酒泉盆地群是由两期不同性质、不同世代盆地叠加而成的。
Jiuquan basin group is formed by the stacking of two stage basins with different property and different generation.
酒泉盆地青西凹陷和营尔凹陷是两个富油凹陷,具有较大的勘探潜力。
Qingxi sag and Ying 'er sag are the two oil-enriched sags in Jiuquan basin with large potentials for exploration.
酒泉盆地普遍发育了晚白垩世-始新世的不整面合,该期构造变形在花海地区表现尤为明显。
The late Cretaceous-Eocene unconformity is widely developed in the Jiuquan Basin, especially in Huahai area where the tectonic deformation is very prominent.
酒泉盆地南缘山前冲断带构造油气藏和富油凹陷内的构造—岩性油气藏为该盆地两个主要的勘探领域。
The structural reservoir in piedmont thrust zone and structural-lithologic reservoir in oil-rich sag of southern margin of Jiuquan basin are two main exploration fields in the basin.
第四纪以来,在青藏高原强烈隆升的影响下,酒泉盆地的古地理环境演化变迁经历了漫长和复杂的过程。
During Quaternary, the paleogeography and environmental evolution of Jiuquan basin experienced a prolonged and complicated process, intensely affected by the uplift of Tibetan Plateau.
窟窿山构造油藏目前是玉门油田的主力产油区块,也是增储上产最具潜力的区块,位于酒泉盆地青西凹陷南部,被祁连山北缘逆掩推覆。
Kulongshan Oil Reservoir, located in the south of the Qingxi Depression, Jiuxi Basin and overrided by the Qilianshan Mountain, is the primary producing area of the Yumen Oilfield.
老君庙构造带是中国发现最早的老君庙油田所处的构造带,位于酒泉盆地南缘新生代前陆冲断带,叠置于早白垩世断陷盆地的南部隆起和石大凹陷之上。
Laojunmiao structural belt is located in Cenozoic foreland thrust belt of south margin, Jiuquan basin, which is superposed over the south uplift and Shida depression of Early Cretaceous faulted basin.
最宽处在酒泉市与柴达木盆地之间,达300千米。
Widest point in Jiuquan City and between the Qaidam Basin, 300 km.
最宽处在酒泉与柴达木盆地之间,达300公里。
Widest point in between Jiuquan and the Qaidam Basin, up to 300 km.
柴达木盆地和酒泉、肃北旋转方向的差异预示了两地区间存在左旋错动。
The opposite rotation direction implies the existence of left lateral dislocation between Qaidam basin and Jiuquan and Subei areas.
柴达木盆地和酒泉、肃北旋转方向的差异预示了两地区间存在左旋错动。
The opposite rotation direction implies the existence of left lateral dislocation between Qaidam basin and Jiuquan and Subei areas.
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