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Characteristics and distribution of tertiary algal limestones reservoirs in Qaidam basin

机译:柴达木盆地三级藻类石灰岩水库的特点及分布

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Tertiary algal limestones reservoirs in Qaidam basin are characterized by wide distribution and being the most important in carbonates reservoirs. Tertiary algal limestones reservoirs in western Qaidam basin have been found in YUEXI, YUEDONG, SHIZIGOU, HUATUGOU and NANYISHAN regions etal, and distributed from E_3~2 to N_2~2. Algal limestones reservoirs in upper member of XIAGANCHAIGOU formation(E_3~2) have been found in YUEXI and YUEDONG regions, those in SHANGGANCHAIGOU formation(N_1) have been found in SHIZIGOU and HUATUGOU regions, those in XIAYOUSHASHAN formation(N_2~1) and SHANGYOUSHASHAN formation(N_2~2) have been found in NANYISHAN region. Algal limestones reservoirs in E_3~2 and N_1distributed mainly to west (southwest) region of YINGXIONGLING depression, those in N_2~1 and N_2~2 distributed mainly to east(northeast) region of YINGXIONGLING depression. Distribution of algal limestones in Qaidam basin is mainly controlled by lake level changes. The types of tertiary algal limestones in Qaidam basin are mainly composed of algal masses limestone, algal laminar limestone, algal stromatolithic limestone, algal micrite limestone and algal oosparite. Algal limestones reservoirs spaces are predominant with solution pores, solution fissures and mold pores. They are possibly controlled by atmospheric water solution and subsurface organic acid solution. Algal masses limestone, algal laminar limestone and algal stromatolithic limestone are favorable reservoirs, algal micrite limestone and algal oosparite are the secondary. Algal limestones reservoirs in YUEXI and YUEDONG regions are the best,average porosity is 20-30%, average permeability is near 100md.Algal limestones reservoirs in NANYISHAN region are the secondary, average porosity is 13-18%, average permeability is 1-10md.Algal limestones reservoirs in HUATUGOU and SHIZIGOU regions are the worst, average porosity is 8-15%,average permeability is 1-10md.
机译:柴达木盆地第三藻灰岩储层特征是广泛分布并且是在碳酸盐储层最重要的。在柴达木盆地西部第三系藻灰岩油藏已在岳西,粤东,狮子沟,花土沟和南翼山地区被发现等人,并从分布E_3〜2 N_2〜2。藻灰岩中的干柴沟(E_3〜2)在岳西和粤东区域已经发现上部构件水库,那些在干柴沟组(N_1)已在狮子沟和花土沟区域发现,那些在XIAYOUSHASHAN形成(N_2〜1)和SHANGYOUSHASHAN形成(N_2〜2)已经在南翼山区域被发现。藻灰岩油藏E_3〜2 N_1distributed主要是西部英雄岭抑郁症(西南)区域,那些N_2〜1和N_2〜2主要分布于英雄岭抑郁东(东北)地区。在柴达木盆地藻灰岩分布主要受湖泊水位的变化来控制。在柴达木盆地类型三级藻灰岩主要由藻类群众灰岩,藻灰岩层,藻stromatolithic灰岩,藻泥晶灰岩和藻类oosparite的。藻灰岩油藏空间是主要用溶孔,解决裂缝和模具细孔。它们可能通过大气水溶液和地下有机酸溶液来控制。藻类群众灰岩,藻灰岩层和藻类stromatolithic灰岩有利于水库,藻泥晶灰岩和藻oosparite是次要的。藻灰岩储层岳西和粤东区域是最好的,平均孔隙度为20-30%,平均渗透率接近100md.Algal灰岩在南翼山区域储层是二次,平均孔隙度为13-18%,平均渗透率是1-10md在花土沟和狮子沟区域.Algal灰岩储层是最差的,平均孔隙度为8-15%,平均渗透率是1-10md。

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