CAJ | 학술논문

中-晚中新世，中卢卡尼亚盆地以发育碳酸盐岩建隆为特征，碳酸盐岩建隆的生长主要受控于构造活动强度、古地貌、海平面变化及陆源碎屑物质的输入：1)中-晚中新世，盆地稳定的构造背景有利于碳酸盐岩建隆的生长；2)渐新世-早中新世，伸展、走滑作用形成的北东-南西向地堑、地垒构造控制了碳酸盐岩建隆的类型和分布；3)海平面周期性升降影响碳酸盐岩建隆生长的旋回性；4)中中新世晚期、晚中新世和上新世，由盆地南缘、东南方向输入的陆源碎屑物质，抑制了碳酸盐岩建隆的生长，并使得其储集物性出现平面上的差异。最后，分析了碳酸盐岩建隆的油气储盖组合特征及其内部油气聚集影响因素。
중-만중신세，중로잡니아분지이발육탄산염암건륭위특정，탄산염암건륭적생장주요수공우구조활동강도、고지모、해평면변화급륙원쇄설물질적수입：1)중-만중신세，분지은정적구조배경유리우탄산염암건륭적생장；2)점신세-조중신세，신전、주활작용형성적북동-남서향지참、지루구조공제료탄산염암건륭적류형화분포；3)해평면주기성승강영향탄산염암건륭생장적선회성；4)중중신세만기、만중신세화상신세，유분지남연、동남방향수입적륙원쇄설물질，억제료탄산염암건륭적생장，병사득기저집물성출현평면상적차이。최후，분석료탄산염암건륭적유기저개조합특정급기내부유기취집영향인소。
During the Middle-Late Miocene, the Central Luconia Basin was characterized by the extensive development of carbonate buildups. Tectonic activity strength, palaeogeomorphology, sea level alternation and the influx of terrestrial material dominated the development of carbonate buildups. 1) The basin remained stable throughout the Middle-Late Miocene, thereby facilitating carbonate deposition. 2) From Oligocene to the Early Miocene, due to extensional and strike-slip tectonics, it was formed in this area the NE-SW trending graben and horst which dominated the type and distribution of carbonate buildups. 3) The cycle of carbonate buildup growth was related to the cycle change of sea level. 4) From the late stage of the Middle Miocene to Pliocene, terrestrial materials migrated from the south and southeast of the basin, suppressed the growth of carbonate buildups, resulting in the plane difference of reservoir physical property. Finally, the reservoir-cap combination features and the controlling factors for petroleum accumulation in carbonate buildups were analyzed.