1) Svecofennian orogenic belts
瑞芬造山带
1.
Svecofennian orogenic belts in northern Europe were formed by early Proterozoic Svecokarelids(2000-1750Ma).
北欧瑞芬造山带（Ｓｖｅｃｏｆｅｎｎｉａｎｏｒｏｇｅｎｉｃｂｅｌｔｓ）形成于早元古代（２０００～１７５０Ｍａ）的瑞卡构造运动（Ｓｖｅｃｏｋａｒｅｌｉｄｓ）。
2) Svecofennide belt
瑞典-芬兰造山带
3) Tianshan orogenic belt
天山造山带
1.
The geoscience transect from Korla to Jimsar runs through the northern margin of the Tarim basin, the Tianshan orogenic belt and the southern margin of the Junggar basin.
库尔勒—吉木萨尔剖面横跨塔里木盆地北缘、天山造山带和准噶尔盆地南缘 。
2.
The Tianshan orogenic belt within Chinese territory is situated in the northwestern China.
天山造山带是一个著名的地震活动带，而阴山-燕山断隆带历史上不但没有大地震发生，小地震也不多见，是一个地震空白区。
4) Langshan orogenic belt
狼山造山带
1.
Mineralization response to the structural evolution in the Langshan orogenic belt,Inner Mongolia.;
内蒙古狼山造山带构造演化与成矿响应
5) Yanshan orogen
燕山造山带
1.
Genesis of the middle-later Jurassic volcanic rocks of Tiaojishan (Lanqi) period and its geodynamic implication,Yanshan Orogen,east China.;
燕山造山带中—晚侏罗世髫髻山期(蓝旗期)火山岩的成因及其动力学意义
2.
The Changli-Chengde-Dalainuoer wide-angle/refraction seismic profile completed in 1985 extends northwestward across the Yanshan orogen.
昌黎—承德—达莱诺尔宽角反射/折射地震剖面完成于1985年,呈NW向横过燕山造山带中段,部分测段与2002年实施的120km深反射地震剖面重合。
3.
The volcanic lavas of the middle-late Jurassic of Tiaojianshan formation in the middle section of Yanshan Orogen (fromXiabancheng county in North Hebei province) are composed of trachyandesite and trachyte.
燕山造山带中段(冀北下板城)中晚侏罗世髫髻山组火山岩主要由粗安岩和粗面岩组成。
6) Yanshan orogenic belt
燕山造山带
1.
Structural Elements Association of Yanshan Orogenic Belt, North China;
华北燕山造山带结构要素组合
2.
This is the first report of ferrogabbros in the Yanshan orogenic belt.
这是迄今为止燕山造山带存在铁辉长岩类岩石的首次报道。
3.
The structural feature of Yanshan orogenic belt, which is not reflected by the published geological maps, is very complex.
燕山造山带具有极其复杂的地质结构构造,其复杂性在现有公开出版的地质图件中未能有效地反映出来。
补充资料：一山兆瑞
位于接引殿路旁的岩壁上。上面坚排“第一山”三字，大字三尺，为天然红苔藓长成。但三字很难现全，有时是“第一”两字，有时又是“一山”两字。据说，如果出现“第一山”三字，这一年就是个好年，于是人们便把它叫做“一山兆瑞”。
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