secondary porosity meaning in Chinese
次级孔隙
次生孔隙度
次生孔隙率
Examples
- The diagenetic environment results in different water - rock reaction and development of secondary porosity
成岩环境在一定程度上影响了水岩反应及次生孔隙发育。 - They changed the porosity characteristics of sandstone , engendering new benefit storing beds consisted with secondary porosity
浊沸石矿物是长6砂岩中普遍的胶结物，它的形成与火山物质水化有关。 - Dissolition is favorable for secondary porosity , thus forming available reservoirs in some sections of low porous and low permeable clastic rocks
从而使某些砂岩段在低孔低渗储层中形成较发育的次生溶蚀孔隙和成岩微裂缝，并成为有效孔隙。 - At the late diagenesis phase , the dissolution of frame grains , especially the dissolution of felspar and laumontite , is the key to form secondary porosity
朵状砂体的大小直接控制油藏的范围及规模，靖安地区的主要油藏多沿不同的朵状体成排分布。 - During diagenetic process , the main factor destroying porosity is function of pressure and cementation . secondary porosity formem formed by unsteady mineral is beneficial to formation ' s development
成岩作用中，压实作用、胶结作用、自生粘土矿物的沉淀是破坏孔隙的主要因素；不稳定矿物溶蚀形成的次生孔隙有利于储层的发育。