次生灰巖 的英文怎麼說
中文拼音 [cìshēnghuīyán]
次生灰巖
英文
secondary limestone-
Several analysis methods such as casting slice, scanning electron microscope, porosity and permeability data, mercury injection data and density of fissures are used to study the reservoir properties of volcanic rocks in huang - yu - re area, the east sag of liaohe basin. volcanic rocks in this area are mainly composed of basalt, diabase, tuff and trachyte. the dominating type of volcanic reservoir space includes secondary solution pores and structural fissures
通過火山巖的常規物性分析壓汞分析和裂縫密度分析，結合鑄體薄片和掃描電鏡，研究了遼河油田黃于熱地區的火山巖儲層物性特徵，認為該區火山巖儲層巖石類型主要有玄武巖輝綠巖凝灰巖和粗面巖，主要儲集空間類型為次生的構造裂縫和溶蝕孔縫。They are free of turbidity, except in some limestone areas and volcanic areas with high secondary permeability where large underground rivers occur.
它們不至於渾濁、只是在灰巖地區和火山地區具有高的次生滲透性並存在大地下河時除外。The great number of pores of reef rocks disappeared due to multi - generational cementation in submarine and taphonomic environments. the pores in reef rocks are mainly secondary and the primary pores are almost filled up. the evolution of pores is wholly controlled by diagenesis, all in a word, the histoty of diagenesis is evolution of pores
礁灰巖中的大量孔隙被海底和埋藏成巖環境中多期膠結物充填而喪失，孔隙類型以次生孔隙為特徵，原生孔隙基本被填實，孔隙演化完全受成巖作用的控制，成巖作用的發展史就是孔隙的演化史。Induced porosity is typified by fracture development as found in some shales and limestones and by the rugs or solution cavities commonly found in limestones
次生孔隙度是以某些頁巖和石灰巖的裂縫和石灰巖中的巖穴和溶洞為代表。分享友人