临清坳陷东部石炭—二叠系二次生烃差异性研究  

Study on Differentiation of Secondary Hydrocarbon Generation for the Carboniferous-Permian Source Rocks in the Eastern Linqing Depression

作　　者：陈武珍[1] 陈红汉[1,2] 李文涛[3] 丰勇[2] 宫雪[1] 熊万林[1] 

机构地区：[1]中国地质大学(武汉)资源学院石油系,武汉430074 [2]中国科学院地质与地球物理研究所兰州油气资源研究中心,兰州730000 [3]中国石油化工股份公司胜利油田分公司地质科学研究院,山东东营257015

出　　处：《沉积学报》2012年第1期179-188,共10页Acta Sedimentologica Sinica

摘　　要：受盆地多旋回叠加和反转演化控制,临清坳陷东部石炭—二叠系含煤系地层烃源岩经历了二次生烃过程,并在空间上表现出强烈的差异性。通过对这套烃源岩生烃史模拟结果表明,石炭—二叠系烃源岩于早中三叠世进入生烃门限,随后印支运动造成全区生烃中止,中新生代烃源岩再次深埋,发生二次生烃作用。不同井区二次生烃在时间和空间上存在差异性,洼陷带发育三个"二次生烃"阶段,生烃高峰期发生在新生代,凸起带发育两个"二次生烃"阶段,生烃高峰期发生在中生代,隆起区尚未发生二次生烃。二次生烃早期生成的烃类基本遭受破坏,晚期生成的烃类具备成藏条件,是勘探的主要目标。现今洼陷带烃源岩已进入成熟—高成熟阶段,成为晚期煤成气藏的气灶。Controlled by the multi-cycle superposition and reverse evolution of basin,the source rocks of Carboniferous-Permian coal-bearing strata has experienced secondary hydrocarbon generation in the eastern Liqing Depression,which shows a strong deviation in the space.The simulation results of hydrocarbon generating history of these source rocks show that,the Carboniferous-Permian source rocks entered the hydrocarbon generation window in the Early-Middle Triassic,then the hydrocarbon generation suspended in the whole region due to the Indosinian movement,after that the source rocks buried again in the Meso-Cenozoic and secondary hydrocarbon generation function occurred.The secondary hydrocarbon generation varies with different well blocks in the time and space.There are three secondary hydrocarbon generation stages in sags,first stage was in the Cretaceous period,second stage was in the Paleogene period,and third stage was in the Neogene period,the peak amount of hydrocarbon generating stage was in the Cenozoic period.Hydrocarbon contribution at the three secondary hydrocarbon generation stages was equivalent to about thirty percent in sags that the Paleogene was relatively thin.While sags that the Paleogene was relatively thick,hydrocarbon contribution in the Paleogene period was the most,which was more than fifty percent,then followed by the Cretaceous period,and hydrocarbon contribution in the Neogene period was the least.There are two secondary hydrocarbon generation stages in prominence,peak amount of hydrocarbon generating stage was in the Mesozoic period.Hydrocarbon contribution in the Cretaceous period was more than ninety percent.There are none secondary hydrocarbon generation stages in uplift.Most of the hydrocarbon that generated early period has been destroyed,while the hydrocarbon which generated late period is available on the geological conditions of hydrocarbon accumulation,this is a main target of oil and gas exploration.Differential subsidence is the main controlling factor of the differentiation of s

关 键 词：煤系烃源岩 二次生烃 多旋回叠合盆地 临清坳陷东部 

分 类 号：TE122.113[石油与天然气工程—油气勘探]