1) west-middle section of East Kunlun Mt
东昆仑中西段
1.
A sequence of paralic strata which contains biota fossils from Early-Middle Devonian is found in Bukadaban district in west-middle section of East Kunlun Mt.
在东昆仑中西段布喀达坂峰地区发现了一套含早—中泥盆世生物化石的海陆交互相地层,从而确定了该地区泥盆纪地层的存在。
2) thrust propagation
东昆仑西段
1.
There is a very well-developed fault system in the western sector of the East Kunlun, and thrust propagation, normal slip and decoupling were the main deformation events in the area; 2.
东昆仑西段是我国西北地区地质研究程度较低的地区之一。
3) eastern segment of the West Kunlun
西昆仑东段
1.
Study shows that the Meso-and Neopro terozoic volcanic rocks distributed south of the line of Cele-Mingfeng-Yutian on the northern margin of the eastern segment of the West Kunlun Mountains ,Xinjiang,consist dominantly of a suite of low-grade(basaltic)andesite with very small amount of rhyolite.
分布于新疆西昆仑东段北缘(策勒—于田—民丰一线以南)的中新元古代火山岩主要为一套浅变质的(玄武)安山岩,夹有极少量的流纹岩。
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。
6) east part of western Kunlun
西昆仑东段北缘
补充资料：十报恩 赠段先生 折段字起
【诗文】：
公物外好生涯。火相逢结大砂。女盘桓看大药。牛哮吼戏灵葩。云铺地丹炉赫，子观天碧眼华。有三生君省悟，中无事步烟霞。
【注释】：
【出处】：
公物外好生涯。火相逢结大砂。女盘桓看大药。牛哮吼戏灵葩。云铺地丹炉赫，子观天碧眼华。有三生君省悟，中无事步烟霞。
【注释】：
【出处】：
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