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horizontal transportation
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  横向输导
    The fault systems, unconformity surfaces, interconnecting pore systems and diapir structures constitute the complex network system of vertical and horizontal transportation within the depression.
    中部弱超压和深部强超压3部分组成,断裂系统、不整合面和相互连通的孔隙系统及底辟构造组成了凹陷内流体纵、横向输导的复杂网络系统;
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  horizontal transportation
Transect observation at the littoral zone suggested that horizontal transportation may be a reason for the high methane concentration in epilimnion and thermocline at the offshore area.
      


Fluid dynamical fields in Damintun Depression, Liaohe Basin show that: the paleogeothermal gradient in the study area is greater than present one; the mudstone compaction could be classified into three types such as normal compaction-normal pressure, uncompaction-low overpressure in single interval, and uncompaction-high overpressure in double intervals. The present profile pressure system consists of normal pressure, slight overpressure and intense over-pressure from top to bottom. The fault systems, unconformity...

Fluid dynamical fields in Damintun Depression, Liaohe Basin show that: the paleogeothermal gradient in the study area is greater than present one; the mudstone compaction could be classified into three types such as normal compaction-normal pressure, uncompaction-low overpressure in single interval, and uncompaction-high overpressure in double intervals. The present profile pressure system consists of normal pressure, slight overpressure and intense over-pressure from top to bottom. The fault systems, unconformity surfaces, interconnecting pore systems and diapir structures constitute the complex network system of vertical and horizontal transportation within the depression. Pressure evolution can be divided into two stages of initial overpressure accumulation and overpressure expulsion , and faults had an important controlling role to the formation, evoltution and distribution of the pressures. The fluid potential energy in profiles present a "double-layer" structure, and the depocenter was the fluid supply area whereas the slope was the main fluid dischareg area.

辽河盆地大民屯凹陷的地下流体动力场特征表明该区古地温梯度大于今地温梯度,泥岩压实可划分为正常压实-常压型、单段欠压实-弱超压型和双段欠压实-强超压型3大类;现今剖面压力系统由浅部正常压力。中部弱超压和深部强超压3部分组成,断裂系统、不整合面和相互连通的孔隙系统及底辟构造组成了凹陷内流体纵、横向输导的复杂网络系统;古压力场演化经历超压原始积累和释放2大阶段,断层对压力的演化与分布起重要的控制作用;流体势在剖面上呈“双层”式结构,洼陷为供流区,斜坡带为主要泄流场所。

 
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