1) Keping River
柯坪河
1.
Hydrological Feature and Flood Analysis in Keping River on South Slope of Tianshan Mountains,Xinjiang;
新疆天山南麓柯坪河水文特性与洪水分析
2) flow domain of Keping river
柯坪河流域
3) Keping
柯坪
1.
The sedimentary environment and genesis of Middle Ordovician nodular limestones in Keping,Xinjiang;
新疆柯坪中奥陶统结核状灰岩的沉积环境及成因
2.
Geochemistry of Salgan Black Shales of Middle-Upper Ordovician in Keping Outcrop, Tarim Basin;
柯坪剖面中上奥陶统萨尔干组黑色页岩地球化学特征
3.
Based on geological background, the author suggested that giant oil and gas fields formed during the second reservoir formation cycle and not destroyed can be found in Keping covered structural region.
文章根据柯坪隐伏构造的石油地质条件,认为在柯坪隐伏构造层中有可能找到未被后期破坏的、于第二成藏旋回期形成的大油气田。
4) Kalpin
柯坪
1.
The Dawangou section of Kalpin area, Xinjiang and Guangzhuang section of Pingliang area, Gansu were proposed as the global stratotype for the base of the Nemagraptus gracilis Biozone and the base of the global Upper Ordovician Series.
新疆柯坪大湾沟和甘肃平凉官庄剖面是 N emagraptus gracilis带及上奥陶统底界的重要剖面 ,研究这两剖面的牙形刺具有十分重要的意义。
2.
Located on the northwest margin of the Tarim basin,the Kalpin Ranges are totally composed of thrust sheets, which comprise from Cambrian to Permian stata generally dipping to north.
塔里木西北的柯坪地区存在着再变形的逆冲岩席。
5) Keping area
柯坪地区
1.
Sedimentary sequences in Keping area, Xinjiang: Constraints from carbon and oxygen isotope compositions of Cambrian to Ordovician carbonate rocks
新疆柯坪地区寒武纪-奥陶纪碳酸盐岩沉积旋回的碳氧同位素研究
2.
The source rocks in Keping area of Tarim basin are studied synthetically and qualitatively by combining the previous findings with the analytical data of samples from drilling cores and the section outcrops.
对柯坪地区的烃源岩进行的综合定性研究表明 ,烃源岩可分为寒武系、奥陶系、石炭系和二叠系四套主要源岩层系。
6) Kalpin area
柯坪地区
1.
Based on the study of Silurian outcrop at the Kalpin area in the northwest of Tarim Basin, Xinjiang, 15 ichnogenus and 28 ichnospecies, namely, Asterichnus lawrencensis, Cochlichnus anguineus, Cruziana ichnosp.
通过对柯坪地区剖面志留系的研究,在柯坪塔格组中已识别出遗迹化石15属20种,它们是:Asterichnus lawrencensis,Cochlichnus anguineus,Cruziana ichnosp。
2.
Based on the study of the Silurian sections in the Kalpin area of the northwestern Tarim Basin, eight ichnogenus and eight ichnospecies were recognized in the Lower Silurian Tataaiertage Formation.
通过对塔里木盆地柯坪地区志留系塔塔埃尔塔格组上段遗迹化石的研究,识别出8属8种。
补充资料：柯河—茸安高山峡谷生态旅游风景区
柯河—茸安高山峡谷生态旅游风景区
柯河—茸安是深切的高山峡谷地貌，在茸安乡达尔仓沟口，海拔2900米，逆大渡河支流（麻尔曲河）柯河峡谷而上，至柯河峡谷俄家俄满雅尔山顶，海拔5036米，相对高差达2136米。河谷深切，河流湍急，地势崎岖。两条峡谷在茸安乡直尕以下汇合后通向马尔康境内，柯河、茸安地带是一个十分独特的立体生态分布区，山顶有碧绿的草甸，下面是黑郁郁的松杉针叶林带，依河而下是针阔叶混交林，河边是郁郁葱葱的灌丝，林中有熊、鹿、麝、藏马鸡等各种珍贵野生动物，栖息生长着羊肚菌、松茸、蕨菜和各种野生中药材。河谷许多地段开发有漂流等特种旅游． 柯河、茸安峡谷秋季红叶风景十分美丽壮观。数十公里的红叶、金色的白桦将整个峡谷点缀得十分美丽。河谷地带还有独特的柯河姊妹碉、伸臂桥、神山寺庙、佛塔和鱼塘石门槛、摩天岭、安湖水库等景点，让人流连忘返。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。