1) East Kunlun
东昆仑山
1.
Geochemical characteristics and tectonic setting of volcanic rocks in the Muztag ophiolitic mélange, East Kunlun Mountains, Xinjiang, China;
东昆仑山木孜塔格蛇绿混杂岩中火山岩的地球化学特征及构造环境
2.
Geochemical characteristics of the Qingshuiquan mafic-ultramafic rocks, East Kunlun;
东昆仑山清水泉镁铁质——超镁铁质岩的地球化学特征
2) eastern Kunlun Mountain
东昆仑山东段
1.
The study on the drainage system in the north slope of the eastern Kunlun Mountains indicates that the E-W trending basin-mountain geomorphology was formed after the Kunlun-Yellow River tectonic movement.
对东昆仑山东段北坡众多河流阶地及其沉积物的研究表明,该区在早更新世晚期昆仑-黄河运动之后形成的东西向盆岭相间的地貌特征奠定了早期河流为东西向外流水系的基础;中更新世晚期以来的又一次强烈构造抬升事件———共和运动,导致昆仑山北坡各主要河流迅速溯源侵蚀发展,伴随河流袭夺而形成现今的水系格局;晚更新世晚期存在一段相对较长的构造稳定期,河谷普遍发生堆积作用,形成分布广泛且厚度较大的晚更新世冲积层;接近全新世以来构造运动频繁而隆升的幅度趋于减弱,形成了5级河流阶地,并且阶地的发育类型普遍为以高级阶地(T5)为基座的上叠阶地,河流至今未能切穿晚更新世稳定期形成的厚冲积层。
4) eastern Kunlun orogenic belt
东昆仑造山带
1.
Discovery of Miocene Sporopollen from Matrix Strata of the Naij Tal Group-Complex in the Eastern Kunlun Orogenic Belt;
东昆仑造山带纳赤台岩群基质地层发现中新世孢粉组合
2.
The eastern Kunlun orogenic belt shows characteristics of soft-collision and multi-cycles.
东昆仑造山带具有软碰撞、多旋回的特点 ,造山带内的沉积盆地具有多物源和不同的大地构造背景 。
3.
According to rock characteristics,the Longshigenggongma mélanges(Neoproterozoic Wanbaogou Group—Early Paleozoic Nachitai Group),southern Qingshuiquan,Eastern Kunlun orogenic belt can be divided into 3 types:flysch rock slice,carbonate rock slice and basalt rock slice.
东昆仑造山带清水泉南部的龙什更公玛混杂岩(新元古界万保沟岩群—下古生界纳赤台岩群)按岩性可分为3类岩片:复理石岩片、碳酸盐岩岩片、玄武岩岩片,其中复理石岩片根据其形成年代不同分为新元古界复理石岩片和下古生界复理石岩片。
5) East Kunlun orogenic belt
东昆仑造山带
1.
Inspirations from the Sino-U.S. cooperative geological mapping in the East Kunlun orogenic belt: ideas and methods
中美合作东昆仑造山带地质填图的启示:填图理念与填图方法
2.
The Wanbaogou Group-complex is a mélange in the East Kunlun orogenic belt,which is composed of two parts:exotic blocks of various ages and matrix strata.
东昆仑造山带万宝沟岩群是一套混杂堆积地层,有外来岩块和基质地层之分,以往根据岩块中的化石将该套地层的时代划为前寒武纪的蓟县纪—青白口纪。
3.
Based on the basin-range coupling theory,the tectonic geology events during Mesozoic and Cenozoic were determined from the point that East Kunlun orogenic belt and west-south Qadam basin were in a common stress field,combining with versatile data and filed geology review.
根据盆山耦合理论,从东昆仑造山带与柴西南盆地受制于共同应力场的角度,结合二者资料及野外考察,对东昆仑山中、新生代以来的构造事件进行了厘定。
6) Eastern Kunlun Fault zone
东昆仑山断裂带
补充资料：昆仑山
【昆仑山】
（地名）内典所谓香山是也。香山具名香醉山，在雪山之北。此山之南有无热池，以为四大河之源。南山戒疏一上曰：“俗云昆仑者，经谓香山也。”(参见：香山)
（地名）内典所谓香山是也。香山具名香醉山，在雪山之北。此山之南有无热池，以为四大河之源。南山戒疏一上曰：“俗云昆仑者，经谓香山也。”(参见：香山)
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