共查询到20条相似文献，搜索用时 93 毫秒
1.
渤海石臼坨凸起沙河街组发育一套湖相混积岩岩性段,呈现出良好的油气显示.利用显微岩石与矿物学观察、扫描电镜、电子探针、碳氧同位素地球化学、气液包裹体温度分析等方法技术,研究总结了渤海石臼坨凸起古近系沙河街组混积岩的成岩作用和孔隙演化特征.沙河街组混积岩储层主要为陆源碎屑质－碳酸盐混积岩,储集空间主要为残余原生粒间孔和生物体腔孔,为高孔高渗储层.储层中发育的成岩作用主要有:①压实作用;②胶结作用,主要为颗粒包壳、孔隙衬垫与充填和交代白云石等自生白云石胶结作用,自生白云石具有典型的多期生长特征;③溶蚀作用,主要为陆源碎屑中的长石、岩屑等的溶蚀,其次是早期衬垫白云石的溶蚀.伴随成岩演化,储层孔隙度由初始的４０％演变到现今的２２％.早期孔隙衬垫白云石、长石溶蚀对古近系沙河街组混积岩中的有利储层发育具有重要控制作用. 相似文献
2.
结合黔东麻江地区下寒武统清虚洞组上部沉积微相特征,通过地球化学指标研究了其沉积环境的微细变化。研究结果显示,清虚洞组上部碳同位素整体在－0.24‰ ~＋1.25‰之间波动;锶同位素分布在0.708 9～0.711 9间;Ce异常整体为弱的负异常,δCe大于0.8;Sr/Ba比值绝大部分大于1,反映出水体较浅、水动力较强的浅滩相沉积环境。研究层位中部第11层的锶同位素、铝含量和稀土元素总量显著增大,指示陆源输入在该时期增强,为距离陆源较近的潮坪环境。上述地球化学指标得出的沉积环境与沉积相分析结果一致,均表明清虚洞组上部整体为浅水富氧的浅滩环境,其中部为陆源碎屑输入丰富的潮坪环境,将清虚洞组滩相分隔为两期。此次研究表明碳酸盐岩的地球化学特征能够反映沉积环境的演化,是判断沉积相的有效辅助手段。 相似文献
3.
文章应用地洼成矿理论和构造地球化学方法,研究了某地区Ｆ１等成矿断裂带的构造地球化学特点和元素的变化规律以及铀不断累增富集成矿的作用过程。在形成泥盆系富铀地层的基础上,经历了后期构造—岩浆活化作用的改造,形成预富矿化场—动力改造热液成矿,形成构造热液型铀矿化—表生淋积,形成叠生富矿段,使之发展成为具有层控、岩控、构控和时控等特点的多因复成型铀矿床,从而为本区进一步找矿指明了方向。 相似文献
4.
南秦岭碧口群岩石组合特征及其构造意义 总被引：2，自引：0，他引：2
裴先治 《地球科学与环境学报》1989,(2)
碧口群是扬子板块西北缘中晚元古代古海沟—岛弧体系的重要组成部分。岩石组合、岩石化学及稀土元素特征研究表明,其下部为蛇绿岩组合,以大洋E型拉斑玄武岩为特征,代表古俯冲杂岩;上部为重力流沉积组合,以火山质碎屑浊积岩及陆源碎屑浊积岩为特征,类似于海沟型复理石组合,代表古海沟堆积。同时构造变形及变质作用特征表明,在蛇绿岩分布区发育有大型韧性剪切带和高压低温变质的蓝闪片岩。由此可见碧口群属于中晚元古代扬子板块西北缘的古海沟—俯冲地体。 相似文献
5.
柴达木盆地西北部的小梁山背斜构造,陆源碎屑和湖相碳酸盐混合沉积广泛发育,地层岩石类型多样,测井响应特征复
杂,岩性识别非常困难。结合岩石物理实验数据(铸体薄片、粒度分析、X射线衍射全岩分析、碳氯分析)和测井资料,对研究区混
积岩岩石组分的类型、粒度和质量分数进行了细致的分析研究,以岩石组分的相对质量分数和测井响应特征为依据,对岩性进行
了简化归类,建立了测井资料识别岩性标准,在此基础上利用ΔGR、Δlg(LLD)和M 参数绘制了混积岩岩性识别电性组合图,并建
立了岩性质量分数计算模型,形成了一套小梁山地区测井岩性综合识别方法,为小梁山地区的储层测井评价和综合地质研究奠定
了基础,对中浅层混积岩的测井解释研究具有借鉴与参考意义。 相似文献
杂,岩性识别非常困难。结合岩石物理实验数据(铸体薄片、粒度分析、X射线衍射全岩分析、碳氯分析)和测井资料,对研究区混
积岩岩石组分的类型、粒度和质量分数进行了细致的分析研究,以岩石组分的相对质量分数和测井响应特征为依据,对岩性进行
了简化归类,建立了测井资料识别岩性标准,在此基础上利用ΔGR、Δlg(LLD)和M 参数绘制了混积岩岩性识别电性组合图,并建
立了岩性质量分数计算模型,形成了一套小梁山地区测井岩性综合识别方法,为小梁山地区的储层测井评价和综合地质研究奠定
了基础,对中浅层混积岩的测井解释研究具有借鉴与参考意义。 相似文献
6.
《东北石油大学学报》2015,(5)
塔河油田南部地区发生多次强烈的岩浆喷发活动,岩浆活动带来地壳深部的热液流体,对储层形成多种改造作用.根据岩心薄片观察资料,分析研究区热液作用模式与机制,结果表明,塔河油田南部奥陶系热液流体活动显著,岩石学特征主要表现为典型的热液成因硅化硅质岩、热液溶蚀缝孔洞发育.地球化学特征表现为热液作用缝洞方解石的稀土元素分配曲线较平缓,表现为LREE富集,显示明显的正Eu异常和较高的Y/Ho值,与研究区所经历的二叠纪岩浆—火山活动有关;热液成因方解石具有较低的87Sr/86Sr值,低于碳酸盐围岩与同期海水的,主要受幔源锶的控制及围岩重溶锶的缓冲影响;受高温高盐度热液流体影响,热液矿物的包裹体均一温度均高于奥陶系地层正常埋藏温度40℃以上,盐度质量分数为正常海水的3~5倍.该研究为塔河油田南部奥陶系碳酸盐储层的油气勘探提供参考. 相似文献
7.
咸化湖盆混积岩中双重孔隙介质及其油气储集意义 总被引：3，自引：0，他引：3
柴达木盆地英西地区始新统下干柴沟组为咸化湖盆沉积的混积岩,其组分包括湖相碳酸盐、碎屑颗粒、泥质等,且岩石中含较多的盐类矿物。通过岩芯观察、物性分析、毛管压力测试、成像测井和场发射扫描电镜研究发现,混积岩具有双重孔隙介质,一类为孔径较大的裂缝和盐类矿物溶蚀孔,另一类为孔径较小的盐间缝和白云石晶间孔,共同构成了毛管压力曲线上的"低窄高宽的双平台"结构,岩石物性整体上较差,以"低孔—特低渗"为主,孔喉普遍较细。电子探针微区成分分析结果表明,白云石元素组成具有"高铝硅低铁锰"的地球化学特征,FeO平均质量分数为1.322%,MnO平均质量分数为0.060%,明显低于热液白云岩中的铁锰质量分数,为准同生交代成因的典型特征。白云石化过程中产生了大量收缩晶间孔,这类基质孔隙储油是支撑英西地区持续稳产的重要因素。 相似文献
8.
沉积岩中的稀土元素具有良好的化学稳定性, 能够较好保存原始沉积记录。为了揭示阳江东凹文昌组发育时期的物源区物质来源、构造背景和沉积环境, 选取凹陷内Y-1井文昌组泥岩样品进行元素测试, 系统分析研究区文昌组泥岩稀土元素地球化学特征。结果表明, 文昌组泥岩稀土元素含量高, 轻稀土元素相对富集, Eu为明显负异常, Ce为微弱正异常特征。文昌组物质来源以花岗岩为主, 含有少量沉积岩, 沉积源区为被动大陆边缘构造背景。Ceanom和δ Ce参数指示文昌期水体处于还原环境, 为优质烃源岩发育提供良好的保存条件, 纵向上水体还原性演化规律为: 强→弱→强→弱, 与文昌组泥岩TOC变化趋势一致。 相似文献
9.
为了探究广西十万大山盆地扶隆坳组地球化学特征及其地质意义,在显微镜下对研究区砂岩进行了系统鉴定、碎屑颗
粒组分统计,并利用ICP-MS对该区泥岩样品进行了微量元素和稀土元素分析,结果显示扶隆坳组砂岩碎屑颗粒组分石英颗粒含
量较高,长石含量较少,岩屑以浅变质岩屑为主,Dickinson图解显示物源区为再旋回造山带;泥岩样品的REE受成岩作用改造微
弱,且主要来自陆源碎屑矿物,源岩主要为沉积岩及花岗岩岩石;稀土元素和微量元素相关参数显示晚三叠世扶隆坳沉积时期气
候相对湿热,沉积了一套以陆相沉积环境为主的碎屑岩。综合前述认识,结合本区构造演化史,推断扶隆坳组物源供给主要来自
晚泥盆世-早石炭世钦防海槽沉积的硅质岩、硅质页岩及泥岩,源区构造背景兼有活动大陆边缘和被动大陆边缘的性质。 相似文献
粒组分统计,并利用ICP-MS对该区泥岩样品进行了微量元素和稀土元素分析,结果显示扶隆坳组砂岩碎屑颗粒组分石英颗粒含
量较高,长石含量较少,岩屑以浅变质岩屑为主,Dickinson图解显示物源区为再旋回造山带;泥岩样品的REE受成岩作用改造微
弱,且主要来自陆源碎屑矿物,源岩主要为沉积岩及花岗岩岩石;稀土元素和微量元素相关参数显示晚三叠世扶隆坳沉积时期气
候相对湿热,沉积了一套以陆相沉积环境为主的碎屑岩。综合前述认识,结合本区构造演化史,推断扶隆坳组物源供给主要来自
晚泥盆世-早石炭世钦防海槽沉积的硅质岩、硅质页岩及泥岩,源区构造背景兼有活动大陆边缘和被动大陆边缘的性质。 相似文献
10.
裴先治 《地球科学与环境学报》1992,(1)
碧口地区晚元古代复理石岩系位于扬子板块西北缘,其主体由下部火山质碎屑浊积岩和上部陆源碎屑浊积岩组成。本文研究了复理石岩系中杂砂岩的岩石学、碎屑模型和岩石化学特征,并与不同板块构造背景下沉积的古代杂砂岩和现代深海砂成分进行了类比。研究表明,复理石岩系形成于沟弧盆系活动大陆边缘构造环境,杂砂岩属大陆岛弧型,物源区为活动大陆边缘的火山—深成岩浆岛弧造山带,源岩为钙碱性长英质火山岩及同源深成侵入岩,沉积盆地为岛弧及俯冲杂岩外侧的古海沟环境。 相似文献
12.
四川盆地珍珠冲组植物群特点及侏罗系与三叠系界线的厘定 总被引：1，自引：0，他引：1
归纳总结了四川盆地珍珠冲组植物化石7类50属128种,须家河组植物化石10类71属267种,并将珍珠冲组植物群划分为上、下两个组合.通过分析两组植物群的发育特点及演化规律,结合区域有关资料,对侏罗系与三叠系界线进行了厘定.在四川盆地北部大巴山前缘地区,依据珍珠冲组(白田坝组)的岩性特征和所含植物化石特征,将侏罗系与三叠系的界线置于含Coniopteris植物化石的珍珠冲组(白田坝组)底部石英质砾岩或石英砂岩之下的假整合面或剥蚀面上;在四川盆地东北部的云阳、奉节及长江以南万县地区,侏罗系与三叠系的界线划在云阳南溪剖面上含Coniopteris murrayana植物化石8.3 m之下的珍珠冲组黄绿色泥质粉砂岩夹粉砂质泥岩地层之底. 相似文献
13.
《中国海洋湖沼学报》2021,(4)
Impact factors on the salinity budget,especially the eddy salt fluxes and smaller-scale diffusive salt fluxes for the upper 50 m of the Bay of Bengal(BoB) in 2014 are investigated using a box model based on the Regional Ocean Modeling System(ROMS) daily outputs.The model results reproduce that the precipitation and river runoffs are the dominant factors modulating the sharp salinity decrease during the summer monsoon season.The analysis shows that the salinity increase after the summer monsoon is mostly due to the meridional advective and diffusive salt fluxes.The vertical advective salt flux,which is sensitive to the different signals of the wind stress curl,plays an important role in balancing the salinity change induced by the meridional advective salt flux during both the summer and winter monsoon seasons.Distinctive spatial mesosc ale structures are presented in the eddy salt flux throughout the year,and their contributions are sizeable(over 30% in the meridional direction and about 10%-30% in the vertical direction).The meridional eddy salt flux is larger in the monsoon seasons than that in the inter-monsoon seasons,and in a positive pattern near the western boundary during the winter monsoon and autumn inter-monsoon.The vertical eddy salt flux makes an important contribution to the salinity budget,especially along the coastal area and around the Andaman and Nicobar Islands.The vertical eddy salt flux becomes large when a tropical cyclone passes the area. 相似文献
14.
15.
Krzysztof KOLODZIEJCZYK 《山地科学学报》2020,17(4):949-972
Among the factors influencing tourist trail network development are political issues, including the presence of state borders, the possibility of crossing them and the accessibility of border zones. In the article, it was decided to look at changes in the offer of tourist trails(hiking and cycling) along the entire border of the Czech Republic after the extension of the Schengen area(within this area, crossing the border is possible anywhere, and not only at official border crossings). It should be emphasized here that the borders of the Czech Republic over most of their length run through mountainous areas and, apart from political factors, natural features should have a major impact on the development of tourist routes. In order to determine the coherence of the current network of trails on both sides of the Czech Republic state border, modern tourist maps have been analyzed, determining the number of places where it is possible to cross the state border with the help of a marked tourist trail. Based on that, two indicators were introduced to determine the degree of openness with all neighboring countries as regards the opportunity to cross on a tourist trail. Changes in the historical situation, a comparison of the accessibility of the border area before entering the Schengen area and 2019, were analyzed for two study areas using archival maps. Over a decade after the extension of the Schengen area, the number of places where tourist trails of neighboring countries approach the border has clearly increased. Crossing is more often made possible using hiking trails than cycling routes(trails of the first type cross the border every 7.91 km, while the latter every 13.3 km), but considering the speed of movement, it can be assessed that the openness for cyclists is higher than for hikers. Moreover, in many places there is still significant potential for further integration of tourist trail networks as trails created in one country often do not have a continuation on the other side of the border. 相似文献
16.
介绍了泰州市在推进国土资源管理走上法制化轨道的过程中采取的一系列措施.从健全规章制度,规范执法行为,实行责任追究制度,制约行政权力到严格考核奖惩,确保各项措施落到实处,便民服务,公开接受社会监督等,取得了明显的成效. 相似文献
17.
Habitat richness influences and even determines biological diversity. Plant habitat suitability assessment can provide technical guidance and information support for ecological restoration. Thirteen factors in three categories of terrain, meteorology and soil were chosen to build a habitat suitability assessment index framework in the Upper Reaches of the Min River, based on the local natural environment and the actual influencing factors of vegetative growth. Combined with the Analytic Hierarchy Process(AHP) and entropy method, which were used to calculate weights of indexes, habitat suitability was studied by using a multi-objective linear weighting model and geographic information systems(GIS) spatial analysis techniques. The assessment results are as follows: Altitude, soil stability, aspect and slope have more important effects on plant habitat suitability in the Upper Reaches of the Min River, and their weights are 0.311, 0.260, 0.198 and 0.125, respectively. Suitable and sub-suitable habitats cover 4431.80 km2 and 6171.12 km2, respectively; most of which are distributed along both sides of rivers and have higher suitability. Unsuitable habitats cover the largest area(6679.76 km2), accounting for 29.83% of the whole area; and the worst unsuitable habitats are 5107.23 km2(22.81%); they account for more than half of the studyarea. These results indicate that the plant habitat in the Upper Reaches of the Min River is poor and ecological restoration is both urgent and difficult. Therefore, based on the principle of taking measures suitable to the habitat in ecological restoration projects, ecological and engineering measures should be combined to have better effects, while increasing the strength of ecological protection. 相似文献
18.
《广东海洋大学学报》2016,(6)
对广东省中山市三角镇的低盐度鱼虾混养池进行连续采样分析,结果表明,混养池中的蓝藻主要有螺旋藻(Spirulina sp.),鱼腥藻(Anabaena sp.),颤藻(Oscillatoria sp.)、铜绿微囊藻(Microcystis aeruginosa)等,其中盐泽螺旋藻的优势度为0.52~0.73。蓝藻是水体中的优势微藻种群,蓝藻细胞数量占微藻细胞数量的88%~99%,蓝藻细胞数为0.99×10~9~5.89×l0~9 cell/L。混养池微藻多样性指数(H’)为1.16~2.49,养殖水体处于中度污染状态。溶解性无机氮的质量浓度为0.13~2.30 mg/L,正磷酸盐质量浓度为0.25~2.39 mg/L,化学需氧量的质量浓度为1.94~13.79 mg/L。微囊藻毒素(MC-LR)在水中质量浓度为0.18~0.79μg/L。蓝藻细胞数量与化学需氧量之间呈显著的正相关关系,表明蓝藻的生长情况与养殖池中的有机污染程度有密切联系,低盐度的富营养化的水体能促进蓝藻的生长,成为微藻群落中的优势种群。MC-LR的质量浓度与蓝藻细胞数量之间无显著相关。 相似文献
19.
CTD data on standard levels coolected during July and December in 1998 and the cubic spline interpolating method were used to study the characteristics of the transition layer temperature and salinity.The thermocline undergoes remarkable seasonal variation in the South China Sea (SCS),and especially in the region of the north shelf where the thermocline disappears in december.The thermocline is stronger and thicker in July than in December,There is no obvious seasonal variation in the halocline.Due to the upper Ekman transport caused by monsoon over the SCS,the thermocline slopes upward in July and downward in december from east to west in the northern SCS.The characteristics of the thermocline and halocline are influenced by local eddies in the SCS.The Zhujiang diluted flow influences significantly the SCS shelf‘s halocline. 相似文献
20.
Based on the analysis of Levitus data, the climatic states of the warm pool in the Indian Ocean (WPIO) and in the Pacific
Ocean (WPPO) are studied. it is found that WPIO has a relatively smaller area, a shallower bottom and a slightly lower seawater
temperature than those of WPPO. The horizontal area at different depths, volumes, central positions, and bottom depths of
both WPIO and WPPO show quite apparent signals of seasonal variation. The maximum amplitude of WPIO surface area’s seasonal
variation is 58% larger over the annual mean value. WPIO’s maximum volume variation amplitude is 66% larger over the annual
mean value. The maximum variation amplitudes of the surface area and volume of WPPO are 20.9% and 20.6% larger over the annual
mean value respectively. WPIO and WPPO show different temporal and spatial characteristics mainly due to the different wind
fields and restriction of ocean basin geometry. For instance, seasonal northern displacement of WPIO is, to some extent, constrained
by the basin of the Indian Ocean, while WPPO moves relatively freely in the longitudinal direction. The influence of WPIO
and WPPO over the atmospheric motion must be quite different. 相似文献