1) Kebai Fault
克百断裂
1.
Sedimentary model of the Permian sandy conglomerate in the footwall of the Kebai Fault,the Junggar Basin
准噶尔盆地克百断裂下盘二叠系砂砾岩的沉积模式
2) Kebai fault zone
百克断裂带
1.
The Kebai fault zone is one of most prolific areas in Junggar Basin.
百克断裂带原油凝固点相对较低,饱和烃含量和含蜡量相对较低;原油根据生物标志化合物特征划分为A类和B类,不同类型原油的分布具有明显的分带性。
3) Ke-Bai fractured zone
克-百断裂带
1.
Discussion on controlling factors for Carboniferous hydrocarbon accumulation in the Ke-Bai fractured zone of the northwestern margin in Junggar Basin
准噶尔盆地西北缘克-百断裂带石炭系油气成藏控制因素新认识
4) Ke-Wu fault belt
克-乌断裂带
5) Kuyak fault
库牙克断裂
1.
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。
6) Tumuxiuke fault belt
吐木休克断裂带
1.
Tumuxiuke fault belt is situated in the northwest part of Tarim basin.
吐木休克断裂带位于塔里木盆地的西北部,是研究区规模最大、最具有研究意义的走滑断裂。
2.
It can be divided into Bachu block uplift and Awati depression by Tumuxiuke fault belt.
研究区位于塔里木盆地的西部 ,以吐木休克断裂带为界将研究区划分为巴楚断隆和阿瓦提凹陷两个构造单元。
补充资料：百克
1.犹言百战百胜。
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