1) North Junggar
北准噶尔
1.
The Qiaoxiahala iron-copper-gold deposit is located in the northern margin of the North Junggar tectonic belt,and is distinct from the Mengku and Abagong iron deposits which also formed in the Devonian in the inner Altay orogenic belt.
乔夏哈拉铁铜金矿床位于北准噶尔构造带北缘,与阿尔泰造山带内分布的近同一时代的蒙库和阿巴宫铁矿不同。
2) northern Junggar
准噶尔北部
1.
In northern Junggar,there exist all kinds of primary gold deposits,which could be divided into five minerogenetic kinds known as epithermal gold deposits,micro finegranular dissemination gold deposits,altered rock gold deposits hosted by ductile shear belts,altered rock gold deposits related to some supergene rocks and metamorphic hydrothermal reformed gold deposits.
新疆准噶尔北部产有各种类型的原生金矿床， 本文将其划分为浅成低温热液型、微细粒浸染型、韧性剪切带蚀变岩型、浅成岩蚀变岩型、变质热液改造型等成矿类型。
3) northern margin of Junggar
准噶尔北缘
1.
A new kind of gold mineralization, named supergene and structural-altered rocks gold deposit has been discovered in the northern margin of Junggar.
准噶尔北缘发现了一种较特殊的金矿化类型即浅成岩－构造蚀变岩金矿。
2.
In northern margin of Junggar, there are some basic metallurgical types of gold deposits named epithermal gold deposits, altered mylonite type gold deposits related to ductile shear zone, hypabassal and structeral altered rocks type gold deposits, and so on.
准噶尔北缘存在浅成低温热液型金矿床、韧性剪切带蚀变糜棱岩型金矿床及浅成岩 构造蚀变岩型金矿床等主要矿化类型 。
6) northern part of East Junggar
东准噶尔北部
1.
Three representative plutons,Wutubulak,Areletuobie and Hadansun,in the lower reaches of the Qinggeli river in the northern part of East Junggar,Xinjiang were chosen for Rb-Sr isochron dating.
选取新疆东准噶尔北部青格里河下游一带乌图布拉克、阿热勒托别和哈旦逊岩体等具一定规模的3个代表性岩体,通过全岩Rb-Sr等时线同位素定年,确定了研究区内玛音鄂博断裂南侧花岗岩类的形成时代分别为(334。
补充资料：北还登汉阳北原题临川驿
【诗文】：
驱车方向阙，回首一临川。多垒非余耻，无谋终自怜。
乱松知野寺，馀雪记山田。惆怅樵渔事，今还又落然。
【注释】：
【出处】：
全唐诗：卷351-24
驱车方向阙，回首一临川。多垒非余耻，无谋终自怜。
乱松知野寺，馀雪记山田。惆怅樵渔事，今还又落然。
【注释】：
【出处】：
全唐诗：卷351-24
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