1) Longmenshan tectonic belt
龙门山构造带
1.
0 earthquake in Sichuan Province occurred on the Longmenshan tectonic belt at the eastern margin of the Qinghai—Tibet Plateau.
0级地震发生在青藏高原东缘的龙门山构造带上。
2.
The Surface rupture of Beichuan-Nanba-Linanshi Fault,which is the northern segment of Longmenshan tectonic belt is studied.
研究了2008年汶川大地震的发震构造龙门山构造带的北段,即北川-南坝-林庵寺断裂的地表破裂。
2) Longmenshan structural belt
龙门山构造带
1.
On the basis of seismic geological characteristics,seismic activity regularities and neotectonic movement,this paper suggests that stability of the Longmenshan structural belt is controlled by the Longmenshan fracture zone.
根据龙门山构造带的地震地质特征、地震活动规律及新构造活动特征，认为该地区区域稳定性受控于龙门山断裂带，而断裂带又以韧性切变形为主，蠕滑运动为特征，这决定了该带在相当长一段时间内，发生强烈地震的可能性不大。
3) Longmen orogenic belt
龙门山造山带
1.
Basin-range coupling system and its control on oil and gas accumulation in the Longmen orogenic belt and the West Sichuan foreland basin;
龙门山造山带与川西前陆盆地耦合关系及其对油气成藏的控制
4) Longmen-Jinping orogenic belt
龙门-锦屏造山带
1.
Uplift of the Longmen-Jinping orogenic belt along the eastern margin of the Qinghai-Tibet Plateau:Large-scale detachment faulting and extrusion mechanism.;
青藏高原东缘龙门-锦屏造山带的崛起——大型拆离断层和挤出机制
6) Longmen Mountain nappe structure zone
龙门山推覆构造
补充资料：构造山
由地壳构造运动形成的山体。可分为褶皱山、断块山、褶皱断层山等。
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