冀中坳陷廊固凹陷河西务构造带潜山储集层特征

对渤海湾盆地冀中坳陷廊固凹陷河西务构造带潜山储集层的岩心及地面露头进行了综合研究.潜山储集层的岩性主要是碳酸盐岩,储集空间包括溶孔、溶洞、裂缝和基岩微观孔隙,形成孔-洞型、裂缝型、缝-洞型和孔-洞-缝复合型的碳酸盐岩储集层.区内多期次的古岩溶作用是储集层形成的重要因素之一,古岩溶作用主要发生于沿潜山不整合面的风化淋滤带、水平潜流带、断层裂隙带及顺层层面,形成相应的溶蚀孔洞型储集层.由构造运动所形成的裂缝不仅增加了储集层的孔隙度,还极大地改善了孔洞的连通性,提高了储集层的渗透性能.但不同岩性、不同构造部位储集层的发育程度不同:白云岩类储集层好于灰岩类储集层,无石炭-二叠系覆盖区的储集层好于有石炭-二叠系覆盖区,断层发育区内储集层好干断层不发育区.河西务构造带西南端潜山储集层发育,是有利的油气勘探区块.图4表4参14

Features of buried hill reservoirs in Hexiwu structural belt, Langgu Sag, Jizhong Depression

The buried hill reservoirs of the Hexiwu structure belt in Langgu Sag, Bohaiwan Basin are comprehensively studied by core and outcrop observation. The reservoir lithology is dominantly carbonate rock, and the reservoir spaces include dissolution pores, dissolution cavities, cracks and bedrock micropores, forming pore-cavity type, crack type, crack-cavity type and combination pore-cavity-crack type reservoirs. Multiple-phase fossil karstification is an important factor during reservoir formation. The fossil karst is developed in the leached belt, submerged current belt, fracture belt and bedding direction along buried hill unconformities. The cracks formed by tectonic movement increase porosity, improve connection of pores and cavities and permeability. The reservoirs developed in different lithologies and tectonic positions have different physical properties: dolomite reservoir is better than carbonate reservoir, and reservoir not overlapped by Permo-Carboniferous stratum is better than that overlapped by Permo-Carboniferous stratum, and reservoir in the fault-developed area is better than that in the non-fault-developed area. The buried hill reservoirs in the southwestern Hexiwu structure belt are well developed and are favorable areas for oil and gas exploration.