1) shale-fractured reservoirs
裂缝性泥质岩油藏
1.
A study of shale-fractured reservoirs in Zhanhua sag;
沾化凹陷裂缝性泥质岩油藏研究
2) fractured mudstone reservoir
泥质岩裂缝油气藏
1.
Almost all fractured mudstone reservoirs found both in and outside China are distributed in source rocks which are mainly composed of mudstones and shales, abundant in organic matter, calcareous and siliceous minerals.
目前国内外发现的绝大多数泥质岩裂缝油气藏都分布在以暗色泥岩及页岩为主的生油岩中 ,常富含有机质、钙质或硅质矿物 ,其有机碳丰度一般为 1 0 ～ 2 0 ,有机质类型多样 ,镜质体反射率多在 0 5 ～ 1 3 。
3) Fracture shale reservoir
裂缝性泥岩油气藏
4) fractured shale reservoir
泥岩裂缝油气藏
1.
Study on fractured shale reservoirs in Liaohe Basin;
辽河断陷盆地泥岩裂缝油气藏研究
5) fractured mud reservoir
泥岩裂缝油藏
1.
An overall analysis of multi-f ractal spectrum be-haviour of fau1t system in each part says that high value zones of multi-f ractal spec-trum f(a) and a have obvious c0rrelation with fractured mud reservoir.
在对松辽盆地北部齐家一古龙地区泥岩裂缝油藏形成机理进行研究的基础上，应用多重分形理论计算了该区地反射层在不同区域内断裂体系的多重分形谱f（a）。
6) fractured sandstone reservoir
裂缝性砂岩油藏
1.
Water-flooding performance of fractured sandstone reservoirs;
裂缝性砂岩油藏的水驱动态规律
2.
In the analysis and prediction of water-drive performance of sandstone reservoirs, its characteristic curves are widely used in study and application, the special forms of fractured sandstone reservoir permeability are used to derive analytical expressions for its characteristic curves of sandstone reservoirs, and the responding theoretical curves are calculated.
利用裂缝性砂岩油藏相对渗透率的特殊形式,根据双重介质两相渗流理论推导出了裂缝性砂岩油藏水驱特征曲线的解析表达式,并计算了相应的理论曲线。
3.
Based on the characteristics of fractured sandstone reservoir,equivalent continuum model for simulating fluid flow is put forward.
为了研究裂缝性砂岩油藏中油水渗流规律以及裂缝对油田开发的影响,利用岩石薄板模型,对6种不同裂缝形态下平行裂缝对水驱油过程进行了物理模拟,通过对水驱油效果的分析比较,得出了不同裂缝形态下水驱油渗流规律;根据裂缝性砂岩油藏的储层特点,建立了裂缝性砂岩油藏渗流等效连续介质模型,利用数值模拟的手段,研究了裂缝性砂岩油藏水驱油特征以及裂缝形态对开发的影响;通过物理模拟和数值模拟结果的对比,验证了等效连续介质模型在裂缝性砂岩油藏渗流模拟中的适用性。
补充资料：泥质岩
| 泥质岩 argillaceous rocks 含有大量粘土矿物，且粒径小于0.0039毫米的沉积岩。又称粘土质岩。包括泥岩、粘土岩、页岩、板岩等。因形成条件不同，有白、灰白、灰、黄、绿、红褐、棕等各种颜色。常见胶状、豆状、鲕粒状结构和鳞片状、毡状、格子状构造。主要由粘土矿物（高岭石、埃洛石、蒙脱石、水云母、海泡石等）、碎屑矿物（石英、长石、云母等）和某些自生非粘土矿物（铁、锰的氧化物、氢氧化物和碳酸盐矿物等）组成。依混入物可分为粉砂泥质岩、砂质泥质岩等；依粘土矿物，可分为高岭石泥质岩、蒙脱石泥质岩、水云母泥质岩等。泥质岩是沉积岩中分布最广的一类岩石，约占沉积岩总面积的60％。泥质岩具有可塑性、耐火性、烧结性、干缩性、吸附性、吸水膨胀性等特点，被工业部门广泛利用。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条