1) southern Tibetan orogen
藏南造山带
2) Tibetan orogen
西藏造山带
3) central Tibetan orogen
藏中造山带
4) 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
5) 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。
6) orogenic belt of the South China
华南造山带
补充资料：上造
1.爵位名。秦制定爵位二十级，第二级为"上造"。后世亦有承袭秦制者。
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