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1)  Limjingang belt
临津江构造带
1.
There are two main tectonic events in Korean Peninsula in Middle Paleozoic——Early Mesozoic,that are the activity of Limjingang belt in middle Korean Peninsula in Middle Paleozoic and the collision event of Domangang orogenic belt(Hambuk Masiff) in the northern part of Korean Peninsula in Late Paleozoic——Early Mesozoic.
古生代中期─中生代早期朝鲜半岛发生了两次主要构造事件,即古生代中期朝鲜半岛中部临津江构造带的活动和古生代晚期—中生代早期朝鲜半岛北部豆满江造山带(咸北地块)的碰撞拼接事件。
2)  Rimjingang-Yannan miogeosyncline
临津江-烟南冒地槽带
3)  Rimjin-gang fault-geosyncline zone of Korea
朝鲜临津江断槽带
4)  Youjiang River tectonic belt
右江构造带
5)  Jiangda Tectonic Belt
江达构造带
1.
Studying on Evolution and Metallogenic Regularity and Ore-Prospecting Direction of the Jiangda Tectonic Belt, East Tibet, SW China;
西藏东部江达构造带演化及成矿规律与找矿方向研究
6)  Jiangnan-Xuefeng Structural Belt
江南-雪峰构造带
1.
According to the analyses on structural evolution and sedimentary features,Jiangnan-Xuefeng Structural Belt and its edge possess favorable petroleum geological conditions.
通过构造演化与沉积特征分析,认为江南-雪峰构造带及周缘具备良好的成油气地质条件;根据古油藏和油气显示在纵向及平面上的分布特征分析以及油气藏解剖,认识到保存条件是油气成藏的主控因素。
补充资料:临津
【诗文】:
临津艳艳花千树,夹径斜斜柳数行。
却忆金明池上路,红裙争自绿衣郎。



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