1) the western Qiulitage tectonic belt
西秋里塔格构造带
1.
To analyze the tectonic evolution characteristics of the western Qiulitage tectonic belt in Mesozoic-Cenozoic,two profiles across the western Qiulitage tectonic belt are restored according to balanced section theory,and BasinMod-1D software of PRA company is used to analyze subsidence history of two wells which are in the western Qiulitage tectonic belt.
根据平衡剖面原理,对经过西秋里塔格构造带的2条地质剖面进行构造复原,利用PRA公司的BasinMod-1D软件对其中的2口井做沉降史分析,结果表明中、新生代的构造演化特征为三叠纪末期发生构造抬升形成古隆起构造,之后的侏罗纪未发生构造沉降,一直处于沉积间断状态,白垩纪早中期发生构造沉降,白垩纪末期库车拗陷整体发生抬升剥蚀,古近纪库姆格列木群沉积期的喜马拉雅早期构造运动强度较弱,苏维依组-康村组沉积期的喜马拉雅中期构造运动强度逐渐增大,到库车组沉积期-第四纪的喜马拉雅晚期构造活动最强烈。
2) Qiulitage structural belt
秋里塔格构造带
1.
Segmentation of oil and gas accumulation in Qiulitage structural belt and its forming mechanism;
秋里塔格构造带油气聚集分段性及成因机制
3) The Qiulitage structural belt
秋里塔格构造带
1.
The Qiulitage structural belt situated in the front of the Kuqa fold-and-thrust belt,with a regional structural position being sandwiched in between the generating-drainage center of the Triassic-Jurassic source rocks in the Kuqa Depression and the front belt of the North Tarim Rise.
秋里塔格构造带位于库车前陆逆冲带前锋 ,区域构造位置介于库车坳陷三叠 侏罗系烃源岩生排烃中心与塔北前缘隆起带之间 ,第三系广泛分布两套膏盐岩层 ,发育多套储盖组合和复杂的构造样式 ,石油地质条件非常优越。
4) The eastern Qiultag structural belt
东秋里塔格构造带
1.
The eastern Qiultag structural belt,which was on the southern edge of Kuqa foreland basin,has occurred tense tectonic compression and subsidence during Cenozoic.
东秋里塔格构造带位于库车前陆盆地的南缘,新生代经历了强烈的构造挤压和构造沉降。
5) Qiulitag anticline zone
秋里塔格褶皱带
1.
Properties of geometry and kinematics related to hydrocarbon traps in Qiulitag anticline zone of Kuqa Depression;
库车坳陷秋里塔格褶皱带几何学和运动学特征与油气圈闭
补充资料：西香格里
西香格里向北延伸至扬子江（金沙江）畔，并与阿喜里接壤，包括了丽江雪山以西的扬子江（金沙江）河谷。最北端的村庄就坐落在通往石鼓的马路边上，也就是沙坝。沙坝以东叫冷水沟，正好处在阿喜与香格里的交界处，冷水沟往西就是箐口塘，往南而不在扬子江河谷范围的其他地方为雄古（纳西语为许古），鲁瓦和竹彼。岔路口（一条由鹤庆通向石鼓，而另一条则从剑川通往丽江）以北，位于高原顶部的地区，普遍称之为落水洞，仍属香格里的地界，落水洞向岔路口以南延伸直至剑川的边界，最南的村庄则是螳螂坝，香格里南部的其它村庄包括律比山、天红、沐海坪以及甸尾。
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