1) middle belt of east Ku nlun Mountains
东昆仑中带
2) central belt of East Kunlun Mountains in Qinghai
青海东昆仑中带
3) Central Eastern Kunlun Suture Zone
东昆仑中部缝合带
1.
SHRIMP U-Pb zircon age of the granulite from the Qingshuiquan area, Central Eastern Kunlun Suture Zone;
东昆仑中部缝合带清水泉麻粒岩锆石SHRIMP U-Pb年代学研究
4) the middle sector of East Kunlun
东昆仑中段
1.
The studies of geological characteristics, melanic inclusion and Nd Sr isotopeshow that the Triassic Bairiqili rock body in the middle sector of East Kunlun was formed bynonhomogeneous and incomplete mixing of crust and mantle magma many times.
通过对岩体地质特征、暗色包体及Nd、Sr同位素资料研究表明:东昆仑中段中三叠世白日其利岩体是由壳幔岩浆不均一或不彻底多次混合作用形成的,岩体内部呈现出酸性、基性岩浆因混合程度和混合比例不同而形成复杂的岩体结构样式,其基性端元为混合不彻底而残留的辉长质岩石,酸性端元是受轻度混染的二长花岗岩,岩浆混合作用方式以就地混合为主,岩体形成于碰撞造山期后的构造环境。
5) 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。
6) eastern Kunlun metallogenetic belt
东昆仑成矿带
1.
The degree of geological research in the eastern Kunlun metallogenetic belt,Xinjiang is very low.
新疆东昆仑成矿带是我国地质工作程度较低的地区之一,在近年矿产勘查中发现了白干湖钨锡矿床等矿床(点)47处,圈定1∶5(10)万水系沉积物异常114处,并确立了该区属钨的地球化学块体。
补充资料：中带
1.古代妇女的内衣带。 2.指温带。
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