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It is shown that in the basins in the Eastern China, onshore and offshore, the formation of CO2 reservoir is crust-sourced and crust-mantal-mixed-sourced, mainly controlled by local activity of hot fluid into the mud diapir area in multi-phase and multi-zones in physical-chemical mechanism of very thick marine calcareous sandstone and mudstone of Pliocene-Miocene. The volcano- and mantle-sourced CO2 in the Qiongdongnan Basin and Pearl River Mouth Basin is mainly controlled by magmatism and major faults which cut through the basements and link to the mantle gas.

研究表明,中国东部陆相断陷盆地与东海陆架盆地及南海北部陆架琼东南盆地东部和珠江口盆地的CO2气藏及高含CO2油气藏中CO2均属典型的火山幔源型成因,主要受控于幔源型火山活动脱气与沟通深部气源的基底深大断裂的导气配置作用,其运聚富集规律及控制因素与幔源型火山活动及深大断裂的发育展布密切相关,CO2气源主要来自地壳深部幔源火山活动所脱出的大量原始CO2;南海北部陆架西区莺歌海盆地CO2气藏及中国东部陆相断陷盆地部分高含CO2油气藏中CO2,则属于壳源型及壳幔混合型成因,CO2形成及运聚成藏,主要受控于火山侵入活动对碳酸盐岩的烘烤和泥底辟热流体晚期分层分块多期的局部上侵活动与沉积巨厚的海相含钙砂泥岩的物理化学综合作用,其运聚分布规律具多期和分层分区的特点。

The source rocks of the former are mainly the well-developed, huge thickness of Neogene marine depression sedimentary rocks and Miocene marine sedimentary rocks; those of the latter are significantly the rift sediments of Paleogene continental facies, and large-scale source rocks of medium-deep lacustrine facies and inshore paludal facies with coal measure strata well-developed.

根据南海北部边缘新生代沉积盆地结构、构造特征可将其划分为走滑伸展型和断陷裂谷两大类型,前者以新近系巨厚海相坳陷沉积及海相中新统烃源岩发育为突出特点,后者则以古近系陆相断陷裂谷沉积和大规模中深湖相烃源岩、近海沼泽相煤系烃源岩发育为主要特征,这些烃源岩的发育展布规律、有机质丰度和生烃母质类型、成熟演化特点以及生烃潜力等均差异较大。

On the basis of analyzing the forming conditions, establishing reservoir forming pattern of vertical migration-fault sealing, developing petroleum reservoir types of fault sealing and fault together with anticline, it is pointed out that the traps near the deep depression and non-piercement salt dome should be the first choice of exploration target area.

在对该区油气成藏条件分析基础上,建立了研究区盐上层系垂向运移-断层封堵型成藏模式,形成断层遮挡型及断层与背斜组合型两种油藏类型,并指出距离盐上深洼陷较近的、盐丘非刺穿构造上的圈闭是首选的勘探目标区。

According to the ecologic and sedimentary features, the Late Permian biota and strata of south Guizhou can be grouped into the "shallow platform type"and "sub byssal aulacogen type".

根据生态环境和沉积环境的差异,黔南晚二叠世生物群和地层可分出两种类型:&浅海台地型&和&次深海裂陷槽型&,后者为深水型。

Results Among the three groups,the children's rib cartilage had the most blood vessels,the most chondrocytes,well-distributed stain of matrixes,and the type Ⅱ collagen was expressed actively and highest in photedensity.The rib cartilage of teenager group had less blood vessels,unhomogeny distributed stain of matrixes,the enlarged and separated cartilage lacunas.The rib cartilage in adult group showed the least blood vessels,the least chondrocytes.the hyalinization of perichondium,the most deposition of calcium salt,and the type II collagen was expressed at the lowest level in photodensity.

结果 儿童组肋软骨膜血管最丰富,软骨基质染色均匀,软骨细胞数目最多,Ⅱ型胶原蛋白表达最活跃,平均积分光密度值最高;青少年组软骨膜内血管减少,软骨基质染色出现明显的不均质状,软骨陷窝体积变大,并呈分隔状,陷窝内软骨细胞数目减少,II型胶原蛋白表达较儿童组减弱;成人组软骨膜血管、细胞成分明显减少,软骨膜内的纤维成分明显玻璃样变,钙盐沉积较青少年组时明显增多,Ⅱ型胶原蛋白表达较青少年组减弱。

Meanwhile, based on the features of nonmarine basin, sequence stratigraphic models of depression and faulted depression are built, so they supply useful theoretical guidance for exploration of oil and gas.

本文引入新的概念和方法,同时根据陆相盆地特特建立了陆相坳陷盆地地层序模式及陆相断陷盆地中陡坡型和缓坡型两类地层层序模式,为油气勘探提供有用的理论指导。

Among above deformation, the thrust-fold structure formed in Triassic established the E-W trend framework controlling the distribution of the late compressive settling. The NNE-NE trend obduction zone and regional folds is contributed to effect of Tethys tectonic region superimposed by Paleo-Pacific tectonic region.

其中三叠纪挤压变形产生的冲断—褶皱构造,奠定了本区中生代近东西向构造格局,并控制后期挤压坳陷型盆地的的空间展布规律;晚侏罗世早期挤压形成的北北东—北东向逆冲推覆构造带和区域性褶皱是特提斯构造域与古太平洋构造域共同叠加的结果。

Further more, except the detachment-type fold in depression formation, the inversion structural styles can be subdivided into five types: reviving type, forward-expanding type, backward-expanding type, tyrannizing type and truncated type according to the mode of association of the thrust faults and the early normal faults.

进而将反转构造样式除坳陷层滑脱褶皱外,依据反转过程中形成的逆断层与早期伸展断层的组合关系归纳为五种类型:复活型、前展型、后展型、欺压型、截断型。

It is considered that the Tertiary unconformity in Jiyang Depression can be divided into three types: typeⅠ1, typeⅠ2 and typeⅡ. Unconformity generally consists of weathered clay, semi-weathered rock and unweathered rock.

研究认为济阳坳陷第三系不整合可划分为三类:Ⅰ1型结构、Ⅰ2型结构和Ⅱ型结构,完整的不整合结构包括风化粘土层、半风化岩石、未风化岩石。

Aimed at the exploration of the lithostratigraphic reservoirs in four types of prototype basins(onshore terrestrial rifts,depressions,forelands and marine kratons)and in glutenites,volcanics and fracture-vug carbonate rocks,significant results are achieved on geological theory,technological innovation and production efficiency through fi...

针对中国陆上陆相断陷、坳陷、前陆和海相克拉通等4类原型盆地和砂砾岩、火山岩、缝洞型碳酸盐岩储集体中岩性地层油气藏的勘探,通过5年系统研究,在地质理论、技术创新与生产实效等方面取得重大成果:①系统建立了4类盆地岩性地层油气藏地质理论;②创建了中低丰度岩性地层油气藏大面积成藏理论;③创新了系统的岩性地层油气藏勘探程序与技术系列,自主创新21项核心专利;④推动了中国陆上由勘探构造油气藏向勘探岩性地层油气藏的重大转变,使中国石油天然气股份有限公司大规模岩性地层油气藏勘探取得显著成效。

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