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三塘湖盆地南缘冲断带位于中央坳陷带以南,以南缘逆冲推覆断裂带为界与中央坳陷带分隔,紧邻条湖、马朗两大生油气凹陷,发育多套储盖组合。逆冲推覆断裂带的形成主要受控于晚海西运动和晚燕山运动,逆冲推覆断裂带下盘发育石板墩、黑墩两个构造带。目前,已发现黑墩P2l、石板墩C2k和西峡沟M4-T14区块J2X等多层系油气藏,证实其为一复式油气聚集带。构造、岩性、裂缝和火山岩体控制了油气藏的形成与分布。下一步应积极拓展南缘冲断带二叠系裂缝型油气藏,加强古生界火山岩油气藏勘探,同时兼顾中生界砂岩油气藏勘探.勘探思路应从构造控油打高点向岩性控油打河道、裂缝控油打破碎带、火山岩体控油打火山体转变。 相似文献
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吐哈盆地水动力类型为重力流盆地,主要供水区是盆地北部博格达山,区域水压头高程呈现北高南低、地层水水势梯度东弱西强的特点,最小水压头高程与白垩纪至第四纪沉降中心的迁移相一致,从东向西由红台地区的洼陷中央逐渐过渡到西部的艾丁湖南斜坡。油气富集规律受控于水动力势场及地层水与地表水的交替区带,油气富集区与水动力低势区完全吻合:小草湖洼陷分布于东南斜坡区,丘东洼陷富集于南斜坡,胜北洼陷则分布于南部和西南部。油气藏形成后同样受水动力场的影响,使油气分布进行调整、再分配,或被地表水驱替而遭破坏。坳陷西南部艾丁湖斜坡区(鲁西低凸起)是水动力低势区,可能是形成岩性地层油气藏的有利场所。 相似文献
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Cubic NaYF4:yb3+(20%)/Er3+(1%) microspheres were synthesized by EDTA-assisted hydrothermal method. Under 980 nm exci-tation, ultraviolet (4G11/2→4I15/2), violet (2H9/2→4I15/2), grogn (4F7/2→4I15/2, 2H11/2→4I15/2, and 4S3/2→4I15/2), and red (4F9/2→4I15/2) upconversion fluorescence were observed. The number of laser photons absorbed in one upconversion excitation process, n, was determined to be 3.89, 1.61, 2.55, and 1.09 for the ultraviolet, violet, green, and red emissions, respectively. Obviously, n=3.89 indicated that a four-photon process was involved in populating the 4G11/2 state, and n=2.55 indicated that a three-photon process was involved in populating the 4F7/2/2H<11/2>4S3/2 levels. For the violet and red emissions, the population of the states 2H9/2 and 4F9/2 separately came from three-photon and two-photon proc-esses. The decrease of n was well explained by the mechanism of competition between linear decay and upconversion processes for the de-pletion of the intermediate excited states. 相似文献
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吐哈盆地台北凹陷深层含油气前景 总被引:1,自引:1,他引:0
吐哈盆地台北凹陷内二叠、三叠系两套烃源岩厚度大且分布稳定、具备良好的生烃条件, 发育三套生储盖组合, 以上二叠统为生油层,中、上三叠统为储油层的生储盖组合最为有利, 而南部辫状河三角洲砂体是主要的储集体类型;下侏罗统存在两套局部储盖组合,其圈闭分布与二叠、三叠系的圈闭分布基本一致。综合评价认为:鄯善孤形带、红连区带、葡北带和北部山前带是台北凹陷开展深层油气勘探的有利区带。 相似文献