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1)  Yilan-Yitong fault zone
依兰-伊通断裂带
1.
A study on Yilan-Yitong fault zone based on Remote Sensing Technology;
基于遥感技术研究依兰-伊通断裂带
2)  Yilan-Yitong fracture zone
依兰-伊通断裂
1.
The discussion of earthquake feature in north segment of Yilan-Yitong fracture zone;
依兰-伊通断裂北段地震活动性研究
3)  Yilan-Yitong graben fault
依兰-伊通地堑断裂
1.
On the basis of the background of the geologic structure and some seismological methods,the seismicity characteristics of the northen section on Yilan-Yitong graben fault were discussed.
依据地质构造背景和某些地震学方法,讨论了依兰-伊通地堑断裂北段的地震活动特征,认为该区域的地震活跃期通常在东北地震区活跃期的“尾声”或平静期开始,具有“首尾相接”的特点。
4)  Jiamusi-Yitong fault zone
佳木斯-伊通断裂带
1.
Discovery and timing of major thrustbelt in Jiamusi-Yitong fault zone;
佳木斯-伊通断裂带大型逆冲构造带的发现及形成时代
5)  Yilan-Yitong graben
依兰-伊通地堑
1.
The distribution and its forming condition of sporepollen fossil resedimented inTertiary system in Yilan-Yitong graben are throughly analyzed in this paper.
本文对依兰-伊通地堑第三系再沉积孢粉化石的分布及其形成条件进行了深入的分析,提出了再沉积的孢粉化石来自晚白垩世地层及其主要的鉴别方法。
6)  Lanliao fault belt
兰聊断裂带
1.
The formation and evolution of Lanliao fault belt in Dongpu Depression may be divided into two periods and five stages such as Mesozoic and Cenozoic Periods,and compression,iniital fracture,strong fracture,shrinkage and after vibration stages.
东濮凹陷兰聊断裂带的形成演化可分为两个时期 5个阶段 ,即中生代、新生代时期和挤压、初裂、强裂、萎缩、余动阶段。
补充资料:伊兰
【伊兰】
 (植物)Eravan!a,又作伊罗,黳罗,堙罗那等。树名。花可爱,气味甚恶,其恶臭及四十里。经论中多以伊兰喻烦恼,以旃檀之妙香比菩提。
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