1) Kuruktag aulacogen
库鲁克塔格裂陷槽
2) Kuruketage region
库鲁克塔格
1.
Carbonate platform sediments have been widely developed in the Ordovician in the Kuruketage region of the Tarim basin but because of the turbulence environment the types of carbonate are mainly micritic intraclast and bioclasts and breaking oolites.
新疆塔里木盆地库鲁克塔格地区奥陶纪曾普遍发育碳酸盐岩台地沉积,但其沉积环境较动荡,碳酸盐岩组合类型为泥晶砂屑、生物碎屑和破碎鲕粒。
2.
In Kuruketage region,northeastern edge of the Tarim basin,The silicalite mainly occurred in the marine depositional sequences of lower Cambrian and middle Ordovician.
新疆塔里木盆地东北缘库鲁克塔格地区硅质岩主要出现在下寒武统和下、中奥陶统海相沉积层序。
3) Quruqtagh
库鲁克塔格
1.
Geochemical Characteristics of Early Cambrian Cherts in Quruqtagh, Xinjiang, West China;
新疆库鲁克塔格地区早寒武世硅质岩地球化学特征及其意义
2.
Three layers of tillites are developed in the Beiyixi formation,Teriaikan formation and Hangeerqiaoke formation of the Neoproterozoic in Quruqtagh region.
库鲁克塔格地区震旦系发育三层冰碛岩,分别是贝义西组、特瑞爱肯组、汉格尔乔克组。
4) Kuruktag
库鲁克塔格
1.
Nodular limestones of Hanguletag formation in the Kuruktag are part of a type of warty sedimentary sequence.
新疆库鲁克塔格地区巷古勒塔格组发育瘤状灰岩,是一种深水沉积序列。
2.
The Ordovician outcropped in Kuruktag, Xinjiang reveals a sedimentary sequence which shows long-term sea level changes.
出露于新疆库鲁克塔格地区的奥陶系揭示出一个完整长周期(Ⅰ级周期)的海侵-海退沉积序列。
3.
The old metamorphic rock system outcroped in Saimashan region of Kuruktag.
出露于库鲁克塔格赛马山一带被前人划分为达格拉格布拉克群的古老变质岩系，通过野外填图及室内分析工作，确定为一套块状无序花岗质正片麻岩，并建立构造岩石单位独断山片麻杂岩。
5) Kuluketage
库鲁克塔格
1.
The outcropping strata in the Kuluketage fault-uplifted zone of Tarim Basin,Xinjiang is a succession of bathyal-neritic deposits including phosphate rock,siliceous rock,volcanic rock,gypsolith,nodular limestone,carbonate tempestite,oolitic limestone and carbonate turbidite.
新疆塔里木盆地库鲁克塔格断隆区出露的寒武系由一系列半深海-浅海沉积物构成。
2.
The fault controls the development of stratum and the tectono-palaeogeographic and tectonic evolution of Kuluketage uplifted block known as the Manjiaer depression in the northeast margin of Tarim basin.
兴地断裂是塔里木盆地东北缘十分重要的大型控盆断裂,该断裂对塔里木盆地东北缘地层发育、构造古地理、库鲁克塔格断隆-满加尔坳陷的构造演化等具有重要的控制作用。
3.
It looks like a NW trend rhombus on morphology was surrounded by western Huola mountain and eastern Kezile mountain which are in the direction of NW, southern Kuluketage mountain and northern Saaer mountain which are EW trend.
盆地呈NW向菱形形态,被西侧的霍拉山和东部的克孜勒山、南部的库鲁克塔格山和北部的萨阿尔明山所围限,前两者呈NW向展布,后两者呈近EW展布。
6) Kuluketage area
库鲁克塔格地区
1.
Kuluketage area is located in the northeastern margin of the Tarim basin.
库鲁克塔格地区位于塔里木盆地东北缘，在片麻岩中出露较多斜长角闪岩类包体，其走向大致与片麻理的方向一致。
补充资料：克陷
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