Editorial office of ACTA PETROLEI SINICA ›› 1994, Vol. 15 ›› Issue (2): 39-47.DOI: 10.7623/syxb199402005

• Petroleum Exploration • Previous Articles     Next Articles

STRUCTURAL FEATURES,EVOLUTION AND OIL AND GAS PROSPECTS OF KAI FENG DEPRESSION

Wang Dingyi1, Tang Xiyuan1, Chen Naiming2   

  1. 1. Northwest University;
    2. Zhongyuan Petroleum Exploration Bureau
  • Received:1992-11-04 Revised:1993-06-12 Online:1994-04-25 Published:2013-07-08

开封坳陷构造特征、形成演化与油气远景

王定一1, 汤锡元1, 陈乃明2   

  1. 1. 西北大学;
    2. 中原石油勘探局
  • 作者简介:王定一,1934年5月生.1955年毕业于西北大学.现任西北大学地质系副教授.通讯处:陕西省西安市.邮政编码:710069.

Abstract: Kaifeng depression,situated in the northern part of the southern North China basin,mainly extending in NWW direction structurally and in the NNE-NE directions in some segments,is a fault-subsided Meso-Cenozoic depression. Its formation was resulted from theNWW faulting with sinistral shear-extensional movement and the NNE-NE faulting withdextral shear-extensional movement,which occurred in the late stage of the early Cretaceous,through the late stage of the Palaeocene and the Eocene.16 wells have been drilled in the depression,4 source bed systems of-O,C-P,J-K andE have been identified.Petroleum resource evaluation showed that there are geological conditions for only small-sized pools in Meso-Cenozoic,and for larger sized pools in Palaeozoic.

Key words: sag, structure, tectonic movement, evaluation of oil and gas resources

摘要: 开封坳陷是南华北盆地北部一个主要呈NWW向展布,而局部地段NNE-NE向构造格局又具明显优势的中新生代断陷型勒陷.其形成是由于早白垩世晚期、古新世晚期到渐新世发生的NWW向断裂作左行剪切拉张平移运动与NNE-NE向断裂作右行剪切拉张平移运动联合作用的结果.该坳陷共发现了-O、C-P、J_3-K_1和E四套生油层系.油气资源评价表明,中新生界仅具有形成小型油气藏地质条件,而古生界具有形成较大型的油气藏地质条件.

关键词: 坳陷, 构造, 构造运动, 油气资源评价