摘要
鄂西渝东地区地质条件复杂,地层产状变化大,局部构造褶皱强烈多变。针对鄂西渝东地区的复杂高陡构造,以地层倾角测井技术对其进行了精细构造解释,并与地震解释剖面相结合和对比,精确地揭示高陡构造中地层的变化。
In west Hubei and East Chongqing,geological conditions are complex,formation occurrence changes a lot and local structure is intensely folded and changeable.Aiming at the characteristics of complex and steep structure,this paper interprets the fine structure of the areas by using formation dip logging and reveals accurately stratigraphic changes in high steep structure by contrast to seismic section interpretation.
出处
《江汉石油职工大学学报》
2011年第6期10-12,23,共4页
Journal of Jianghan Petroleum University of Staff and Workers
关键词
鄂西渝东地区
地层倾角测井
高陡构造
地震剖面
West Hubei and East Chongqing
Formation Dip Logging
High Steep Structure
Seismic Section
