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121.
琼东南盆地陵南低凸起深水钻井岩心的稀土元素地球化学特征及其意义 总被引:2,自引:0,他引:2
A geochemical analysis of rare-earth elements(REEs) in 97 samples collected from the core of deep-water Well LS-A located at the Lingnan Low Uplift Area of the Qiongdongnan Basin is conducted, with the purpose of revealing the changes of sedimentary source and environment in the study region since Oligocene and evaluating the response of geochemical characteristics of REEs to the tectonic evolution. In the core samples, both ∑REE and ∑LREE(LREE is short for light-group REEs) fluctuate in a relatively wide range, while ∑HREE(HREE is short for heavy-group REEs) maintains a relatively stable level. With the stratigraphic chronology becoming newer, both ∑REE and ∑LREE show a gradually rising trend overall. The ∑REE of the core is relatively high from the bottom of Yacheng Formation(at a well depth of 4 207 m) to the top of Ledong Formation, and the REEs show partitioning characteristics of the enrichment of LREE, the stable content of HREE, and the negative anomaly of Eu to varying degrees. Overall the geochemical characteristics of REEs are relatively approximate to those of China's neritic sediments and loess, with significant "continental orientation". The ∑REE of the core is relatively low in the lower part of Yacheng Formation(at a well depth of 4 207–4 330 m), as shown by the REEs partitioning characteristics of the depletion of LREE, the relative enrichment of HREE, and the positive anomaly of Eu; the geochemical characteristics of REEs are approximate to those of oceanic crust and basalt overall, indicating that the provenance is primarily composed of volcanic eruption matters. As shown by the analyses based on sequence stratigraphy and mineralogy, the provenance in study region in the early Oligocene mainly resulted from the volcanic materials of the peripheral uplift areas; the continental margin materials from the north contributed only insignificantly; the provenance developed to a certain extent in the late Oligocene. Since the Miocene, the provenance has ceaselessly expanded from proximal to distal realm, embodying a characteristic of multi-source sedimentation. In the core strata with 31.5, 28.4, 25.5, 23, and 16 Ma from today, the geochemical parameters of REEs and Th/Sc ratio have significant saltation, embodying the tectonic movement events in the evolution of the Qiongdongnan Basin. In the tectonic evolution history of the South China Sea, the South China Sea Movement(34–25 Ma BP, early expansion of the South China Sea), Baiyun Movement(23 Ma BP), late expansion movement(23.5–16.5 Ma BP), expansion-settlement transition, and other important events are all clearly recorded by the geochemical characteristics of REEs in the core. 相似文献
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青藏高原抬升加热气候效应研究的新进展 总被引:30,自引:4,他引:26
对近4年来关于青藏高原加热影响气候的研究进行回顾.首先介绍利用位涡方程和热力适应理论,揭示;夏季高原上空低层气旋式及高层反气旋式环流结构稳定维持的动力学机理.结果表明高原加热作用造成的低层正涡源是低层气旋式环流得以稳定维持的重要原因.而边界层摩擦产生的负位涡是平衡正位涡的主要因素.高原加热还在高原上空形成负位涡,它影响着盛夏的大气环流,是青藏高原上空强大而稳定的反气旋环流得以维持的重要因素.在春夏过渡季节青藏高原非绝热加热对大气环流季节变化以及亚洲季风爆发的影响力方面,进一步确认了感热加热在过渡季节早期(5月中旬以前)环:流演变中的重要作用.青藏高原非绝热加热的时间演变引起了海陆热力差异对比的变化,使副热带高压带首先在孟加拉湾东部断裂,亚洲季风因而在孟加拉湾爆发.结果还表明,用纬向风垂直差异的时空分布能更准确地表示季节变化的区域差异.在青藏高原非绝热加热与北半球环流系统年际变化的联系方面,发现夏季青藏高原的加热强(弱)的年份,高原感热加热气泵(SHAP)高(低)效工作,使高原加热对周边地区低层暖湿空气的抽吸效应和对高层大气向周边地区的排放作用加强(减弱),高原及邻近地区的上升运动,下层辐合和上层辐散均增强(减弱),从而影响着高原和周边地区的环流以及亚洲季风区大尺度环流系统.而且高原的加热强迫还能够激发产生一支沿亚欧大陆东部海岸向东北方向传播的Rossby波列,其频散效应可影响到更远的东太平洋以至北美地区的大气环流.研究还表明,盛夏的南亚高压存在"青藏高压型"和"伊朗高压型"的双模态,它们与高原加热状态有关,且显著地与亚洲季风区的气候分布密切联系. 相似文献
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125.
利用耦合的全球海气模式(NCAR CCSM3), 对青藏高原春季土壤湿度异常影响我国夏季7月降水的机制进行了数值模拟。结果表明, 高原6~62 cm深度的中层土壤湿度异常与表层土壤湿度异常有很好的一致性, 相对而言, 中层土壤湿度异常的持续性较好。若5月高原中层土壤偏湿, 则春末至夏初高原地面蒸发、 潜热通量增加, 而感热通量、 地面温度降低, 高原表面的加热作用减弱, 使得印度高压西撤偏晚, 环流系统的季节性转换偏晚, 东亚地区形成有利于我国夏季出现第I类雨型的环流分布形势, 使我国东部雨带偏北, 华北地区多雨, 江淮地区降水偏少, 华南地区降水偏多; 反之亦然。 相似文献
126.
A physically-based multi-layer snow model Snow-Atmosphere-Soil-Transfer scheme(SAST)and a land surface model Biosphere-Atmosphere Transfer Scheme(BATS)were employed to investigate how boreal forests influence snow accumulation and ablation under the canopy.Mass balance and energetics of snow beneath a Scots pine canopy in Finland at different stages of the 2003-2004 and 2004 2005 snow seasons are analyzed.For the fairly dense Scots pine forest,drop-off of the canopy-intercepted snow contributes,in some cases,twice as much to the underlying snowpack as the direct throughfall of snow.During early winter snow melting,downward turbulent sensible and condensation heat fluxes play a dominant role together with downward net longwave radiation.In the final stage of snow ablation in middle spring,downward net all- wave radiation dominates the snow melting.Although the downward sensible heat flux is comparable to the net solar radiation during this period,evaporative cooling of the melting snow surface makes the turbulent heat flux weaker than net radiation.Sensitivities of snow processes to leaf area index(LAI)indicate that a denser canopy speeds up early winter snowmelt,but also suppresses melting later in the snow season. Higher LAI increases the interception of snowfall,therefore reduces snow accumulation under the canopy during the snow season;this effect and the enhancement of downward longwave radiation by denser foliage outweighs the increased attenuation of solar radiation,resulting in earlier snow ablation under a denser canopy.The difference in sensitivities to LAI in two snow seasons implies that the impact of canopy density on the underlying snowpack is modulated by interannual variations of climate regimes. 相似文献
127.
以JASON-2卫星在上升和下降轨迹中所形成的交叉点的东海局部海域作为研究区域,以3个交叉点作为研究的实验点,SWAN模式基于1'-0.5'(间隔为0.1')的三角形水深网格的分辨率,对东海局部区域模拟2011年1-8月份的波浪数值,并将模拟的结果与JASON-2卫星的有效波高进行对比,结果表明,采用局部加密的三角形网格能够提高波浪数值模拟的精度,在采用有限三角形网格分辨率情况下,模拟精度随着网格分辨率的规律性增加呈现不规则递增现象,同时,设备运算效率会出现指数似的降低。通过对运算结果的统计可知,采用0.6'的三角形水深网格的分辨率获得模拟结果中精度幅度提高最大,同时加密的三角形网格主要对水深梯度较大的东南区域作用效果明显。 相似文献
128.
引言(又名前言、序言、概述)经常作为论文的起始段落,主要回答"为什么做该项研究"这个问题,细分起来又可包括两个方面的内容,一是问题从何说起,即问题的出处,二是问题为何提出,即提出的必要性. 相似文献
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刘新秒 《前寒武纪研究进展》2009,(4):309-309
参考文献只列出公开发行书刊、正是的学位论文和地质报告,非公开发行者用脚注表示。标注参考文献一定要内容全面,一般包括下列几项:1)主要责任者(专著作者、论文集主编、学位申报人、报告撰写人、期刊文章作者、析出文章作者等),为了节省版面,一般在人名多于三个时,仅列出前三个,其它用“等”字代替, 相似文献