1) thrust belt in the foreland of Kunlun Mountain
昆仑山前冲断带
2) Kunlun fault zone
昆仑山断裂带
1.
Finite difference numerical simulation of trapped waves in the Kunlun fault zone;
昆仑山断裂带围陷波的有限差分数值模拟解释
3) Eastern Kunlun Fault zone
东昆仑山断裂带
4) The north marginal fold-and-thrust belt of the Western Kunlun
西昆仑北缘冲断带
5) western Kunlun foreland basin
西昆仑山前
1.
An apatite fission track investigation was carried out from the Cenozoic (N) sandstones along Kokyar section in the western Kunlun foreland basin.
西昆仑山前柯克亚剖面厚度约7 000 m,通过对该剖面4个样品的磷灰石裂变径迹特征进行的详细分析,按地层厚度计算,样品埋深应为3 000~5 000 m,按古地温梯度计算埋深温度至少为60℃,进入磷灰石裂变径迹的退火带温度。
6) Kunlun orogenic belt
昆仑造山带
1.
Discussion on Depositional Characteristics and Basin Quality in Kunlun Orogenic Belt During Early-Middle Devonian;
昆仑造山带早—中泥盆世沉积特征及盆地性质探讨
2.
The results indicate that: in Carboniferous period,Kunlun orogenic belt was in an extension setting,and the north Kunlun was an active margin rift with littoral-neritic sediments of salf-blue water and volcanic basin;the Central Kunlun was an ocean island and underwater uplift,the oceanic islands were denudation areas,whereas the underwater uplifts were mai.
通过多年野外观察、分析测试,结合覆盖全区的1∶250000区域地质调查资料及其他前人研究成果,选择昆仑造山带晚古生代洋盆发育的典型时期石炭纪,对其地层、岩相特征、构造古地理以及构造演化进行了研究。
3.
It was in Paleozoic that the tectonic and deposition system of Kunlun orogenic belt had been formed.
昆仑造山带基本构造-地层格架奠基于古生代,晚泥盆世是加里东造山旋回和华力西造山旋回转换的关键阶段,加里东碰撞造山和其后的伸展裂陷等记录均存在于晚泥盆世沉积地层中。
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