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141.
SEED格式STEIM2数据压缩算法在实时地震数据传输中的应用 总被引:9,自引:1,他引:8
在一定带宽内,及时、高效、无失真地传输地震数据是地震数据传输的基本要求,SEED格式给出的数据格式在数据压缩方面有其独到之处,但SEED格式没有定义数据正确性和完整性保证机制和检验方法,因而影响实时传输中的使用。本文提出一种基于SEED格式的STEIM2数据压缩算法,同EDAS数据包形式兼容的实时压缩数据包编码方法,来实现实时压缩数据的传输。经理论评估和实际数据检验,它容易实现,效率高,安全,可靠,完全可以应用于实时数据传输。 相似文献
142.
In this paper,the quantitative relationship between the wild fruit communities and direct environmental factors is discussed on the basis of detailed data on landscape scale habitats obtained through field vegetation investigation.The results from TWINSPAN and DCCA showed that:1) In the distribution sections of the wild fruit forest in the Keguqin Mountain region,the basic patterns characteristic of the different habitats are due to topographic factors,nutrients and moisture conditions;2) The elevation affected the most basic differentiation of plant communities in the study area,indicating that the elevation condition was the most important factor restricting the distribution of the wild fruit communities in the study area;3) The close relationship between the moisture content in the upper soil layer and the elevation reflected the influence of moisture conditions on both wild fruit and herb-layer communities;4) Nutrient differences not only indicated that the habitat conditions were different in themselves but also showed that the present nutrient conditions of the habitats were seriously affected by human activities.In summary,under complicated mountainous topographic conditions,the habitat conditions for the communities differed very significantly,and the combination of elevation,soil moisture content,total nitrogen,slope aspect,and pH value influenced and controlled the formation of community distribution patterns in the study area. 相似文献
143.
绿岩带是太古宙大陆地壳重要的构造单元。 按照岩石组合特征, 绿岩带可划分为 3 个类型:1) 巴伯顿型, 主要由基性-超基性火山岩组成, 含少量酸性火山岩及沉积岩, 中性火山岩很不发育;2) 苏必利尔型, 主要由中性火山岩和中-基性火山岩组成, 含沉积岩; 3) 达尔瓦尔型, 以广泛发育的沉积岩为特征。 其中, 巴伯顿型绿岩带在世界范围内分布较广, 且组成较为复杂, 表现出一系列独特的岩石学和地球化学特征:1) 基性-超基性火山岩在绿岩带层序中占主导地位;2) 发育具有异常高的地幔潜能温度的科马提岩类;3) 存在太古宙亏损型和富集型玄武岩等。 华北克拉通清原地区的表壳岩虽然经历高级变质作用, 但仍 具有清晰的层序, 与巴伯顿型绿岩带岩石组合特征类似, 因此我们倾向于将其厘定为清原绿岩带。 清原绿岩带主体形成于 2.5 Ga, 与广泛分布的新太古代花岗质片麻岩形成时代一致, 并不存在大规模的中太古代地质体。 清原绿岩带的岩石学和地球化学研究表明新太古代晚期原始地幔柱模型可以较为合理的解释清原地区及华北克拉通东部陆块其它新太古代基底岩石的成因, 但太古宙原始地幔柱与显生宙地幔柱在某些方面有所不同。 相似文献
144.
本文对躬穷左波Fe-Cu矿区出露的三套酸性侵入岩进行了系统的LA-ICP-MS锆石U-Pb年代学和岩石地球化学研究。年代学测试结果显示花岗斑岩、二长花岗斑岩和钾长花岗岩~(206)Pb/238U加权平均年龄分别为147.0 Ma、143.6 Ma和142.8 Ma,矿区存在晚侏罗世—早白垩世存在3期岩浆事件。岩石地球化学组成特征显示,花岗斑岩属准铝质-弱过铝质I型花岗岩;二长花岗斑岩为高钾钙碱性系列,属弱过铝质I型花岗岩;钾长花岗岩经历了强烈的结晶分异作用,属高分异I型花岗岩。岩石微量元素富集Rb、Th、U、Pb而亏损Nb、Ta、Ti、P元素,Nb/Ta比值接近大陆地壳组成及锆石负的εHf(t)值特征,指示成岩物质以壳源物质为主。躬穷左波晚侏罗世矽卡岩型Fe-Cu矿化事件的发现对于完善班—怒带西段成矿规律和指导区域找矿工作具有重要意义。 相似文献
145.
全面分析了气候变化给企业带来的机遇与挑战。全球契约的"关注气候"倡议为企业响应全球号召应对气候变化带来了机遇,全球契约是全球企业共同应对气候变化、实现企业社会责任和树立企业形象的良好平台。另外,通过调查研究分析了中国民营企业应对气候变化的现状,并提出了相关政策建议。 相似文献
146.
地震计阶跃标定自动处理算法研究 总被引:1,自引:0,他引:1
标定是监测运行中的地震计主要技术参数的有效手段,保证了观测数据的产出质量。本文介绍了一种新的地震计阶跃标定算法,旨在提高算法的稳定性和自动化程度,适合计算机自动的,成批的处理标定数据。 相似文献
147.
To reconstruct the productivity changes for the last 10 500 a in the northeastern East China Sea (ECS), biogenic compounds (such as carbonate, organic carbon and opal), marine micropaleontological fossils (planktonic foraminifera, benthic foraminifera, radiolarian and silicoflagellate) and the compositional characters of benthic foraminifera fauna analyses were carried out on a sediment core DOC082 obtained from the western slope of Okinawa Trough (29°13.93′N, 128°08.53′E; 1 128 m water depth). The long-term changes of biogenic and micropaleontological proxies display some similarities through the last 10 500 a, which show three different phases: lower values are recorded during the early and middle Holocene (before about 4 000 a BP), followed by an abrupt and remarkable increase at about 4 000 a BP, the late Holocene (after about 3 000 a BP) is characterized by continuously high values. The multi-proxy data of paleoproductivity and percents of benthic foraminifera genera (Uvigerina and Bulimina) show that during the early and middle Holocene (10 500–4 000 a BP) productivity was relatively low with a sudden and distinct increase at about 4 000 a BP, and the late Holocene (3 400–0 a BP) is marked by significantly higher productivity. Also, the radiolarian-based sea surface temperature (SST) records reveal a distinct decline in SST in the late Holocene after 3 200 a BP, very different from the early and middle Holocene. For the last 3 000 a, the enhanced biological productivity and distinctly lower SST indicate a major change of oceanographic conditions in the northeastern ECS. These marine environmental anomalies are consistent with other paleoclimatic records for the late Holocene in the Chinese continent and its surrounding regions. After analyzing the mechanisms of modern productivity and SST changes in the northeastern ECS, and based on the climatic anomalies in the Chinese continent and variations in the Kuroshio Current during modern El Niño periods, we suggest that the anomalous environmental conditions in the northeastern ECS may imply intensified El Niño activity during the late Holocene. 相似文献
148.
Pathways of mesoscale variability in the South China Sea 总被引:5,自引:0,他引:5
The propagation of oceanic mesoscale signals in the South China Sea (SCS) is mapped from satellite altimetric observations
and an eddy-resolving global ocean model by using the maximum cross-correlation (MCC) method. Significant mesoscale signals
propagate along two major bands of high variability. The northern band is located west of the Luzon Strait, characterized
by southwestward eddy propagation. Although eddies are the most active in winter, their southwestward migrations, steered
by bathymetry, occur throughout the year. Advection by the mean flow plays a secondary role in modulating the propagating
speed. The southern eddy band lies in the southwest part of the SCS deep basin and is oriented in an approximately meridional
direction. Mesoscale variability propagates southward along the band in autumn. This southward eddy pathway could not be explained
by mean flow advection and is likely related to eddy detachments from the western boundary current due to nonlinear effects.
Our mapping of eddy propagation velocities provides important information for further understanding eddy dynamics in the SCS. 相似文献
149.
<正>A theoretical model of a friction pendulum system(FPS) is introduced to examine its application for the seismic isolation of spatial lattice shell structures.An equation of motion of the lattice shell with FPS bearings is developed.Then, seismic isolation studies are performed for both double-layer and single-layer lattice shell structures under different seismic input and design parameters of the FPS.The influence of frictional coefficients and radius of the FPS on seismic performance are discussed.Based on the study,some suggestions for seismic isolation design of lattice shells with FPS bearings are given and conclusions are made which could be helpful in the application of FPS. 相似文献
150.