1) dextral pull-apart basin
右行拉分盆地
2) pull-apart basin
拉分盆地
1.
Jiaolai basin is a dextral strike-slip pull-apart basin.
胶莱盆地为右行非对称性菱形拉分盆地,其西部北北东向边界断裂和东部北东向边界断裂为Y主剪切断裂,南部北东向边界断裂为R剪切断裂,北部北东东-东西向边界断裂为R'剪切断裂。
2.
322,Resulting from the sinistral displacement of the NE-trending fault,there is a pull-apart basin in the Feng Zhou area.
由于北东向断层的左行走滑，在丰州一带生成拉分盆地。
3.
The sinistral strike-slip activity of the Xiaojiang fault with trend of N-S has led to the tectonic formation and development of the pull-apart basin,and after the basin formation the deformation of structural reversion was developed due to the same activity.
南北走向的小江断裂左行走滑活动，控制了拉分盆地构造的形成和发展，成盆期末又发生了构造反转变形，同时提出了盆地形成和构造反转的地球动力模式。
3) pull apart basin
拉分盆地
1.
Jiaolai Basin is a pull apart basin which was formed in the right lateral strike slip movements of Mouping Jimo faults during J 3-K 1.
胶莱盆地是 Ｊ３ － Ｋ１ 期间由牟平—即墨断裂带在右旋走滑运动中形成的 Ｓ型拉分盆地，盆地的产生与盆地边缘金矿的形成具有密切的成因关系。
2.
The pull apart basins were developed along the Luonan-Luanchuan fault belt under background of right slip movement in the northern Qinling area during the Late Cretaceous.
在新元古代—中奥陶世,其控制了洛南—栾川、云架山—二郎坪裂陷盆地的发育;志留纪末期—泥盆纪初,断裂由南向北逆冲推覆;晚古生代,断裂处于不活动状态;中三叠世末—早白垩世早期,造山带逆冲系前锋不断向北推进;晚白垩世,北秦岭地区处于右旋走滑背景,沿洛南—栾川断裂形成拉分盆地。
4) Youjiang basin
右江盆地
1.
Characteristics of hydrocarbon-bearing ore-forming fluids in the Youjiang Basin,South China:implications for hydrocarbon accumulation and ore mineralization;
右江盆地含油气成矿流体性质及其成藏-成矿作用
2.
Study on reservoir characteristics of the Late Paleozoic reef in Youjiang basin, China;
晚古生代右江盆地生物礁储层特征研究
3.
The palaeokarstification in the Late Palaeozoic Youjiang Basin, southwestern China;
晚古生代右江盆地古岩溶作用研究
5) strike-slip pull-apart basin
走滑拉分盆地
1.
Sequence stratigraphy in a strike-slip pull-apart basin: An example from the Laiyang Group in the Jiaolai Basin;
走滑拉分盆地层序构成特征——以胶莱盆地莱阳群为例
6) Yuehe pull apart basin
月河拉分盆地
补充资料：青海共和盆地南塔拉草地的退化与沙化
青海共和盆地南塔拉草地的退化与沙化
翼鲜臀犷华攀..州 青海共和盆地南塔拉草地的退化与沙化‘湘“
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