1) Yanshan tectonic belt
燕山构造带
1.
Aiming at the problem of tectonic deformation of Indosinian period in eastern part of North China , the field investigation as well as the map compiling was carried out; The appearance and characteristic of deformation of Indosinian period in Bohai Bay basin, Yanshan tectonic belt ,Liaoxi, Liaodong, and Luxi areas were discussed.
针对华北东部印支期构造变形问题 ,进行了野外调研和室内编图工作 ;讨论了渤海湾盆地及燕山构造带、胶南隆起、辽西、辽东等地区印支期构造运动的表现、变形特征、变形期次 。
2.
The Yanshan tectonic belt, which is located at the northern margin of the North China block,has often been referred to as the cradle of Chinese geology.
位于华北地块北缘的燕山构造带，是中国地质工作的摇篮地区之一，以中新生代强烈的板内变形而闻名于世。
2) Yanshan structural belt
燕山构造带
1.
Depositional process and evolution of Luanping Early Cretaceous basin in the Yanshan structural belt.;
燕山构造带滦平早白垩世盆地沉积过程和演化
2.
The Fengshan basin is a well-preserved extensional basin in the Yanshan structural belt.
凤山盆地是燕山构造带内的一个早白垩世伸展盆地。
3) Yanshanian orogenic belt
燕山期构造带
4) 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。
5) 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。
6) the Yanshan orogen
燕山造山带
1.
According to the chronological and geochemical data of Jurassic-Early Cretaceous magmatic rocks and the sequence of tectonic events,the framework of magmatism sequence from the Early Jurassic to Early Cretaceous in the Yanshan orogen, North China was proposed.
根据燕山地区侏罗纪—早白垩世岩浆岩的同位素年代学和化学成分资料,以及该地区构造变形序列,初步总结了燕山造山带岩浆活动时间序列和岩性组合:第一阶段的代表是早侏罗世英安岩和玄武岩;第二阶段以中侏罗世中性火山岩和闪长岩 石英二长岩/花岗闪长岩 花岗岩侵入岩组合为标志;第三阶段表现为晚侏罗世中、酸性火山岩和闪长岩 石英二长岩 正长岩 花岗岩侵入岩组合的活动;第四阶段为早白垩世早期安粗岩和流纹岩以及闪长岩 石英二长岩 正长岩 碱性正长岩 花岗岩侵入岩组合为标志;第五阶段以120Ma以后发育的小规模火山岩和花岗岩 碱性花岗岩组合为标志。
2.
According to the chronological and geochemical data of Jurassic-Early Cretaceous magmatic rocks and the sequence of tectonic events, the framework of magrnatism sequence from the Early Jurassic to Early Cretaceous in the Yanshan orogen, North China was proposed.
根据燕山地区侏罗纪—早白垩世岩浆岩的同位素年代学和化学成分资料,以及该地区构造变形序列,初步总结了燕山造山带岩浆活动时间序列和岩性组合:第一阶段的代表是早侏罗世英安岩和玄武岩;第二阶段以中侏罗世中性火山岩和闪长岩-石英二长岩/花岗闪长岩-花岗岩侵入岩组合为标志;第三阶段表现为晚侏罗世中、酸性火山岩和闪长岩-石英二长岩-正长岩-花岗岩侵入岩组合的活动;第四阶段为早白垩世早期安粗岩和流纹岩以及闪长岩-石英二长岩-正长岩-碱性正长岩-花岗岩侵入岩组合为标志;第五阶段以120Ma以后发育的小规模火山岩和花岗岩-碱性花岗岩组合为标志。
补充资料：板带轧制速度规程(见板带轧制规程设计)
板带轧制速度规程(见板带轧制规程设计)
speed schedule for plate and strip rolling
bandai zhazhi sudu guieheng板带轧制速度规程(speed seheduxe fo:plateand strip rolling)见板带札制规程设计。
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