1) Himalayan movement
喜山运动
1.
By analyzing tectonic activities,hydrocarbon source-reservoir-seal associations and crude geochemistry in Laizhouwan sag,it is considered that the main tectonic events to control hydrocarbon accumulation are Himalayan movement and Tanlu Fault activity.
通过对莱州湾凹陷构造活动、生储盖组合及所发现原油地球化学特征的分析,认为影响该区油气成藏的构造活动主要为喜山运动和郯庐断裂活动。
2) Himalayan structural evolution
喜山期构造运动
3) the second episode of Himalaya Movement
喜山运动Ⅱ幕
1.
The change of subsidence model in Cenozoic petroliferous basins of Eastern China which goes from rifting subsidence stage in the Late Oligocene to whole thermal subsidence in the Early Miocene was caused by the second episode of Himalaya Movement.
渐新世末至早中新世,喜山运动Ⅱ幕促使中国东部新生代含油气盆地由断陷沉降向整体坳陷转变,造成古/新近系地层的广泛不整合、盆内次级断层发育以及局部地区的正反转构造等特征;并且造成不整合面附近地层的沉积体系发育特征由渐新世末的滨浅湖、冲积扇和河流—三角洲相沉积为主到中新世的冲积扇—辫状河相沉积为主的转变。
4) take up mountain climBing.
喜欢上登山运动
5) I like sports.
我喜欢运动。
6) Himalayan movement
喜马拉雅运动
1.
Episodes and geodynamic setting of Himalayan movement in China;
中国喜马拉雅运动的期次及其动力学背景
2.
Himalayan movement originated from powerful compressive stress in Tethys tectonic domain, which caused north Tianshan mountains to quick and extensive uplift and thrusting toward Junggar basin followed by shaping foreland depression of intracontinental orogenic type developed in the southern margin of Junggar basin.
喜马拉雅运动期源自特提斯构造域的强大挤压应力使北天山快速、大幅度隆升,并向盆地冲断,在盆地南缘发育了陆内造山型类前陆坳陷。
3.
Himalayan movement in this basin can be divided into eleven stages in terms of weak-strong intensity of structural compression.
酒西盆地位于青藏高原的东北缘,天然地震活跃,喜马拉雅运动在盆地的活动可划分出11个阶段,其构造挤压强度依次由弱变强,在上新世中期达到高峰,是该区构造的主要变形期和定格期,也是该区油气成藏的主要时期。
补充资料：秋夜肃公房喜普门上人自阳羡山至
【诗文】：
山栖久不见，林下偶同游。早晚来香积，何人住沃洲。
寒禽惊后夜，古木带高秋。却入千峰去，孤云不可留。
【注释】：
【出处】：
全唐诗：卷147_62
山栖久不见，林下偶同游。早晚来香积，何人住沃洲。
寒禽惊后夜，古木带高秋。却入千峰去，孤云不可留。
【注释】：
【出处】：
全唐诗：卷147_62
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