1) trastensional basin
张扭性盆地
2) transtensional rifting basin
扭张性断陷盆地
1.
Through research in basin structures, subsidence and tectonic-sedimentary migration process, we proposed that the Yinggehai basin is a sinistral transtensional rifting basin from Eocene to early Oligocene.
本文通过对盆地结构、沉降特征和构造 -沉积迁移过程的研究 ,提出莺歌海盆地在始新世—早渐新世期间属左旋扭张性断陷盆地 ,晚渐新世—早中新世的盆地演化阶段受到红河断裂带的左行剪切运动影响。
3) Transtensional basin
扭张盆地
4) the transtensional faulted-depression basin
张扭性断陷-坳陷盆地
5) tensional basin
张性盆地
1.
Extensional fold is an important component part of tectonic deformation in tensional basins,which distributes widely,and mostly belongs to normal fault-related folds.
伸展褶皱是张性盆地区构造变形的重要组成部分,其分布相当普遍,多属于与正断层相关的褶皱。
6) extensional basin
张性盆地
1.
Structural Modelling System in extensional basin is a backward modelling software based on the restoration and balancing principles and technique which are originally developed for fold-and-thrust belts.
张性盆地构造演化模拟系统是一套以平衡剖面原理和技术为基础的构造反向模拟软件。
补充资料：连续性与非连续性(见间断性与不间断性)
连续性与非连续性(见间断性与不间断性)
continuity and discontinuity
11an父ux泊g四f“山。麻以角g、.连续性与非连续性(c。nt，n琳t:nuity一)_见间断性与不间断性。and diseo红ti-
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