1.Study shows that the Ordovician carbonate formation in this area has the characteristic of very low groundmass porosity.
明确了研究区奥陶系储层为超低基质孔的致密碳酸盐岩,岩溶作用为本区储层发育的主控因素。
2.Study shows that the Ordovician carbonate formation in this area has the characteristic of very low groundmass porosity.
明确了研究区奥陶系储层为超低基质孔的致密碳酸盐岩,岩溶作用为本区储层发育的主控因素。