北部湾盆地涠西南凹陷油气运聚成藏特征   总被引：2，自引：0，他引：2  

李颂  杨小晏 《世界地质》2012,31(2):365-370

北部湾盆地涠西南凹陷是个断陷湖盆,在油气运聚体系中,断裂可以起到沟通烃源岩的作用,将烃源岩和储层连通在一起; 不整合面造成不同层系的接触与连通,从而为其附近发育的各种圈闭提供油气侧向运移的通道,并形成油气藏。涠西南凹陷已发现的油气分布特征总体上呈“断裂沟源、断脊运移、两面控藏、复式聚集、满凹含油”的油气分布格局,形成了一个“一源多储、复式聚集、连片含油”的油气聚集区。  相似文献   

“小而肥”油藏油水分布特征及成因探讨——以海拉尔贝尔凹陷贝中油田为例   总被引：1，自引：0，他引：1  

黄劲松  刘长国  付晓飞  吕延防  孙永河 《吉林大学学报(地球科学版)》2012,42(1):9-17

针对“小而肥”油田油气成藏特点,以贝尔凹陷贝中油田为例,在对其探评井及开发井测井曲线、地震解释成果、测井解释资料、试油试采动态开发数据研究整理的基础上,结合其断裂系统拆分结果,通过典型实例分析和油藏解剖得知,贝中油田南一段主力油层在“满凹含油”的基础上,形成含油性差区或水区的主要控制因素为:断层断失作用造成目的层内主力...  相似文献   

利用C-F模型识别僵尸网络迁移   总被引：1，自引：1，他引：0  

臧天宁  云晓春  张永铮  门朝光 《武汉大学学报(信息科学版)》2010,(5)

基于C-F模型识别僵尸网络的迁移,以僵尸网络迁移过程中表现出的多个特征为基础,提出了一种识别僵尸网络迁移的方法,能够协同多个特征判断给定的两批僵尸主机是否具有迁移关系。通过几个典型僵尸样本的评测,有效地识别了僵尸网络的迁移行为。与单纯采用IP地址重合度的方法进行了对比,在僵尸网络成员数量动态变化的情况下,仍然保持了理想的识别结果。  相似文献   

Onshore sandbar migration at Tairua Beach (New Zealand): Numerical simulations and field measurements   总被引：1，自引：0，他引：1  

B. van Maanen  P.J. de Ruiter  Giovanni Coco  K.R. Bryan  B.G. Ruessink 《Marine Geology》2008,253(3-4):99-106

We observed the onshore migration (3.5 m/day) of a nearshore sandbar at Tairua Beach, New Zealand during 4 days of low-energy wave conditions. The morphological observations, together with concurrent measurements of waves and suspended sediment concentrations, were used to test a coupled, wave-averaged, cross-shore model. Because of the coarse bed material and the relatively low-energy conditions, the contribution of the suspended transport to the total transport was predicted and observed to be negligible. The model predicted the bar to move onshore because of the feedback between near-bed wave skewness, bedload, and the sandbar under weakly to non-breaking conditions at high tide. The predicted bathymetric evolution contrasts, however, with the observations that the bar migrated onshore predominantly at low tide. Also, the model flattened the bar, while in the observations the sandbar retained its steep landward-facing flank. A comparison between available observations and numerical simulations suggests that onshore propagating surf zone bores in very shallow water (< 0.25 m) may have been responsible for most of the observed bar behaviour. These processes are missing from the applied model and, given that the observed conditions can be considered typical of very shallow sandbars, highlight a priority for further field study and model development. The possibility that the excess water transported by the bores across the bar was channelled alongshore to near-by rip-channels further implies that traditional cross-shore measures to judge the applicability of a cross-shore morphodynamic model may be misleading.  相似文献   

北部湾盆地海中凹陷油气成藏条件分析   总被引：1，自引：0，他引：1  

孙建峰  ;须雪豪  ;席敏红 《海洋地质译丛》2008,(2):36-39

海中凹陷位于北部湾盆地西南部，其勘探程度低，对油气成藏条件欠缺系统的认识和深入的研究。以含油气系统理论为指导，在简要介绍地层与构造特征的基础上，重点论述了烃源岩、储集层、圈闭及输导介质等油气系统的基本要素，认为海中凹陷发育多套烃源岩、多套储集层、多种类型圈闭和复合的输导介质，具备油气系统形成的基本条件，具有较为广阔的油气勘探前景。  相似文献   

Elevated biomass of mesozooplankton and enhanced fecal pellet flux in cyclonic and mode-water eddies in the Sargasso Sea   总被引：2，自引：0，他引：2  

Sarah A. Goldthwait  Deborah K. Steinberg 《Deep Sea Research Part II: Topical Studies in Oceanography》2008,55(10-13):1360

Accumulating evidence points to the importance of mesoscale eddies in supplying nutrients to surface waters in oligotrophic gyres. However, the nature of the biological response and its evolution over time has yet to be elucidated. Changes in mesozooplankton community composition due to eddy perturbation also could affect biogeochemical cycling. Over the course of two summers we sampled seven eddies in the Sargasso Sea. We focused on and followed a post-phytoplankton bloom cyclonic eddy (C1) in 2004 and a blooming mode-water anticyclonic eddy (A4) in 2005. We collected zooplankton in all eddies using a Multiple Opening and Closing Net Environmental Sampling System (MOCNESS) and quantified biomass (>0.15 mm, in five size fractions) from 0 to 700 m over nine discrete depth intervals. Zooplankton biomass (>0.5 mm) in the upper 150 m was similarly enhanced at night for the periphery of C1 and the center of A4 at 0.514 g m⁻² and 0.533 g m⁻², respectively, compared to outside (0.183 g m⁻² outside C1 and 0.197 g m⁻² outside A4). Despite minimal chlorophyll a enhancement and dominance by picoplankton in C1, zooplankton biomass increased most for the largest size class (>5 mm). Gut fluorescence for euphausiids and large copepods was also elevated on the C1 periphery. In A4, peak biomass occurred at eddy center coincident with peak primary production, but was highly variable (changing by >3-fold) over time, perhaps resulting from the dense, but patchy distribution of diatom chains in this region. Shifts in zooplankton community composition and abundance were reflected in enhancement of fecal pellet production and active transport by diel vertical migration in eddies. Inside C1 the flux of zooplankton fecal pellets at 150 m in June 2004 was 1.5-fold higher than outside the eddy, accounting for 9% of total particulate organic carbon (POC) flux. The flux of fecal pellets (mostly from copepods) increased through the summer in eddy A4, matching concurrent increases in zooplankton <2 mm in length, and accounting for up to 12% of total POC flux. Active carbon transport by vertically migrating zooplankton was 37% higher on the periphery of C1 and 74% higher at the center of A4 compared to the summer mean at the Bermuda Atlantic Time-series Study (BATS) station. Despite contrasting responses by the phytoplankton community to cyclonic and mode-water eddies, mesozooplankton biomass was similarly enhanced, possibly due to differential physical and biological aggregation mechanisms, and resulted in important zooplankton-mediated changes in mesoscale biogeochemistry.  相似文献   

汶川8.0级地震前后陕西地区地倾斜特征迁移分析     

张创军  牛安福 《大地测量与地球动力学》2009,29(Z1):11-14

对汶川8.0级地震前后陕西地区地倾斜观测资料的分析发现，汶川地震前陕西地区地倾斜存在沿龙门山断裂带方向由东北向西南震中迁移，震后地倾斜反向迁移，迁移平均速度为3～4 km/天。进一步分析认为，震前陕西地区地倾斜向震源迁移可能对汶川8.0级地震起到了触发作用，而震后地倾斜向远场迁移有可能是诱发陕甘川交界的中强余震的主因。  相似文献   

东海西湖凹陷温压系统与油气成藏   总被引：3，自引：0，他引：3  

张先平  陈海红  张树林  叶加仁 《海洋地质与第四纪地质》2008,28(2):87-91

针对西湖凹陷存在异常温压系统的现象,利用钻井测温资料、测井声波时差压力、流体包裹体、镜质体反射率和磷灰石裂变径迹等资料对西湖凹陷的温压系统特征、类型及其对油气成藏的影响进行了系统研究。结果表明,西湖凹陷不同构造单元具有各异的温压场特征;西湖凹陷不同构造单元的温压系统类型不尽相同,其中保俶斜坡带和三潭深凹为高压型温压系统,浙东背斜带为常压型温压系统;西湖凹陷不同温压系统具有各异的流体流动样式和油气运聚规律;浙东中央背斜带内的流体能量相对最低,是研究区内有利的油气运聚区域。  相似文献   

基于位置大数据的国庆假期青藏高原人群分布时空变化模式挖掘   总被引：1，自引：0，他引：1  

易嘉伟  杜云艳  涂文娜 《地球信息科学学报》2019,21(9):1367-1381

人类活动是引起青藏高原生态环境发生改变的重要因素。很多学者对青藏高原史前人类活动和近几十年的人口分布格局与人口流动开展了大量研究,但有关人群时空分布的精细尺度研究相对缺乏。海量的位置大数据为认识高原人群短期的动态变化提供了新途径。本文利用手机定位数据、人口迁徙数据等高时空分辨率的位置大数据,通过时间序列分解方法和基于统计检验的异常判别方法,分析了2017年国庆期间青海与西藏的人群分布时空变化特征,并探讨了假期旅游行为及人口迁徙与变化特征之间的关系。研究结果显示：① 在省级和城市整体尺度上,定位请求量的假期变化在时间上呈现先降后升的“潮汐”变化模式;② 在精细网格尺度上,西宁和拉萨城市及周边地区的人群分布变化在空间上呈现中心跌、周边涨的“离心化”变化模式。国庆假期人们向城市周边热门景点移动聚集的旅游行为和城市之间的人口迁徙都是导致西宁和拉萨周边地区定位请求量上涨的重要潜在原因,而两座高原城市中心定位请求的下跌不仅与人口迁徙有关,还与假期人类日常行为及定位请求频次的变化等因素有关。通过位置大数据挖掘节庆假期人群分布的时空变化,不仅加深了对高原人口分布格局与流动变化的认识,也为高原城镇化与生态保护的精细化管理与决策提供支撑。  相似文献   

The population structural transition effect on rising per capita CO2 emissions: evidence from China     

Junfeng Wang  Yaqing Wu  Yue Zhao  Shutong He  Zhanfeng Dong  Wenguang Bo 《Climate Policy》2013,13(10):1250-1269

ABSTRACT

The per capita CO₂ emissions (PCCE) of many developing countries like China have been rising faster than total CO₂ emissions, and display spatial divergence. Such temporal growth and spatial divergence will have a significant influence on efforts to mitigate CO₂ emissions. Given the research gap on the impact of the structural transition in population on PCCE, we constructed an econometric model using the dynamic panel method. The results reveal that the population structural transition has a significant nonlinear impact on PCCE, as the rate of population growth in China decelerates. Both demographic ageing and urban-rural migration have a stronger impact on PCCE than other factors. This effect, however, decreases beyond a certain threshold. An increase in the number of households due to urbanization and family downsizing has resulted in a positive effect on PCCE, without a threshold turning point. The research also finds that an increased share of the service sector in employment can reduce PCCE only if the sector employs more than 31.56% of the total employed population. Overall, these findings indicate that policymakers should pay attention to the prominence of the demographic structural transition for effective climate policy.

Key policy insights

• Policymakers should address rising per capita carbon emissions (PCCE) and their spatial divergence in future climate policies, not just total CO₂ emissions.

• The transitioning demographics of ageing and urbanization in China show a nonlinear, inverted U-shaped effect on PCCE instead of a continuously positive effect.

• Based on the nonlinear effect of employment structure on PCCE, policymakers should focus on the relationship between the structural transition of the economy and PCCE in future climate mitigation policies.

  相似文献