研究表明这些深水沉积应是活跃的构造作用的响应，对认识三江地区的构造活动具有指示意义。
The deep_water sediments seem to be the response to active tectonics, and hence are of indicating significance to trace tectonic activity in Three_River area.
其储层特征主要受到沉积、成岩和构造作用的控制。
Moreover, the reservoir characteristics are determined by deposition, diagenesis and tectonism.
现在主要的储集空间为沉积后的构造作用形成的裂缝以及沿着这些裂缝发育的溶蚀孔、洞、缝。
As the present, the main reservoir space is the crack because of the tectonism and the hole or corrosion hole what growth along these crack.
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