1) Sujiao orogenic belt
苏胶造山带
1.
In which,Songshan rockmass is deemed to be granite of A 1 subtype,formed in an extensional environment of Sujiao orogenic belt in Jinning stage and the orogenic Tanlu strike-slip fracture belt;Niushan rockmass is deemed to be granite of A 2 subtype,formed in an extensional environment of Sujiao orogenic belt of collision post-orogenesis in Sinian stage;Tiqiushan rockmass is deemed to be granit.
其中宋山岩体属A1亚型花岗岩类 ,形成于晋宁期苏胶造山带同造山的郯庐走滑断裂带的拉张环境 ;牛山岩体属A2 亚型花岗岩 ,形成于震旦期苏胶造山带碰撞造山后的拉张环境 ;踢球山岩体属A1-A2 过渡亚型花岗岩 ,形成于燕山期苏胶造山带陆内造山后和郯庐断裂带的拉张环
2) Sulu orogen
苏鲁造山带
1.
Zircon ages and Hf isotopic composition of gneisses from the Rongcheng ultrahigh-pressure terrain in the Sulu orogenic belt;
苏鲁造山带荣成超高压地体片麻岩锆石年龄和铪同位素组成特征
2.
Major and trace element geochemistry of granitic gneisses from Sulu orogen,eastern Shandong Peninsula: evidence for a Neoproterozoic active continental margin in the northern margin of the Yangtze craton.;
苏鲁造山带胶东区段花岗片麻岩类的常量与微量元素地球化学:扬子克拉通北缘新元古代活动大陆边缘的证据
3.
Low-grade metamorphic rocks of greenschist facies occurred in the ultrahigh pressure (UHP) metamorphic zone in the Sulu orogen.
苏鲁造山带超高压变质带内部出露仅经过绿片岩相变质作用的浅变质岩系,地质调查显示,石桥浅变质岩与周边超高压变质岩呈构造接触(构造片岩);地球化学研究证实,该浅变质岩形成于扬子板块北缘大陆边缘厚地壳上裂陷或沉积盆地的构造背景;单矿物电子探针分析结果显示,其部分浅变质岩发育多硅白云母,形成于中-高压相变质环境,说明这些浅变质岩曾经历大陆板块俯冲的动力变质作用过程。
3) Sulu orogenic belt
苏鲁造山带
1.
Three layers are present in the middle and upper crusts in the northern border of Sulu orogenic belt, as revealed by the S-N-strike reflecting seismic profiles that cross the Zhucheng sag.
横穿诸城凹陷的南北向反射地震剖面揭示,苏鲁造山带北侧边界的中上地壳中存在着三层结构,即上部的胶莱盆地沉积盖层、中部的苏鲁楔状地体和下部代表华北板块的胶北地体;诸城凹陷边缘和内部断裂均显示同沉积正断层性质,苏鲁楔状地体中发育一组向北仰起的叠瓦状逆冲断层,而胶北地体显示了向南俯冲的态势。
2.
High-pressure sinistral strike-slip shear belts in the NE-trending Tan-Lu fault zone along the western margin of the Sulu orogenic belt are first reported in this paper.
本文首次报导苏鲁造山带西缘新发现的北东向郯庐高压左旋走滑韧性剪切带。
4) Su-Lu orogen
苏鲁造山带
1.
Lithostratigraphic framework on the southern margin of the Su-Lu orogen;
苏鲁造山带南缘岩石-地层格架
2.
According to the synthetic study of regional correlation of metamorphic supracrustal rocks in the orogen, and the sequence of the magmas evolvement and their Nd isotope, it is suggested that the basement of Su-Lu orogeny belongs neither North China block, nor Yangtze block, but an unattached geotectonic unit.
苏鲁造山带的基底在大地构造上是归属华北板块还是扬子板块 ,抑或二者兼而有之还是二者都不是 ?存在着不同意见。
3.
According to detailed mapping in the Jinping area on the southern edge of the Su-Lu orogen, it is affirmed that the boundary between the ultrahigh-pressure metamorphic belt and high-pressure metamorphic belt is a ductile shear zone.
通过对锦屏山地区详细填图,确认了苏鲁造山带南缘超高压变质带与高压变质带的界线性质为一韧性剪切带,锦屏地区不存在区域性褶皱,而是由于朐山花岗质片麻岩和云台岩群变质火山岩构成强干岩层,锦屏岩群变质沉积岩构成软弱岩层,形成夹心饼式(layercakeassemble)组合,在印支期右行剪切作用下,形成不均一剪切,使朐山花岗质片麻岩形成长约10km,宽约5km的无根剪切舌状体,物质运动方向指向南。
5) Jiaonan orogenic belt
胶南造山带
1.
The latest understandings of fundamental geology of Jiaonan orogenic belt;
对胶南造山带基础地质问题的新认识
2.
Along with the deformation becoming more and more intensive, great changes are noticed in chemical composition of the tectonites developed in the ductile shear zones on the margin of the Jiaonan orogenic belt.
胶南造山带北缘剪切带，随着变形程度的增强，其构造岩的岩石化学成分发生明显的变异；在总结成分变异特征的基础上，分析了成分变异与体积变化、渗流流体作用的关系。
6) Dabie-Sulu orogenic belt
大别-苏鲁造山带
1.
Possible tectonic manifestations of the Dabie-Sulu orogenic belt on the Korean Peninsula;
大别-苏鲁造山带在朝鲜半岛可能的构造表现
补充资料：阿尔卑斯造山带
欧洲的阿尔卑斯以及其它一些年青的巨大造山带和褶皱山系。早第三纪和晚第三纪由于阿尔卑斯运动(中国称喜马拉雅运动)，使沿欧洲南部中生代的古地中海发生了强烈褶皱，形成横贯东西的阿尔卑斯-喜马拉雅山脉(从西班牙至亚洲南部)。严格地说，此词只限于造山带的北翼，由徐士(E.Suess)创名。同义词有“地中海带”、“阿尔卑斯-喜马拉雅带”。板块构造学说认为，这个造山带属碰撞型山链。(共213字)
【引用信息】徐世芳，李博主编.地震学辞典.北京：地震出版社.2000.第5页.
【引用信息】徐世芳，李博主编.地震学辞典.北京：地震出版社.2000.第5页.
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