1) Aulacogen
裂陷槽
1.
Recognition of Buried Aulacogen and Hydrocarbon Potential in Qiangtang Area of Qinghai-Tibet Plateau.;
青藏羌塘地区隐伏裂陷槽的识别及油气远景
2.
According to the ecologic and sedimentary features, the Late Permian biota and strata of south Guizhou can be grouped into the “shallow platform type”and “sub byssal aulacogen type”.
根据生态环境和沉积环境的差异 ,黔南晚二叠世生物群和地层可分出两种类型 :“浅海台地型”和“次深海裂陷槽型”,后者为深水型。
3) rift trough
裂陷槽
1.
On the basis of the division, correlation and study of the framework of sequences in the stable regions and rift trough in the Luofu, Dachang sections, Nandan County,the formati.
根据南丹罗富、大厂裂陷槽盆地泥盆系层序地层研究和与相邻稳定型泥盆系层序地层对比及层序地层格架分析，揭示了裂陷槽盆地的形成演化过程。
4) aulacogen
裂陷槽盆
1.
Chen M H, Shi L. Filling and evolution of the Late Paleozoic Shuicheng-Ziyun aulacogen in western Guizhou, China. Geological Bulletin of China,;
黔西水城—紫云地区晚古生代裂陷槽盆充填和演化
5) Trough shaped rift graben
槽形裂陷
6) Yan-Liao Aulacogen
燕辽裂陷槽
1.
Mesoproterozoic palaeoearthquake and palaeogeography in Yan-Liao Aulacogen;
燕辽裂陷槽中元古代古地震与古地理
补充资料：陷裂
1.陷落坼裂。
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