Residual original intergranular pore developed during early diagenesis of sandstone,secondary pore was created by dissolution in late diagenesis.

 
  • 成巖早期膠結作用形成剩余原生粒間孔,晚期的溶蝕作用形成次生孔隙。
今日熱詞
目錄 附錄 查詞歷史
国内精品美女A∨在线播放xuan