1) Jiangnan intracontinental orogenic belt
江南陆内造山带
2) Jiangnan orogen
江南造山带
1.
Neoproterozoic(～850 Ma) subduction in the Jiangnan orogen:evidence from the SHRIMP U-Pb dating of the SSZ-type ophiolite in southern Anhui Province;
江南造山带存在新元古代(～850 Ma)俯冲作用——来自皖南SSZ型蛇绿岩锆石SHRIMP U-Pb年龄证据
2.
Some Neoproterozoic Geological Events Involved in the Development of the Jiangnan Orogen
江南造山带形成过程中若干新元古代地质事件
3.
A geometrical and kinematic analysis of the Early-Mesozoic Yueyang-Chibi fold-thrust belt in southern Jiangnan orogen
江南造山带北部早中生代岳阳—赤壁断褶带构造特征及变形机制研究
3) Jiangnan orogenic belt
江南造山带
1.
Geochemical constraints on the tectonic setting of the Proterozoic turbidites in the Xuefeng Uplift region of the Jiangnan orogenic belt;
江南造山带雪峰隆起区元古宙浊积岩沉积构造背景的地球化学制约
2.
This paper is discussion microflora(contain 27genera and 40 species)and it,s age significance of the east segment of Jiangnan Orogenic Belt.
本文论述了江南造山带东段浅变质岩系发现的微古植物化石(计有27属40种)和它的时代意义,分析研究了西村组优势属为 Leiominuscula,Leiofusa,Asperatopsophosphaera,Germinosphaera,Melanocyillum 等5属；昌溪组优势属为 Germinosphaera,Leiominuscula,Leiopsophosphaera,Triangumorpha,Leiofusa 等5属；厘定了西村组、昌溪组地质时代为中元古代蓟县纪,通过对比和论证,提出了伏川蛇绿岩套形成的下限地质年龄在913-963Ma,上限地质年龄在800Ma。
3.
It can also be deduced that the Jiangnan orogenic belt can probably extend westward to Huili-Panzhihua area on the western margin of the Yangtze Block instead of turning southward from the Guizhou-Yunnan area.
本文的研究表明江南造山带向西可能一直延伸到扬子西缘的会理攀枝花一带,而不是经黔滇向南转折。
4) intracontinental orogenic zone
陆内造山带
1.
Stratigraphy of Mesozoic and Cenozoic intracontinental orogenic zones: an example from the Yanliao orogenic zone;
中新生代陆内造山带的地层学研究———以燕辽造山带为例
5) Yanshan intracontinental orogenic belt
燕山陆内造山带
1.
Panshan granitoid pluton situated in the southern margin of middle segment of Yanshan intracontinental orogenic belt consists of four intrusive units (Langjiayu,Guanzhuang,Dongluozhuang,Xiaopanshan) and porphyritic quartz-monzonite veins.
位于燕山陆内造山带中段南缘的蓟县盘山花岗岩体由狼家峪、官庄、东罗庄和小盘山4个侵入单元组成,并发育侵入期后含斑石英二长岩脉,发育环绕岩体分布的周缘向斜并侵蚀早期东西向蓟县断裂。
6) intra continent orogenic transfer zone
陆内造山转换带
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