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1.
浊沸石是准噶尔盆地二叠系砂砾岩储层常见的胶结物,成岩成储作用复杂。以玛湖凹陷东斜坡下乌尔禾组为例,分析岩心、铸体薄片资料,采用X线衍射、电子探针能谱及RT—DEN联合约束反演等方法,构建含浊沸石砂砾岩储层测井定量识别图版,优选浊沸石溶孔砂砾岩储层油气富集区。结果表明:对于更靠近研究区湖盆中心的P_2w_3~1油层,规模浊沸石溶孔储层的发育程度及油气富集条件更佳。含浊沸石砂砾岩储层预测标准为电阻率不小于20.0Ω·m,密度不大于2.46 g/cm~3,按照"垂向上,累计含浊沸石砂砾岩储层厚度大于6 m;平面上,单块面积大于40 km~2;含浊沸石砂砾岩储层厚度—主成藏期古鼻凸—通源断裂综合配置佳"的约束原则,P_2w_3~1油层优选规模浊沸石溶孔油气富集区块4个、总面积201 km~2。其中,B、C区块为Ⅰ类潜在油气富集区;A区块西侧低井控区及D区块为Ⅱ类潜在油气富集区。该结果为玛湖凹陷斜坡区及其他盆地浊沸石溶孔储层定量预测提供借鉴。  相似文献   

2.
在明确泥质体积分数、粒度为准噶尔盆地玛湖凹陷西斜坡区三叠系百口泉组低孔低渗砂砾岩储层质量主控因素基础上,结合储层—测井资料,构建储层评价因子CZ,利用常规测井曲线判别砂砾岩储层质量(储集空间、渗流能力);根据储层—测井—地震资料,在波阻抗反演基础上,利用储层评价因子CZ进行地质统计学模拟储层反演,预测百口泉组优质储层的平面展布范围.结果表明,Ⅰ类储层CZ8,储层质量最优,主要分布于玛132-玛13井一线,平面上叠置连片;Ⅱ类储层8CZ5,储层质量较优,多围绕I类储层边缘展布,主要分布于玛15、玛16、玛133井一带;Ⅲ类储层5CZ2,储层质量较差,主要分布于玛154、玛17井一带.该预测结果在油田现场井位部署中应用效果良好,部署8口井,Ⅰ类、Ⅱ类储层符合率分别为82%、85%.该方法为无核磁共振等特殊测井地区的低孔低渗砂砾岩储层分类评价及预测提供新思路.  相似文献   

3.
天然裂缝是深层致密砂岩储层重要的油气运移通道和储集空间,对库车坳陷博孜区块油气产能具有重要意义。利用岩心、薄片、成像测井以及实际生产资料,在明确塔里木盆地库车坳陷博孜区块超深层致密砂岩储层天然裂缝发育特征的基础上,厘定了天然裂缝对油气产能的影响。研究结果表明:库车坳陷博孜区块超深层储层构造裂缝发育,其中主要发育未充填-半充填的高角度剪切缝,局部发育半充填-全充填张性缝,受多期构造运动影响,区内主要发育N-S向和NW-SE向天然裂缝,部分呈近EW向;裂缝是研究区重要的储集空间和渗流通道,通过成像测井资料和试油资料构建了裂缝发育系数和裂缝有效系数用以定量表征裂缝对油气产能的影响,并建立了这两项表征参数和油气产能的定量评价图版,通过验证说明裂缝发育系数和裂缝有效系数可以较好地评价研究区裂缝的有效性,实现了通过裂缝参数对裂缝性储层品质的分类预测。研究成果不仅为研究区油气高效勘探开发提供了地质依据,同时提供了一个致密砂岩储层裂缝对油气产能影响的实例。  相似文献   

4.
西湖凹陷平北斜坡带平湖组广泛发育含油气性活跃的三角洲平原分流河道储层。利用岩心薄片、粒度分析、测录井、地震等资料,分析岩石矿物、沉积微相、测井相、地震相特征;结合实测GR曲线,完成综合预测误差滤波分析曲线(Inpefa)转换,实现河道演化期次划分;利用Marr小波分频、RGB融合技术预测河道展布范围。结果表明:分流河道岩性以长石岩屑质石英砂岩为主,储层孔隙以次生孔隙为主,粒度概率累积曲线为跳跃和悬浮两段式,发育斜层理、波纹层理等沉积构造;河道测井相为低伽马、中—高幅、钟型—箱型、齿化—微齿化特征;地震相为中—低频、中—强振幅、透镜状反射,河道反射构造为孤立、侧积、叠置3种样式。研究区发育4期河道砂体,河道由北向南展布,流向由早期北北东向转成晚期近南北向,晚期南部区域河道砂体发育规模大,为岩性油气藏勘探的有利区。  相似文献   

5.
石炭系火成岩储层是准噶尔盆地油气勘探开发的重要方向之一.以准噶尔盆地西北缘红车断裂带石炭系火成岩储层为主要研究对象,基于薄片鉴定、取心分析及测录井等资料,分析研究区的7种优势岩性及测井响应特征,采用多参数分布交会法,建立自然伽马—密度、中子孔隙度—密度和自然伽马—构建参数交会图版,预测优势岩性的平面分布.结果表明:研究区优势岩性为玄武岩、安山岩、火山角砾岩、凝灰岩、凝灰质砂砾岩、凝灰质细砂岩和沉凝灰岩;优势火成岩岩性具有局部发育的分布特征,以凝灰质为主的岩性(凝灰岩、凝灰质砂砾岩和凝灰质细砂岩)主要分布于研究区北部和主断层东侧,火山熔岩(玄武岩、安山岩)和火山角砾岩主要分布于研究区主断层西侧.多参数分步交会法可有效应用于研究区优势火成岩岩性识别,为利用常规测井资料有效识别火成岩岩性提供一种方法.  相似文献   

6.
准噶尔盆地腹部深层八道湾组致密储层特征及主控因素   总被引:1,自引:1,他引:0  
综合利用岩心、测井、薄片、扫描电镜及分析化验等资料,分析准噶尔盆地莫索湾—莫北地区侏罗系下统八道湾组致密储层宏观、微观特征及质量主控因素。结果表明:该储层为典型深层低—特低孔、低—特低渗致密碎屑岩储层;砂体主要为浅水三角洲型前缘水下分流河道细粒、中—细粒岩屑类砂岩,成分成熟度和胶结物体积分数低,岩屑和塑性岩屑体积分数高;成岩作用主要包括破坏性压溶作用、胶结作用及建设性溶蚀作用。孔隙垂向上主要位于混合孔—孔隙稳定和次生孔—孔隙增加两个变化带;孔喉为中—细孔—细喉型,大小、分布、连通性及渗流能力较差。储层质量(物性)主控因素为沉积相带、成岩作用和异常压力,共同决定储层原始和现今物性。该研究结果为深化盆地深层致密油气储层勘探开发提供依据。  相似文献   

7.
随着勘探程度的提高,深水重力流成因的浊积岩储层已成为我国东部断陷湖盆油气勘探开发的重要目标之一。因为沉积分异不足和成岩破坏,重力流砂岩的储层质量通常整体较差,优质储层的预测成为制约其有效油气勘探的关键地质因素。利用岩心、测井资料及储层物性、岩石薄片分析结果,研究了南堡凹陷东北部东营组二段重力流砂岩的岩相特征、成因类型、储层特征,以探索优质储层的控制因素和发育规律。研究表明,区内重力流沉积可细分为8种岩相,解释为滑动滑塌、砂质碎屑流、泥质碎屑流、浊流4类成因。储层物性参数统计分析证实,本区重力流砂岩储层非均质性强,储层质量受控于砂岩成因、砂-泥结构及其影响的溶蚀强度。从成因看,砂质碎屑流和浊流对重力流砂岩优质储层的发育贡献最大。砂质碎屑流成因的块状砂岩厚度较大、泥岩夹层较少、钙质胶结物的溶蚀程度高,储层质量最好;而浊流成因的砂岩厚度较薄,与泥岩呈互层或夹层产出,成岩环境封闭、钙质胶结物溶蚀程度低,储层质量较差。本研究为湖盆深水重力流砂岩油气的高效勘探开发提供了一种基于成因和结构的储层预测思路。  相似文献   

8.
根据岩心观察、镜下薄片鉴定、分析化验和测井解释等结果,分析巴楚地区泥盆系东河塘组储层岩石学、储集空间和物性特征.结果表明:东河塘组为高成分成熟度和高结构成熟度的石英砂岩,孔隙空间以溶蚀粒间孔为主要类型,储层物性以低孔低渗为特征;优质储层受沉积相带和成岩改造的双重控制,滨岸砂坝次生溶蚀孔隙发育,储层物性最好,含油气级别最...  相似文献   

9.
大路沟地区三叠系延长组长6储层特征及影响因素   总被引:10,自引:2,他引:8  
通过露头、岩心、测井分析测试资料,对大路沟地区长6油层组储层岩石学、孔隙结构和储集物性等特征进行研究.结果表明:该区延长组长6油层组为典型的低孔、低渗储层;储集砂体为成分成熟度低而结构成熟度高的长石砂岩;储层孔隙类型为原生粒间孔、粒内溶蚀孔、铸模孔或残余铸模孔;孔隙结构具有小孔隙、微细喉道的特点;储层性质明显受原始陆源组分、沉积相和成岩作用的相互影响;原始陆源组分的结构和含量对储层物性有直接影响;沉积相是基础,砂体厚度大、粒度较粗的水下分流河道的储集物性明显优于其他微相砂体;成岩作用对储层物性优劣起主导作用,压实作用、胶结作用导致储层致密,物性变差,溶蚀作用使储层得到改善.  相似文献   

10.
准噶尔盆地车排子凸起沙湾组的油气来源于东侧的昌吉凹陷和南侧的四棵树凹陷,分析连接烃源岩与油气藏的砂岩输导层的输导特征和性能,结合颗粒荧光定量技术测定的QGF指数变化趋势和光谱特征,追踪沙湾组砂岩输导层油气运移路径.结果表明:研究区沙湾组一段东侧和沙湾组二段南侧砂体于地质历史时期发生油气运移;排612—排609井、排606—排602井一带和排8井区为沙一段油气由东南至西北方向的优势运移路径,与红车断裂带共同构成油气垂向和侧向运移的高效通道;优势运移路径指向的西北地区继承性构造高部位的岩性、地层和岩性—构造等圈闭是未来勘探的重点.  相似文献   

11.
Aquaculture production efficiency may increase by using feed additives. This study investigated the effects of different dietary additives [w/w: 2% small peptides, 0.01% probiotics( Bacillus licheniformis) and 0.2% prebiotics(inulin)] on growth performance, digestive enzyme activities, and oxidative stress in juvenile Epinephelus coioides reared in artificial seawater of two salt concentrations(13.5 vs. 28.5). Weight gain rate was significantly higher in fish fed the diet supplemented with small peptides, B. licheniformis, inulin, or synbiotics than that in fish fed the basal diet; the greatest weight gain rate was found in fish fed the small peptide treatment [56.0% higher than basal diet]. Higher feed efficiency was detected in fish fed the diet supplemented with small peptides than that of fish in the other dietary treatments. Total protease activity in the stomach and intestines was highest in fish fed the small peptide-treated diet, whereas lipase activity was highest in those fed synbiotics(combination of Bacillus licheniformis and inulin) than that in fish fed the other treatments. Antioxidant enzyme(total superoxide dismutase and catalase) activities and hepatic malondialdehyde content were higher in fish receiving the dietary supplements and maintained in artificial seawater containing 13.5 salinity compared with those in the control(28.5). Hepatic catalase activity in grouper fed the diets with small peptides or synbiotics decreased significantly compared with that in control fish. Overall, the three types of additives improved growth rate of juvenile grouper and digestive enzymes activities to varying degrees but did not effectively improve antioxidant capacity under low-salinity stress conditions.  相似文献   

12.
The Liangshui Natural Reserve in Heilongjiang Province of China was selected as the study area. The authors collected the samples of forest litter (Tilia amurensis, Fraxinus mandshurica, Pinus koraiensis, Acer mono, Betula costata, and mixed litter), soil in humus horizon (0--5cm) and soil horizon (5-20cm), and soil macrofauna (Oligochaeta, Geophiloporpha and Juliformia) from 2001 to 2002. The role of soil macrofauna in the material cycle was analyzed through comparing the macro-element contents among various parts of the subsystems and using enrichment index (El). The results indicate that dynamic changes of various litters are very complicated. The contents of Fe in each kind of litter increase firstly, and then decrease in the study period. The changes of macro-element contents are greater in the broad-leaf litter than in the coniferous litter, and the mixed litter is in the middle level, but the differences among them are not significant. The contents of Mg and Fe in humus are higher than those in soil, but the contents of Ca in soil are higher than that in humus. The dynamic changes of macro-element contents in soil and soil fauna are not consistent with those in litter. The diplopod presented obvious enrichment of Ca and Mg (E1〉1), but it does not significantly enrich Fe. Earthworm has a stronger enrichment ability of Fe than diplopod and scolopendra, but E1〈1. Soil fauna can make great influences on the material cycle of the subsystems.  相似文献   

13.
The Liangshui Natural Reserve in Heilongjiang Province of China was selected as the study area.The authors collected the samples of forest litter (Tilia amurensis,Fraxinus mandshurica,Pinus koraiensis,Acer mono,Betula costata,and mixed litter),soil in humus horizon (0-5cm) and soil horizon (5-20cm),and soil macrofauna (Oligochaeta,Geophiloporpha and Juliformia) from 2001 to 2002.The role of soil macrofauna in the material cycle was analyzed through comparing the macro-element contents among various parts of the subsystems and using enrichment index (EI).The results indicate that dynamic changes of various litters are very complicated.The contents of Fe in each kind of litter increase firstly,and then decrease in the study period.The changes of macro-element contents are greater in the broad-leaf litter than in the coniferous litter,and the mixed litter is in the middle level,but the differences among them are not significant.The contents of Mg and Fe in humus are higher than those in soil,but the contents of Ca in soil are higher than that in humus.The dynamic changes of macro-element contents in soil and soil fauna are not consistent with those in litter.The diplopod presented obvious enrichment of Ca and Mg (EI>1),but it does not significantly enrich Fe.Earthworm has a stronger enrichment ability of Fe than diplopod and scolopendra,but EI<1.Soil fauna can make great influences on the material cycle of the subsystems.  相似文献   

14.
1IN T R O D U C T IO N With therapiddevelopment of urbanizatio,nurban land was exploitedand utilizetdoform differendtomains be- ing subjectto many potentialpollutionsourcessuch as vehicleemission, industrialactivitieasnd household garbage.Particularl, yur…  相似文献   

15.
16.
Porosity (n) and Dispersivity (D) were modeled in relation to Solute Transport Time (t) in a saturated, homogeneous, isotropic, unconfined aquifer using the MOC model. It was noted that n and D have an important influence on solute transport time t in groundwater, with a consistently strong and direct relationship between n, D, and t. In the case of porosity, the relationship was found to be directly related to t when other aquifer properties remained unchanged. This was also mathematically argued using a form of the flow equation put forward by Henry Darcy (1856). Dispersivity on the other hand had somehow the same relationship with solute transport time t as porosity, but with much less effect. That is, higher dispersions lead to longer solute transport time within the aquifer system. This was because as the individual solute particles set off from the average seepage velocity, they traversed through longer distances due to tortuosity, mechanical mixing, diffusion, and microscopic heterogeneity latent in the porous media. Also when n and D were co- treated over t, n was noted to be dominant over D with regard t. This follows that the effect of porosity on solute transport time far out shadowed that of dispersivity. Stated in other words, the dispersivity of a substance in any porous medium is to a large extent a function of the porosity of that medium.  相似文献   

17.
The contents of nearly forty-elements in surface sediments in Jiaozhou Bay were determined using a Neutron Activation Analysis Technique(Grancini,et al.,1976;Li Peiquan et al.,1985,1986;Li Xiuxia etal.,1986).This paper's detailed discussion on only nine elements(Fe,Mn,Co,Cr,Sc,As,Sb,Zn andV)includes their distributions,concentrations,correlationships,material sources,background,etc.Based on Zavaristski's classification method,Fe,Mn,Co Cr and V belong to the second group;As and Sb to theeighth groups:Sc and Zn to the third and sixth groups.It was found that their notably good correla-tionship is mainly due to the similarity of their ionic structures and that their variation is controlled by theFe content(except Mn).The source of sediments is mainly terristrial material,and the composition ofsediment is similar to that of shale and shale+clay.The contents for a large number of ele-ments are within the scope of the background level,but there still is pollution of Zn and Cr,at least in a few stations.  相似文献   

18.
Mollisols are common in South America. They cover about 8.87 × 10 7 ha, 1.3 × 10 7 ha and 4.3 × 10 6 ha in Argentina, Uruguay and Southern Brazil respectively, which is 11.5% of the world total. Most of South American Mol- lisols were developed on Pleistocene and Holocene sediments and lie within the limits of the temperate zone, though the extreme north is bordering subtropical and the extreme south is within a cold-temperate zone. All suborders of Mollisols occur in Argentina, the most extensive being Udolls followed by Ustolls, whereas only Udolls, Aquolls and Albolls occur in Uruguay. Vertisols in Uruguay have many properties similar to Mollisols, and the occurrence of Vertisols is strongly associated with Mollisols. The Pampean Mollisols are a significant component of the global breadbasket of modern times. The main Argentine crops are wheat,corn,sorghum, barley, soybeans and sunflower, while Mollisols in Uruguay remain mostly dedicated to cattle and sheep grazing though crop production has been increasing very rapidly in the last decade. Throughout South America, research has shown that Mollisols are experiencing losses of soil organic matter and nutrients, and degradation of physical properties after long cropping periods, resulting in soil scientists calling for increased conservation practices to reduce future losses and a deterioration of soil quality, and thus a more sustainable agriculture in the region.  相似文献   

19.
Plants possess effective mechanisms to respond quickly to the external environment.Rapid activation of phosphatidylinositol-specific phospholipase C(PLC)enzymes occurs after a stimulus.The PLC in Dunaliella salina play s important roles in growth and stress responses.However,the molecular basis of PLC action in D.salina remains little understood.To gain insight into the potential biological functions of this enzyme,we cloned a phospholipase C gene from D.salina in a previous study,named DsPLC(GenBank No.KF573428).Here,we present the prokaryotic expression,purification,and characterization of the DsPLC gene.The entire coding region of DsPLC was inserted into an expression vector pET32 a,and the DsPLC gene was successfully expressed in Escherichia coli.The DsPLC protein was purified and identified using a polyclonal antibody and western blotting.Expressing DsPLC fused with a green fluorescent protein(GFP)in onion showed that DsPLC-GFP was localized to the intracellular membrane.Quantitative real-time PCR analysis revealed that the relative expression of the DsPLC gene was induced significantly by 3.0-mol/L NaCl at 4 h.Our results support the importance of PLC enzymes in plant defense signaling.This study provides a basis for further functional studies of the DsPLC gene and for additional analysis of the potential roles of PLC enzymes in response to abiotic stress.  相似文献   

20.
The age, growth and maturation of Sthenoteuthis oualaniensis were determined with statolith data collected with a light purse seine from the Bashi Channel of central Pacific Ocean. The estimated longevity of the squid was no more than 6 months for females, and no more than 5 months for males. Growth in mantle length(ML) was best described by logistic models for both females and males, while growth in body weight(BW) was best fitted by power curves. The maximum absolute growth rate(AGR) and instantaneous growth rate(IGR) in ML or BW both occurred at 91–105 days for females and 76–90 days for males. Back calculated hatching dates were from October to January, with a peak in December, although the short duration of sampling date might have had an influence on the result. The lower percentage of mature females(37.2%) suggested that the study area during the sampling date was not a spawning ground for the species. Size and age at first maturity were 183 mm ML and 136 days for females, whereas they were 156 mm ML and 85 days for males.  相似文献   

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