1) 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
2) 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。
3) Upper Kelpingtag Formation
上柯坪塔格组
4) Kepingtage Formation
柯坪塔格组下段
1.
Genesis of Marine Sandstone Parasequence of Ordovician Lower Kepingtage Formation in the Western Margin of the Manjiaer Depression and Its significance;
塔里木盆地满加尔凹陷西缘奥陶系柯坪塔格组下段海相砂岩准层序成因与意义
5) 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。
6) 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。
补充资料：上坪乡
上坪乡概况
上坪乡位于县西部，洮坪河上游，总面积347．07平方公里，耕地1．89万亩，总人口6929人，有行政村10个，乡政府驻地上洮坪村(北纬34°10′，东经104°51′，)，距县城40公里。
1953年始置上坪乡，1961年成立上坪人民公社，1983年恢复乡建制。
该乡属高寒阴湿地带，是全县最高地区，平均海拔2400米左右，年平均气温8℃，年降水量约600毫米，无霜期在120天左右。境内山大沟深，重峦迭嶂，森林茂密，水流湍急，回环曲折，河谷两岸90余里，风景秀丽。没遮拦梁海拔3312米，为县内最高峰。
该乡为县内最大林区。粮食作物以小麦、洋芋、洋麦为主，玉米、蚕豆等次之。1990年粮食年总产1571．22吨，工农业总产值142．18万元，农民人均纯收人263．77元，有木材加工、竹木编织等副业。特产有大黄、当归、蜂蜜等。有草场19万亩，礼县惟一的养马基地大河边马场就在境内。
有小学11所，在校师生500余人。乡有卫生院，村有医疗站。有简易公路通往林区。
蕨菜，俗称“羊蕨”，是上坪乡一大特产，杆茎盐渍厚质粘味鲜，为宴席中之名菜。
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