青藏高原隆升、琼东南盆地沉降和西沙岛礁发育之间的耦合关系   总被引：1，自引：0，他引：1  

毕东杰  张道军  翟世奎  刘新宇  修淳  张爱滨  曹佳琪 《海洋学报》2017,39(1):52-63

本文基于琼东南盆地15口钻井和西沙石岛岛礁“西科一井”的钻井资料,结合过井地震剖面,系统分析了琼东南盆地沉降（沉积充填）和西沙岛礁生长速率及其变化特征,探讨了青藏高原隆升与琼东南盆地沉降和西沙岛礁发育之间的耦合关系,三者在发育时间和发育过程上表现出高度的一致性,且南海古海水中Sr同位素组成变化也表现出对青藏高原隆升速率变化很好的响应。相对于深水区,浅水区的沉积物堆积速率及其变化能够更好地反映盆地的沉降速率及其变化。琼东南盆地的沉降（沉积物堆积）和西沙岛礁的发育过程均可以分为3个阶段,分别对应于青藏高原的3个隆升期,时间自老到新分别为:23~16 Ma BP、16~5.5 Ma BP、5.5 Ma BP至今。相比而言,岛礁的发育过程与青藏高原的隆升之间的耦合关系更为密切。在青藏高原的快速隆升期,相应发生盆地沉降（沉积充填或沉积物堆积）和岛礁生长速率的加快,同时对应发生了南海海水87Sr/86Sr比值的增大,说明青藏高原隆升可能是影响琼东南盆地乃至整个南海沉降（沉积充填）、岛礁发育和古海水Sr同位素组成变化的主要因素。  相似文献   

Annual growth rings of the shrub Anarthrophyllum rigidum across Patagonia: Interannual variations and relationships with climate     

A.M. Srur  R. Villalba 《Journal of Arid Environments》2009,73(12):1074-1083

Annual growth rings are well-defined in some shrubby species distributed along the Patagonian steppe and provide useful information to identify the environmental factors that influence the radial growth of shrubs in the region. However, little is known about variations in ring width from these species and their relationships with local environment. In this paper we present 18 growth ring width chronologies covering the last 2–3 decades from the shrub Anarthrophyllum rigidum (Fabaceae) encompassing most of its natural range of distribution in Argentina. Interannual variations in growth were first analyzed collectively to identify common regional patterns. In addition, shrub growth at each site was compared with local climate records and site-specific characteristics. Based on a principal component analysis (PCA), sites were joined in four major groups related to the site proximity to the Andes (foothills versus Patagonian plateau) and latitude (north versus south Patagonia). The relatively similar percentage of PCA variance associated with each group reflects environmental differences among sites. Consistent with this observation, we noted large variability in the responses of the A. rigidum woody growth to regional climatic fluctuations. At most sites, this species is favored by abundant winter precipitation, warmer spring and autumn temperatures (controlling the duration of the growing season), cool summers, or a combination of these factors. However, deviations from these patterns are also recorded. Our study represents the first large-scale dendroclimatological analysis of a shrubby species in southern South America. The results presented here provide information on the main patterns and factors affecting the growth of A. rigidum in Patagonia, and may be useful for determining well-suited practices for management and conservation of this ubiquitous species.  相似文献   

多尺度地理空间点群目标相似关系的计算研究   总被引：1，自引：0，他引：1  

江浩  褚衍东  闫浩文  郭丽峰 《地理与地理信息科学》2009,25(6)

研究多尺度地理空间点群目标相似关系的计算问题.基于4类点群信息,将点群目标包含的信息重新分成统计信息、专题信息、拓扑信息、几何信息和度量信息,这5类信息是影响点群相似性程度的主要因子.根据这5类信息描述参数的特点,给出了各个因子的相似度计算公式,建立了多尺度地理空间点群目标相似关系的计算模型,并通过算例验证了该模型的可行性与有效性,为地图综合质量的评价提供了一种新方法.  相似文献   

循环荷载作用下高温-高含冰量冻土特性试验研究   总被引：3，自引：0，他引：3  

高志华  赖远明  熊二刚  李波 《岩土力学》2010,31(6):1744-1751

为了研究高温-高含冰量冻土这种极不稳定土体的动力学特性,开展了固结围压为0.3、0.5、1.0、3.0、5.0 MPa,控制温度为-0.5、-1.0、-2.0、-4.0 ℃、初始含水率为50%的高含冰量青藏线重塑冻土的动三轴试验。根据试验结果,提出了用广义的双曲线模型来描述动应力-应变关系,并且给出了模型参数预报关系式;基于动弹性模量和轴向应变之间的非线性关系,提出?3 =0.5 MPa为临界围压。当围压大于0.5 MPa时,动弹性模量随着动应变的增大呈减小的趋势;当围压小于0.5 MPa时,动弹性模量随着动应变先增大后又减小;此外,动阻尼比随应变幅值和围压的增大而增大,随着温度的降低,动阻尼比变小。  相似文献   

鄂尔多斯盆地延长组高自然伽马砂岩储层特征   总被引：10，自引：0，他引：10       下载免费PDF全文

张小莉  冯乔  孙佩  李渭 《地球物理学报》2010,53(1):205-213

鄂尔多斯盆地延长组岩芯分析与测井特征研究表明,相对高自然伽马砂岩具有高长石、高Th、局部高U、K含量变化不大的共同特征,Th、U含量特征与凝灰岩极为相似;相对高自然伽马砂岩具有相对高自然伽马、高声波时差、低电阻率值的测井曲线特征,与凝灰岩测井曲线特征也极其相似;再者,从长6到长4+5油层组的各亚组,凝灰岩层逐渐不发育的同时,伴随相对高自然伽马砂岩发育程度依次增强;上述3项特征预示着延长组相对高自然伽马砂岩可能为同沉积期或较先期沉积的凝灰岩经搬运后作为砂岩组成部分再沉积形成的.四性关系研究表明：（1）依据自然伽马-自然电位曲线重叠图、声波时差-自然电位曲线重叠图,可快速识别相对高自然伽马砂岩;（2）相对高自然伽马砂岩具有相对发育的次生孔隙,非均质性强,一般物性越好,声波时差-自然电位曲线重叠图幅度差越大;（3）计算自然电位-自然电位曲线重叠图的幅度差,反映相对高自然伽马砂岩含油性,幅度差越大,表明其含油性越好.  相似文献   

What is the role of the model in socio-hydrology? Discussion of “Prediction in a socio-hydrological world”*     

Lieke Anna Melsen  Jeroen Vos  Rutgerd Boelens 《水文科学杂志》2020,65(Z2):1435-1443

ABSTRACT

Srinivasan et al. provide an interesting overview of the challenges for long-term socio-hydrological predictions. Although agreeing with most of the statements made, we argue for the need to take socio-hydrological analysis a step further and add some fundamental considerations, especially concerning the crucial importance of many (conscious and unconscious) assumptions made upfront of the modelling exercise. Eventual assumptions of technological determinism need correction: Models are not “value-free”, but uncertain, subjective and a product of the society in which they were shaped. It is important to acknowledge this uncertainty and bias when making decisions based on socio-hydrological models, considering also that these models are “social and political actors” in and by themselves. Furthermore, socio-hydrological models require a transdisciplinary approach, since physical water availability is only one of the boundary conditions for society. Last but not least, interaction with stakeholders remains important to enable understanding of what the variable of interest is.  相似文献   

秦岭-黄淮平原交界带地表径流与其时间变化的关系分析   总被引：2，自引：1，他引：1  

管华  李斌 《地理科学》2004,24(3):281-285

根据秦岭-黄淮平原交界带及其邻近地区42个径流站1962~1999年的观测资料,分析了地表径流量及其时间变化(年内分配和年际变化)的空间分布规律,得出二者之间存在正相关关系的结论,并探讨了这种反常现象的成因。  相似文献   

Dehydration of clastic sediments in subduction zones: Theoretical study using thermodynamic data of minerals     

Ying Li  Hans‐Joachim Massonne  Arne Willner  Hong‐Feng Tang  Cong‐Qiang Liu 《Island Arc》2008,17(4):577-590

Pseudosections for two sediments and one basalt calculated in the system K₂O–Na₂O–CaO–MgO–FeO–Fe₂O₃–Al₂O₃–TiO₂–SiO₂–H₂O for the P–T range 10 to 35 kbar, 300 to 900°C give useful insights into the amount of H₂O released from oceanic crust in subduction zones. In cold subduction zones (20 kbar–300°C to 35 kbar–500°C) hydrous minerals storing 3 to 4 wt% H₂O are still present in metasediments at depths of 120 km. In the same environment, metabasite releases 1 wt% H₂O in the depth range 100 to 120 km, but 4.5 wt% H₂O is transported to greater depths. In hot subduction zones (300°C hotter than the cold subduction zone at 100 km depth), dehydration events of metasediments in the depth range 50 to 80 km correspond to the breakdown of chlorite and paragonite. In the calculations no further water is released at greater depths because the modal content of phengite, the only hydrous mineral phase at these depths, remains almost constant. For the same P–T path, metabasite shows continuous dehydration between 40 and 80 km releasing almost 3 wt% H₂O. At 120 km depth less than 0.4 wt% of H₂O remains. In an average modern subduction zone (～6°C/km) most dehydration of sediments occurs at depths of 70 to 100 km and that of basalts at depths of 80 to 120 km. Only 1.3 wt% H₂O in metasediments and 1.6 wt% H₂O in metabasalt has the potential to be subducted to depths greater than 120 km. The dehydration behavior of sediments concurs with the generally held idea that subduction zone fluids are most effectively transported to great depths by cold subduction. In hot subduction zones, such as those characteristic of early Earth, most H₂O carried by oceanic crust is liberated at depths less than 120 km and, thus, would not contribute to island‐arc magmatism.  相似文献   

太湖不同形态异味物质含量、相互关系及其与环境因子关系的探讨   总被引：1，自引：0，他引：1  

齐敏  孙小雪  邓绪伟  陈隽  谢平 《湖泊科学》2013,25(1):31-38

根据2009年6月到2010年5月太湖水样中溶解态和结合态异味化合物(2-甲基异茨醇(MIB)、土嗅素(GEO)、β-环柠檬醛、β-紫罗兰酮)的月间采样分析结果,综合考虑各种环境因子以及蓝藻种属,探讨了溶解态和结合态异味化合物之间的关系以及影响太湖中异味化合物的主要环境因子.结果表明溶解态MIB和结合态β-环柠檬醛、β-紫罗兰酮是研究期间湖水中的主要异味化合物,这些物质对于太湖水体发生异味具有较大贡献或较大潜在贡献.通过本文研究和对以往文献讨论推测,太湖中溶解态和结合态异味化合物相关关系较弱的原因可能是,异味化合物生产和释放速率的变化、微生物降解、光解、吸附和挥发等.同时发现微囊藻和叶绿素a与太湖异味化合物关系密切.蓝藻水华对于太湖异味化合物的发生具有重要影响,控制蓝藻水华发生的关键是控制或减缓太湖异味问题.  相似文献   

球状星团NGC4147基于依巴谷系统的自行和空间运动     

王家骥  武振宇 《天文学报》1999,40(3):335-336

王家骥等［１］曾得到球状星团ＮＧＣ４１４７的绝对自行为（－２．８２±０．４９,２．３７±０．４３）ｍａｓ／ｙｒ．但是,其中所用的参考星表是Ｂｒｏｓｃｈｅ等［２］１９８５年发表的结果,含有ＡＧＫ３星表的系统误差．在Ｄａｕｐｈｏｌｅ等［３］给出的２６个球状星团轨道远银心距（ａｐｏｇａｌａｃｔｉｃｄｉｓｔａｎｃｅ）与金属度［Ｆｅ／Ｈ］的关系图上,ＮＧＣ４１４７处于一个特殊的位置,即按照它的远银距（５２ｋｐｃ）,它的金属度［Ｆｅ／Ｈ］应该大于－２．０,但实际上只有－１．８３［４］．类似的问题在文［１］的…  相似文献