摘要
Based on the analysises of regional structural setting, basin formation and deformation, this paper demonstrates that the Xianfeng basin has been formed and inverted under the strike-slip regime. The article is a partial result of the whole research.
Based on the analysises of regional structural setting, basin formation and deformation, this paper demonstrates that the Xianfeng basin has been formed and inverted under the strike-slip regime. The article is a partial result of the whole research.
关键词
云南
煤层
盆地
小江断裂带
成盆构造特征
地层构造
strike-slip fault, basin formation, structural inversion, brown coal basin
