault s strong water delivery on nuclear disposal field of Beishan Mount;
阿尔金断裂中的地下河对北山修建核废物库的不利影响
2.
Uplift dynamics of the Qinghai-Tibet Plateau and Altun fault;
青藏高原隆升动力学与阿尔金断裂
3.
The Altun fault is an important Cenozoic strike slip fault zone in Mid Asia,which defines the northwest boundary of Qinghai Tibet Plateau and separates the Tarim and Qaidam basins.
阿尔金断裂是青藏高原的西北边界,分隔了塔里木与柴达木盆地,是新生代中亚大陆内一条重要的走滑断裂带,目前已成为中、外地学界瞩目的研究热点。
5)  Altyn Tagh Fault
阿尔金断裂
1.
Study of Distributing Pattern of the Eastern Terminal of the Altyn Tagh Fault Zones;
阿尔金断裂带东端断裂展布型式的研究
2.
Characteristics and tectonic setting of the Tula aluminous A-type granite at the south side of the Altyn Tagh fault, NW China.;
阿尔金断裂南侧吐拉铝质A型花岗岩的特征及构造环境
3.
Multi-stage strike-slip motion and uplift along the Altyn Tagh fault since the Late Cretaceous;
晚白垩世以来沿阿尔金断裂带的阶段性走滑隆升
6)  the Altyn Tagh fault
阿尔金断裂
1.
The relation between the Altyn Tagh fault and the Cenozonic basin;
阿尔金断裂与周缘新生代盆地关系
2.
It is thought that the Kuyak fault and the Altyn Tagh fault belong to the same fault, and it is first proposed that the displacement of the Kuyak fault is about 80 km.
认为库牙克断裂与阿尔金断裂为同一条断裂,并首次提出库牙克断裂的断距约80km。
3.
Based on field observations,this paper analyses sedimentary processes and deformation history of the strike slip basins developed along the central segment of the Altyn Tagh Fault zone(located between long 88°E and long 92°E) and puts forwards to geological evidences for Late Cenozoic left lateral strike slip offset along the fault zone.
通过对沿阿尔金断裂中段 (位于东经 88°至 92°)发育的晚第三纪走滑盆地沉积历史和走滑变形过程的野外观测以及对第四纪索尔库里盆地形成和演化过程的沉积环境复原的分析 ,提出了阿尔金断裂中段晚新生代左旋走滑位错的地质新证据。
补充资料:博阿科

尼加拉瓜中部城市,博阿科省首府。位于中央高原西侧,南距尼加拉瓜湖40公里。海拔388米。人口2.2万(1978)。内地农牧区的贸易和加工中心。工业以乳制品和畜产品加工为主,另有锯木业,并生产肥皂、砖瓦、矿泉水、巴拿马草帽等。有公路通马那瓜。

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