1) Overpressured basin
超压盆地
1.
Relationship between excess-pressure gradient and gas accumulation in overpressured basin;
超压盆地内剩余压力梯度与天然气成藏的关系
2.
The compacting processes in impermeable mudstones of overpressured basin can be classified into two stages,i.
超压盆地泥岩的压实演化可划分为两个阶段，即连续压实和幕式压实阶段，其中幕式压实阶段又可根据导致流体压裂的主控因素进一步划分为两个亚阶段，即水力压裂和生烃压裂，前者主要由于泥岩欠压实和新生流体源的增压所致，后者则主要由于泥岩中有机质生烃及烃类裂解后增压所致。
2) strong overpressured sedimentary basin
强超压盆地
3) Overpressured fluid system
盆地超压流体系统
4) superbasin
超级盆地
5) Compressional basins
挤压盆地
6) compressional basin
压性盆地
1.
According to the basic concepts of sequence stratigraphy and the controlling factors of compressional basin,dual features of sequence were found and sequence stratigraphy framework of Bohu depression was set up,based on an integrated investigation of well logs,seismic data,cores and outcrops.
将层序地层学基本原理与压性盆地控制因素相结合,通过各种地质、钻井、测井和地球物理等资料的综合分析,建立了焉耆盆地博湖坳陷前陆盆地层序地层格架,综合分析前陆盆地挤压构造背景下层序结构的二元性特征,并在此基础上建立起博湖坳陷侏罗系的层序发育模式,分析了二元性层序发育机理。
补充资料：冲击波超压与动压