A seismic reflection and GLORIA study of compressional deformation in the Gorringe Bank region, eastern North Atlantic

Seismic reflection and GLORIA side-scan sonar data obtained on RRS Charles Darwin cruise CD64 reveal new information on the styles of deformation in the Gorringe Bank region, at the eastern end of the Azores–Gibraltar plate boundary. Previous studies suggest that Gorringe Bank was formed by the overthrusting of a portion of the African plate upon the Eurasian plate. The new seismic data show, however, that the most intensely deformed region is located south of Gorringe Bank, on the northern flanks of a NW–SE-trending submarine ridge which includes the Ampere and Coral Patch seamounts. The deformation is expressed as long-wavelength (up to 60  km), large-amplitude (up to 800  m) folds in the sediments and underlying acoustic basement, which in places are associated with one or more reverse faults, and as a fabric of short-wavelength folds (up to 3  km) with a NE trend. In contrast, the same sedimentary units when traced beneath the flanking plains are undeformed, except for some faults with a small throw (~30  m), some of which offset the seafloor. GLORIA data show that recent deformation is broadly distributed over the region. Structural trends rotate from 45° in the west to 70° in the east of the region, nearly perpendicular to the NW-verging plate motion vectors as determined from plate kinematic models. Flexure modelling suggests that a portion of Gorringe Bank has loaded 152  Ma oceanic lithosphere and that a maximum of 50  km of shortening has occurred at Gorringe Bank since the mid-Miocene. Our observations support a model in which there is no single plate boundary in the region, rather that the deformation is distributed over a 200–330  km wide zone.     

应用人工神经网络识别华南沿海全新世海滩岩和海岸沙丘岩

华南全新世海岸沙丘岩和海滩岩同是热带、亚热带海岸线附近的胶结的岩石,其沉积儿构造极为相似,很容易混淆。人工神经网络是最近发展起来的一种信息处理方法,可以处理模糊的,非线性的、含有噪声的数据,为海滩岩和沙丘岩的识别提供了一种新方法。用华南海岸风成砂和海滩砂的粒度参数作为训练样本,华南海岸全新世沙丘岩和海滩碉的粒度参数作为测试样本,经过训练的Ｂ－Ｐ网络能够根据海滩砂和海岸沙丘砂的粒度参数来区分大部分的     

Networking

This essay outlines the ways that networks structure opportunities foremployment and advancement and the ways that networks build frameworks of support, particularly for women in geography. I consider the evidence supporting the contention that personal contacts and social networks affect careeroutcomes. I then note that each person's networks are likely to be biased in favor of others who share common interests and concerns. In particular, gender affects network composition in significant ways. Because network composition affects how a network functions, it is worth considering the personal and professional advantages of building diverse networks. In the final section I suggest ways to build such networks.     

监测网顾及可区分标准的解析二类设计

在变形体的变形模型不完全清楚的情形下,须用可区分度标准进行监测网的设计。根据展式,首次导出了监测网顾及可区分标准的解析二类设计模型,并对其解算及算例中以说明。     

神经智能信息处理系统的研究现状及其在水文水资源中的应用展望

从神经网络(NN),模糊系统(FS)和进化算法(EC)三者相结合的角度,介绍了神经智能信息处理系统的研究现状,讨论了该系统在水文水资源中的应用,并对其应用发展趋势进行了预测。     

变形参考系及不同变形参考系中变形数据的联合处理

本文首先讨论了变形参考系及实现方法,然后讨论了不同变形参考 变形的数据统一问题。在此基础上,建立了欧亚板块东南部块体的块体变形参考系,并在该块体变形参考系中联合了ＩＴＲＦ９７速度场和中国ＧＰＳ－Ａ级网复测资料计算了中国大陆与周围板块的现今相对运动,进而分析了中国大陆及周转板块的现今相对运动规律。     

Automatic recognition of freight car number

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腾冲火山区微震观测(Ⅱ)

论述了腾冲火山地区流动数字化台网的建设与观测过程。根据腾冲台网记录的各种微震图像,将其进行分类分析。主要有包络型事件、微构造破裂事件、汽爆事件、高频地震和小震群。由震相分析判断热海台记录到岩浆熔融体上的反射ＳxＳ波,腾冲地震台记录到Ｓ波不发育图像。表明腾冲火山区南部存在岩浆熔融体,估计距地表５～８ｋｍ。腾冲台网观测表胆腾冲火山区周边地区地震活动水平明显高于火山区,火山区南部的马鞍山热海一带是腾冲火     

腾冲炎山区微震类型与波谱分析

利用腾冲火山地区流动数字化地震台网的微震资料,对发生于火山区内及附近地区的２４个微小地震事件进行波谱分析。采用布龙模式计算震源参数。研究这些微震震源参数,显示位于火山区南部的热海和马鞍较高,主要以小震群、微破裂及汽爆等方式释放应力。通过对微地震记录事件的时域和频域分析,将腾冲火山地区微地震事件划分为四个类型,即包络型、汽爆型、高频型和震群型。     

配电网GIS中的拓扑分析研究

配电网络拓扑分析是配电管理系统高级应用软件的重要组成部分,其研究具有重要的理论和应用价值。本文就所开发的配电网G IS项目中,提出了基于图论的一种在G IS上构建配电网拓扑模型的算法并给出了其数据结构,将影响配电网拓扑结构的开关、T接点看作节点,将配电变压器和馈线段看作边,利用从属关系反映他们间的连接关系。这种算法节省了拓扑分析的计算时间,适合实时应用。最后,以电源点回溯的实现算法来说明拓扑分析方法的具体应用。经过实际应用表明,基于G IS的配电网拓扑分析方法具有很大的实用性和推广价值。