›› 2013, Vol. 34 ›› Issue (6): 1-1.

• 论文 •    

南堡凹陷不整合类型及剥蚀量恢复

彭清华1,周江羽2,蒋少斌3a,王玉梅3b,马月琴3b   

  1. (1.中国地质调查局 成都地质矿产研究所,成都 610081;2. 中国地质大学 资源学院,武汉 430074;3.中国石油 新疆油田分公司 a.监理公司;b.实验检测研究院,新疆 克拉玛依 834000)
  • 出版日期:2019-01-01 发布日期:1905-07-14

Unconformity Types and Erosion Thickness Restoration in Nanpu Sag, Huanghua Depression, Bohai Bay Basin

PENG Qinghua1, ZHOU Jiangyu2, JIANG Shaobin3a, WANG Yumei3b, MA Yueqin3b   

  1. (1.Chengdu Institute of Geology and Mineral Resources, China Geological Survey, Chengdu, Sichuan 610081, China; 2.Faculty of Resources, China University of Geosciences, Wuhan, Hubei 430074, China; 3.PetroChina Xinjiang Oilfield Company, a.Supervision Company, b.Research Institute of Exploration and Development, Karamay, Xinjiang 834000, China)
  • Online:2019-01-01 Published:1905-07-14

摘要: 南堡凹陷经历了多幕拉张沉降和抬升剥蚀旋回演化历程,形成了6个区域性的不整合,按形态和成因可划分为平行不整合和削截不整合2大类;新生界底部、沙一段底部、东营组底部、馆陶组底部不整合为构造削截不整合;石炭系底部、中生界底部不整合为平行不整合。研究区不整合对油气成藏的控制作用主要表现在储集层改造、充当油气运移通道、封盖性等3个方面。利用镜质体反射率趋势线法对高尚堡地区东营组剥蚀量进行了恢复,结合泥岩声波时差和地层对比法,恢复了南堡凹陷其他地区东营组的剥蚀量。研究发现南堡凹陷东营组的剥蚀强度大致可分为2个区:东北部的强剥蚀区和中北部的弱剥蚀区。总体上,南堡凹陷东营组普遍遭受剥蚀,构造高部位剥蚀量大,中心凹陷区域剥蚀量小。

Abstract: Nanpu sag underwent multi?stage extensional subsidence and uplifting?erosion cycle evolution, formed six regional unconformities, which can be divided into two categories: parallel unconformity and truncation unconformity. The former includes the Carboniferous bottom and the Mesozoic bottom unconformities; the latter includes the Cenozoic bottom, the Shahejie formation member?1 bottom, the Dongying formation bottom and the Guantao formation bottom ones. The control effects of these unconformities on hydrocarbon accumulation in the study area are mainly manifested in the following three aspects: reservoir reconstruction, as the oil and gas migration channels and sealing. Vitrinite reflectance trend line method is used to recover the erosion thickness of Dongying formation in Gaoshangpu area, Combined with interval transit time method and stratigraphic correlation method, the erosion thickness of Dongying formation in other areas of Nanpu sag has been recovered. The study shows that the erosion intensity of Dongying formation in Nanpu sag could be divided into two districts: the strong erosion district in the northeast part and the week erosion district in the north?central part. Overall, the Dongying formation in Nanpu sag has suffered from erosion, its structural high is big, and its central sag area is small in denudation quantity

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