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101.
珠江口盆地阳江东凹恩平21洼古近纪文昌组沉积期发育断陷湖盆,由于该区古近纪经历多期岩浆底辟和整体构造抬升,导致原型盆地被强烈改造,使其主要生烃层段文昌组的原型盆地面貌不清,从而给油气勘探和资源潜力评价造成困难。本文遵循改造型盆地的研究思路,将地震解析、声波时差法和趋势厚度法相结合,恢复了文昌组沉积期洼陷的原始面貌,并明确了优质烃源岩的展布范围。研究表明,阳江东凹恩平21洼在始新世文昌组沉积末期遭受强烈的剥蚀改造,造成洼陷东北部1/4沉积地层剥蚀殆尽;在文二段沉积期,恩平21洼北部与恩平14洼连通形成广盆深水的沉积环境,控制文二段半深湖相优质烃源岩的形成。从文昌组烃源岩的原始沉积规模和勘探实践来看,阳江凹陷具有良好的资源潜力。 相似文献
102.
There are numerous controversies surrounding the tectonic properties and evolution of the Proto-South China Sea(PSCS).By combining data from previously published works with our geological and paleontological observations of the South China Sea(SCS),we propose that the PSCS should be analyzed within two separate contexts:its paleogeographic location and the history of its oceanic crust.With respect to its paleogeographic location,the tectonic properties of the PSCS vary widely from the Triassic to the mid-Late Cretaceous.In the Triassic,the Paleo-Tethys and the Paleo-Pacific Oceans were the major causes of tectonic changes in the SCS,while the PCSC may have been a remnant sea residing upon Tethys or Paleo-Pacific oceanic crust.In the Jurassic,the Meso-Tethys and the Paleo-Pacific oceans joined,creating a PSCS back-arc basin consisting of Meso-Tethys and/or Paleo-Pacific oceanic crust.From the Early Cretaceous to the midLate Cretaceous,the Paleo-Pacific Ocean was the main tectonic body affecting the SCS;the PSCS may have been a marginal sea or a back-arc basin with Paleo-Pacific oceanic crust.With respect to its oceanic crust,due to the subduction and retreat of the Paleo-Pacific plate in Southeast Asia at the end of the Late Cretaceous,the SCS probably produced new oceanic crust,which allowed the PSCS to formally emerge.At this time,the PSCS was most likely a combination of a new marginal sea and a remnant sea;its oceanic crust,which eventually subducted and became extinct,consisted of both new oceanic crust and remnant oceanic crust from the Paleo-Pacific Ocean.In the present day,the remnant PSCS oceanic crust is located in the southwestern Nansha Trough. 相似文献
103.
Geotechnical and Geological Engineering - The progressively brittle failure of foliated rocks involving the initiation, propagation, and aggregation modes is closely related to the microscopic... 相似文献
104.
大同火山活动的阶段性历史是一个尚未被揭示清楚的地学问题。野外实地考察及室内磁化率、化学成分、粒度和古地磁的测定结果显示:古湖滨处水平层理发育的火山碎屑层存在4个不同倾角的倾斜;古湖近岸处的湖相沉积层中含有4层火山碎屑层;古湖深处的湖相沉积层中出现4个磁化率显著正异常的层位,且这些层位粒度都较粗;古湖岸上的黄土沉积中出现3个磁化率为峰值、Rb/Sr比值为谷值的层位;古湖深处湖相沉积剖面中存在B/M和Jaramillo磁极性界限。据此进一步分析后认为:① 湖相沉积剖面中的磁化率显著正异常层位、黄土沉积中的高磁化率—低Rb/Sr比值层位可能是混入了大量火山灰物质;它们是区域火山活跃期的记录。② 系列沉积剖面特征指示区域火山活动曾经历4个活跃期,每个活跃期期间有多次密集的火山喷发。③ 4个活跃期的年代大约为早于0.90 Ma BP(第一活跃期)、~0.47 Ma BP(第二活跃期)、~0.31 Ma BP(第三活跃期)和~0.09 Ma BP(第四活跃期);黄土沉积中还记录了区域北部有一个发生于~0.19 Ma BP的活跃期。此外,区域湖相沉积中所记录的4个火山活跃期都出现在湖退时期,平静期出现在湖侵时期。 相似文献
105.
利用青岛市环境监测中心站环境监测资料、青岛市气象常规观测资料、美国国家环境预报中心(NCEP)再分析资料,对青岛地区2016年12月18—21日的一次雾霾重污染天气过程进行分析。结果表明:污染期间,亚欧大陆中高纬度地区500hPa呈两槽一脊的环流形式,青岛处于弱槽系统控制下,空气质量好转时,高空锋区明显增强,西北风加大,地面冷锋快速东移;此次雾霾重污染天气过程空气中近地面相对湿度一直维持较高,重污染期间小于2.6m·s~(-1)的地面风速对污染物扩散没有明显作用;污染物的浓度增加、持续阶段与气象要素能见度、风速、混合层厚度呈负相关性,与相对湿度呈正相关性,与温度的相关性较低;污染过程中青岛市区24h的输入污染源主要来自半岛北部地区,主要污染物为PM_(2.5)颗粒。 相似文献
106.
中国城市群从区域向空间网络的转变,成为城乡统筹发展功能的主体地域单元。基于“交通—产业”的耦合视角,以京津冀城市群为研究区域,选取北京、天津、石家庄、唐山作为城市群发育的辐射中心,结合空间网络分析、引力模型、多层次空间结构MSS-Tree算法,测度识别京津冀城市群空间结构及现状发育范围。结果发现:①京津冀城市群还不成熟,辐射中心周边的辐射发育区“岛、洞”现象明显,表现为连片分布的大城市阴影区;其中北京市周边缺乏成熟副中心,天津市受到北京极化作用影响,辐射区大幅萎缩;石家庄、唐山辐射区发育不足,需首先加强自身经济建设;②交通、产业辐射发育范围重合度较低,交通的先导作用加速了中小城镇生产要素流失,形成环京津贫困带。据此提出了自下而上整合、由内向外扩展的地区发展策略建议。 相似文献
107.
欧洲是“一带一路”倡议的重点覆盖地域,是亚欧大陆经济走廊的重要组成,维护其地区安全稳定,排除干扰中欧两大市场合作互联的潜在安全隐患,对于“一带一路”倡议的稳固推进十分必要。基于地理学视角,考虑难民安置政策因素,采用灰色关联分析、层次分析、多目标规划等方法对2015-2017年欧洲难民危机时空演变过程及迁移格局优化进行分析。① 时空演化分析显示难民集中于2015年登陆欧洲,欧洲各国登陆难民、接收难民数量极化突出,双重失衡;② 灰色关联分析显示难民迁移决策具有福利优先、收入优先的导向,各国难民政策调整为迁移决策带来不确定性,既有迁移格局难以长期维持;③ 层次分析显示北欧西欧国家难民宜居性较高,东欧南欧国家宜居性相对较差,部分避难国承担安置难民数量与其宜居性不符;④ 多目标规划的优化格局显示,由于欧洲各国忽视全球化背景致使难民政策指向错误,迁移网络更加混乱失衡,优化后来自土耳其、乌克兰的难民迁移趋势向西欧集中,来自希腊、匈牙利的难民迁移趋势在空间上更加平均分散,来自意大利的难民迁移趋势向西欧南欧呈扇形分散。优化后迁移格局有助于缓解地区安全局势、为“一带一路”建设创造良好的政治、经济环境,平衡劳动力资源配置,为建设投资提供潜在市场。最后在研究结果的基础上提出若干协同合作调整难民迁移格局的危机缓解措施。 相似文献
108.
Given enormous capital costs, operating expenses, flue gas emissions, water treatment and handling costs of thermal in situ
bitumen recovery processes, improving the overall efficiency by lowering energy requirements, environmental impact, and costs
of these production techniques is a priority. Steam-assisted gravity drainage (SAGD) is the most widely used in situ recovery
technique in Athabasca reservoirs. Steam generation is done on surface and consequently, because of heat losses, the energy
efficiency of SAGD can never be ideal with respect to the energy delivered to the sandface. An alternative to surface steam
generation is in situ combustion (ISC) where heat is generated within the formation through injection of oxygen at a sufficiently
high pressure to initiate combustion of bitumen. In this manner, the heat from the combustion reactions can be used directly
to mobilize the bitumen. As an alternative, the heat can be used to generate steam within the formation which then is the
agent to move heat in the reservoir. In this research, alternative hybrid techniques with simultaneous and sequential steam-oxygen
injection processes are examined to maximize the thermal efficiency of the recovery process. These hybrid processes have the
advantage that during ISC, steam is generated within the reservoir from injected and formation water and as a product of oxidation.
This implies that ex situ steam generation requirements are reduced and if there is in situ storage of combustion gases, that
overall gas emissions are reduced. In this research, detailed reservoir simulations are done to examine the dynamics of hybrid
processes to enable design of these processes. The results reveal that hybrid processes can lower emitted carbon dioxide-to-oil
ratio by about 46%, decrease the consumed natural gas-to-oil ratio by about 73%, reduce the cumulative energy-to-oil ratio
by between 40% and 70% compared to conventional SAGD, and drop water consumption per unit oil produced. However, oil recovery
is between 25% and 40% below that of SAGD. Design of successful hybrid steam–oxygen processes must take into account the balance
between injected steam and amount of injected oxygen and combustion gas products that dilute injected and in situ-generated
steam in the depletion chamber by lowering its partial pressure, and thus its saturation temperature which in turn impacts
production rates and recovery. 相似文献
110.