湿地扇扇中辫状水道沉积微相-岩石相划分方法

综合应用岩心、测井、分析化验等资料,对湿地扇扇中辫状水道粗碎屑沉积特征进行了详细研究,提出了沉积微相-岩石相的划分方法。根据不同岩石相的物性、电性及含油性特征,将扇中辫状水道微相细分为辫状水道砂砾岩相、辫状水道粗砂岩相和辫状水道细砂岩相。研究结果表明,沉积微相-岩石相对油水分布具有明显的控制作用,其中以辫状水道砂砾岩相单井日产油能力最高,辫状水道粗砂岩相次之,辫状水道细砂岩相最低,比较符合油田的开发实际。辫状水道粗砂岩相因物性最好,剩余油丰度高,可作为下一步挖潜的主要目标。     

新疆克拉玛依市生态敏感性研究(英文)

Karamay City is a typical mining city, relying on oilfield exploration and development. After 60 years of construction and development, Karamay has become the first large oilfield and an important base of the national petroleum and petrochemical industry in China. Based on spatial analysis, and Geographic Information Systems (GIS) grid computing and overlay techniques, whilst considering the effect of oilfield development and aimed at the ecological problems of Karamay City in the Xinjiang Uygur Autonomous Region of China, we conducted research on the spatial characteristics of the comprehensive ecological sensitivity of Karamay. The ecological problems of natural environment evolution include soil erosion, land deserti-fication, soil salinization, and biodiversity reduction. The most significant disturbance factor from the activities of humans in this area is oilfield exploitation. This study carries out an analysis of single factor ecological problem sensitivity and integrated ecological sensitivity. The results of the research are as follows: (1) Soil erosion is relatively sensitive, especially in Karamay district, Dushanzi district, north of Urho district and west of Baijiantan district, which is mainly a result of the vertical dropping slopes, serious rainfall erosion and the distribution of scattered woodland. (2) The main types of land desertification are represented by high and moderate grade sensitivities, and high and extremely high sensitive areas are distributed in the intersection of Karamay and Baijiantan districts. This is due to evaporation exceeding rainfall in these areas, and the soil mainly consists of sand and is seldom covered by vegetation. (3) The soil salinizatiion sensitivity grades are mainly moderate, high and extremely high. The highly sensitive areas are mainly distributed in southeast of Baijiantan district, north and east of Karamay district and east of Urho district. The primary causes are evaporation exceeding rainfall and extreme human activities. (4) The main types of biodiversity sensitivity are light and moderate grade. Highly sensitive areas are located in the east and south of Karamay district, north of the Baiyang River basin and parts of the wetland areas. (5) Oil fields development areas are highly ecologically sensitive, which are located in the northern oilfields of Urho district, western oilfields of Baijiantan district, northwestern oilfields of Karamay district and central oilfields of Dushanzi district. (6) The main types of integrated ecological sen-sitivity are high and moderate. The high and extremely highly sensitive areas are located in the central and northern parts of Karamay district, and southwest of Baijiantan district. The evaluation results will provide guidance for the future planning and development, the protection of the ecological environment and the realization of harmonious social, economic, and ecological development in Karamay City.     

砂砾岩储层特征及控制因素:以红山嘴地区三叠系克拉玛依组上段为例

为了有效地在准噶尔盆地红山嘴地区克拉玛依组上段(克上段)寻找有效储集体,利用岩心、铸体薄片、扫描电镜及压汞等资料的综合分析,对研究区的储层特征和储层发育的控制因素进行了研究。结果表明该区克上段储层岩屑含量高,结构成熟度和成分成熟度偏低;分析了控制储层发育的因素,沉积因素(基质含量、岩性及砂砾岩成因类型)是内因,砂砾岩储层中,基质含量与物性成反比;牵引流物性好于洪流型,碎屑流型最差;成岩作用(压实、胶结及溶蚀作用)为外因,压实作用造成砂砾岩孔隙结构变差,胶结作用在富基质和含基质型具有破坏作用,而对于贫基质型起保护作用;通过对砂砾岩储层特征与控制因素综合分析,将研究区的储层分为4类,并绘制了有利储层分布图,扇三角洲前缘内带物性最好,外带次之,平原物性较差。     

克拉玛依干旱生态农业区土壤质地的空间异质性研究

土壤具有高度的空间异质性,而地统计学方法已经被证明是研究土壤空间分布的最有力工具,质地作为一项重要的土壤物理特征,研究其在空间上的异质性在农业中具有重要意义。应用地统计学方法,对克拉玛依干旱生态农业区0～30 cm、30～60 cm、60～100 cm土层进行了土壤质地的半方差函数分析,结果表明:在整个研究区范围内,不同粒径土壤颗粒组成特点类似,均以粉粒平均含量最高,通体土壤颗粒的变异性都很强,尤以砂粒最为突出。研究区内除底层粉粒外,变异半方差模型都为球状模型,各土层土壤颗粒都表现出较强的空间结构性,空间相关距在6～9 km左右。基于半方差模型,用普通克里格法对研究区0～30 cm土层不同粒径土壤颗粒进行插值,表明土壤颗粒的分布情况和研究区地质地貌的分布特点相吻合。     

用微构造分析的方法精细表征油藏

结合实际工作中微构造分析方法在准噶尔盆地储层油藏描述研究中的应用,认为它们在油藏描述中的重要作用体现在以下几个方面:主要在弥补大层段、大等值线间距绘制下难以发现的砂体顶面或底面的微细变化,会发现与原地层构造总趋势一致而局部又不尽相同的微幅度构造或微体差异、在背斜构造-岩性油藏中,通过微局部分析确定更准确的含油边界、经过精细储层微构造分析排除假断层。结合多个区块的生产特征,具体分析了各类微构造对开发的影响,得出了在油藏开发前期和后期尽可能把采油井优先布在正向微构造上,把注水井尽可能布在负向微构造上的认识。对研究区的砂岩、砾岩多个区块储层微构造与油水井生产动态特征分析后进一步提出:油层微结构对油水井生产动态的影响作用是显著的,但不具唯一性。最终得出开发阶段为了精细刻画储层内部单砂体,用微构造分析的方法精细成图是体现研究深度的必要手段。     

克拉玛依油田七中东区克下组沉积微相及演化

通过对区域地质背景、岩心相、测井相分析,并结合分析化验等资料,认为克拉玛依油田七中、东区克下组沉积相为山麓-洪积相.将本区划分为扇根内带、扇根外带、扇中和扇缘4个亚相.从下到上,克下组沉积相平面分布从以扇根砂砾岩为主,演化为以扇中砂砾岩与泥岩互层为主,最终转变为扇缘泥岩夹少量砂砾岩.划分了槽流砾石体、片流砂砾体、漫洪砂体、漫洪细粒沉积、辫流水道、径流水道、漫流砂体和漫流细粒共8个沉积微相,描述了各微相岩石学特征、结构特征、构造特征和电性特征,指出沉积相平面展布及垂向演化特征,建立了研究区沉积模式.     

新疆吐哈盆地连木沁构造带克拉玛依组生物地质特征

新疆吐哈盆地连木沁构造带,在连4-S井4215～4832m取样分析,该地层孢粉化石数量和属种较多,主要为苔癣、蕨类植物孢粉和裸子植物花粉,孢粉化石组合具有较清楚的时代地层意义,通过分析命名为Aratnspontes - Punctatispozites - Colpectopollis组合。根据组合主要分子的时限及其含量变化,以及与有关已知时代孢粉组合进行比对,可确认该地层地质时代为克拉玛依组。     

准噶尔盆地红山嘴地区三叠系克上组两类粗粒三角洲的沉积记录差异及其成因*

准噶尔盆地红山嘴地区三叠系克上组存在扇三角洲与辫状河三角洲这两类粗粒三角洲,其界定在油气沉积学领域一直备受关注,而基于岩相类型及其垂向组合特征的沉积作用研究,辅以砂体宏观展布规律将有助于这两类三角洲的判别。红山嘴地区克上组扇三角洲以发育各种交错层理砾岩相(Gi、Gt、Gp)与块状砾岩相(Gmm、Gcm、Gcs)为特点,而辫状河三角洲则发育各种砂岩相(St、Sp、Sm和Sh等);扇三角洲6种岩相组合显示其碎屑流与密度流沉积相对发育,韵律特征不明显,而辫状河三角洲的7种岩相组合均显示其牵引流沉积作用更为显著,且正韵律居多;坡度陡、物源足造就了扇三角洲“砂体发育而分布局限、切割叠置频繁”的沉积响应特点,辫状河三角洲则因坡度中等且物源供给弱而具有“砂体薄而广布、多为孤立式接触”的响应特点。     

西准噶尔克拉玛依岩体的成因:年代学、岩石学和地球化学证据

西准噶尔地区克拉玛依岩体主要由闪长岩和花岗岩组成,锆石SHRIMP法给出的岩体结晶年龄为(315.5±2.8)Ma,为晚石炭世侵入岩.克拉玛依岩体具岛弧岩石的元素地球化学特征:总体上岩石富钠.A/CNK=0.57～0.84,富集LREE,(La/Yb)N=4.7～6.1,Eu显示弱负异常(δEu=0.76～0.91),...