1) Kalpintag Fault
柯坪塔格断裂
1.
The Kalpintag Fault locates at the most forefront of Kalpintag nappe tectonics, and can be separated into eastern and western segments by Piqiang Fault.
柯坪塔格断裂位于西南天山柯坪塔格推覆构造的最前缘,以皮羌断裂为界分成东西两段。
2) Kalpintag
柯坪塔格
1.
The Kalpintag nappe is located at the southwestern foot of the Tianshan Mountains,consisting of several rows of NE-to EW-trending fold-reverse fault zones.
柯坪塔格推覆体位于天山西南麓,由多排NEE—EW向的褶皱-逆断裂带组成。
2.
Based on a lot of outcrop geological surveys, we discussed the thrust fault belt in the front of the east section of Kalpintag in Kalpin area and found many evidences, including the fault incising the surface of diluvium and fluvial channel sediments and terraces, and also the fracture and subsection character of the faults.
柯坪塔格前缘断裂东段是柯坪推覆构造系前缘的一条活动断裂,野外调查获得了其晚第四纪错断洪积扇、冲沟阶地面的证据,实测了变形地貌面上的断层陡坎,分析了断层的形变量,通过采样测年估算了断层的缩短速率。
3.
This paper tries to discuss paleoearthuakes along the east section of the range front fault of Kalpintag during late Quaternary by doing field investigation along the fault, measuring geomorphic deformation and excavating trenches in some important sites where young alluvial fans were displaced obviously.
文中试图通过对柯坪推覆构造区的影像解译和野外观察、断错地貌的实测和探槽开挖,探讨柯坪塔格山前断裂东段晚第四纪以来的古地震活动。
3) Keping fault
柯坪断裂
4) Kepingtage Formation
柯坪塔格组
1.
Sedimentary characteristics and pool distribution in the Silurian Kepingtage Formation of Tazhong area;
塔中地区志留系柯坪塔格组沉积特征与油气分布
2.
Trace Fossils in the Silurian Kepingtage Formation in the Kalpin Area,Xijiang;
新疆柯坪地区志留系柯坪塔格组的遗迹化石
3.
Sedimentary Characteristics of Silurian Kepingtage Formation,Tahe Area
塔河地区志留系柯坪塔格组沉积特征
5) Lower Kelpingtag Formation
下柯坪塔格组
1.
The graptolite－bearing strata mentioned above may be correlated with those of Kelping mountains of the northwestern margin of Tarim Basin， approximattely corresponding to the Lower Kelpingtag Formation and the Upper KelpingtagPormation separately
它们所含笔石地层的层位，可与塔里木盆地西北缘柯坪地区的相应地层层位作对比，分别大致相当于下柯坪塔格组和上柯坪塔格组。
6) Upper Kelpingtag Formation
上柯坪塔格组
补充资料：格里菲斯断裂判据
分子式：
CAS号：
性质：按格里菲斯理论，脆性材料的断裂强度σ由下式表示：式中，E为弹性模量；r为单位表面的断裂表面能；c为半裂纹长度。将上式右边分母移到左边，得σ=，此式即称为格里菲斯判据。它表明，对于任何给定材料，当σ(πc)1/2等于或大于由该材料性能(E，r)决定的某个临界值时，才会发生断裂。
CAS号：
性质：按格里菲斯理论，脆性材料的断裂强度σ由下式表示：式中，E为弹性模量；r为单位表面的断裂表面能；c为半裂纹长度。将上式右边分母移到左边，得σ=，此式即称为格里菲斯判据。它表明，对于任何给定材料，当σ(πc)1/2等于或大于由该材料性能(E，r)决定的某个临界值时，才会发生断裂。
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