吉林省西部月亮湖沉积物的²¹⁰Pb和¹³⁷Cs测年及沉积速率   总被引：3，自引：0，他引：3  

柴社立  高丽娜  邱殿明  柴源  郭佳  徐学纯 《吉林大学学报(地球科学版)》2013,(1):134-141

在吉林省西部月亮湖沉积柱中137 Cs和210Pb比活度测定的基础上,进行了沉积柱137 Cs和210Pb测年和现代沉积速率研究。月亮湖沉积柱在18cm和32cm处存在2个明显的137 Cs峰值,所对应的时标分别为1986年和1963年,据此时标计算的1963 2006年月亮湖的平均沉积速率为0.74cm/a,19862006年平均沉积速率为0.90cm/a。对比了CIC、CRS和CFCS模式的210Pb计年结果,其中:CIC模式的计年结果明显偏离137 Cs时标;64cm以浅沉积物的CRS、CFCS模式计年结果接近,并与137 Cs时标基本一致;但当沉积物的深度大于64cm时,CRS、CFCS模式计年结果具一定差别,鉴于此深度以下CFCS模式计年的指数方程的相关系数较低,其计年结果的代表性较差,因此,此深度以下采用CRS模式计年。根据CRS模式计年结果计算的月亮湖沉积速率为:1835 1898年平均为0.33cm/a,1898 1920年平均为1.09cm/a,1920 1961年平均为2.21cm/a,1961 2006年平均为0.94cm/a。沉积速率的年际变化反映了月亮湖及其流域内自然环境变化和人类活动的影响程度。  相似文献   

川东北地区某顺层滑坡的破坏机制研究     

安世泽  刘宗祥  周小义  邹维勇 《地质灾害与环境保护》2013,24(1):14-19

通过对该挖方滑坡的地质条件、岩土体结构、软弱结构面特征、变形特征及监测数据的分析,并采用FLAC3D进行数值模拟,探讨川东北红层地区软弱夹层岩体边坡的破坏机制,为类似条件边坡的开挖、监测、预警和支护提供参考。  相似文献   

Comparative analysis of transcriptomes from albino and control sea cucumbers, Apostichopus japonicus     

MA Deyou  YANG Hongsheng  SUN Lin  XU Dongxue 《海洋学报(英文版)》2014,33(8):55-61

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社交网络不良信息传播模型研究     

安俊秀  曹书哲  王鹏 《成都信息工程学院学报》2014,29(3):255-260

当前社交网络的信息传播模型主要是对病毒SIR模型的改进而形成的,因其主体不同而具有不完善性,为更好地揭示不良信息在社交网络中的传播规律,从而寻找预防和控制不良信息传播的最优方法。根据社交网络中信息传播的方式和特点,与传染病动力学理论结合构建出SEIR模型来研究不良信息在社交网络中的传播。模型定义了4种传播规则,分析不良信息在不同状态用户之间的传播过程,并且应用扩散核函数和空间协方差方程对相关参数进行了分析。最后通过对比实验说明调节控制率γ的大小对虚假信息在网络中的传播有一定的控制作用。  相似文献   

高分辨率遥感影像的建筑物自动提取   总被引：1，自引：0，他引：1  

安文  杨俊峰  赵羲  史玉龙 《测绘科学》2014,39(11):80-84

文章结合结构图分析方法,提出一种针对高分辨率遥感影像中建筑物自动提取方法.该方法利用几何限制对线基元进行初连接,解决由于边缘检测无法完整提取建筑外边缘问题;通过构造结构图确立线基元之间连接关系,搜索结构图中闭合路径,建立高级别特征,对过于散列的线基元进行整合;在此基础上,综合考虑建筑物的几何结构、光谱特征等图像信息筛选闭合路径,实现对建筑物的提取.最后通过对天绘一号高分辨率遥感影像进行建筑物自动提取验证了该方法的有效性.  相似文献   

天津市农村宅基地确权登记发证工作流程的探讨     

安卫  戈扬  陈玲  倪旸  廖益涛 《北京测绘》2014,(6):117-121

2012年11～12月份,天津市国土房管部门开始进行农村宅基地确权登记发证的试点工作,我区选取精武镇小卞庄村作为试点村进行调查。本文详细地介绍了农村宅基地实地调查的基本原则、总体要求和工作流程,摸索出一套合理、高效的工作流程,为以后的宅基地调查工作的大面积铺开奠定坚实的基础。  相似文献   

平面六边形格网上格点多边形的面积计算方法     

李凯  童晓冲  贲进  安源 《测绘科学技术学报》2014,(4)

全球离散格网系统是一种新型的全球多尺度空间数据模型,相关问题的研究已引起学术界的广泛关注并已取得可喜进展。其中,格网量测体系的建立是当前学术界的研究难点,同时也是格网实用化必须解决的核心问题。文中将平面六边形格网上任意覆盖区域抽象为"格点多边形",推导并证明了其面积计算公式,通过对比算例验证了结论的正确性和优越性。  相似文献   

三江源区植被 NDVI 对区域气候的时滞效应分析     

安如  徐晓峰  杨仁敏 《东北测绘》2014,(2):1-5

以三江源区为研究区,主要利用一元线性趋势法和简单相关分析法分析了源区1982～2004年生长季累积NDVI的时间序列变化特征及其与气温、降雨、光照时间、风速、地表温度这些气候因子之间的相关性,从月尺度上研究了三江源区植被NDVI对气候因子响应的滞后性特征。最后表明,生长季累积NDVI对气温的滞后期为1个月,对风速的滞后期为2个月,对地表温度的滞后期为4个月,而对降雨量和日照时数不存在滞后响应或者滞后期小于1个月。  相似文献   

Remote sensing survey and research on internal solitary waves in the South China Sea-Western Pacific-East Indian Ocean (SCS-WPAC-EIND)     

Junmin Meng  Lina Sun  Hao Zhang  Beilei Hu  Fucheng Hou  Sude Bao 《海洋学报(英文版)》2022,41(10):154-170

Internal solitary waves (ISWs) are common mesoscale dynamic processes in the ocean that are spread throughout the world’s oceans. The South China Sea (SCS), Western Pacific (WPAC) and Indian Ocean (EIND) (SCS-WPAC-EIND) are areas where ISWs frequently occur. In particular, in the northern part of the South China Sea, Sulu Sea, Celebes Sea, Andaman Sea, Lombok Strait and northeastern part of Taiwan Island, ISWs exist almost year-round. Remote sensing is an important technique to carry out investigations and research on ISWs on a large scale. In particular, optical sensors represented by the Moderate Resolution Imaging Spectroradiometer (MODIS) can observe ISWs for a long time and on a large scale, while SAR sensors such as Sentinel-1 A/B can compensate for the deficiencies in optical sensors and comprehensively observe ISWs. Based on many years of remote sensing surveys of ISWs, this paper uses MODIS and Sentinel-1 satellite remote sensing images of more than 70 000 scenes from 2010 to 2020 to carry out survey studies of ISWs in the SCS-WPAC-EIND. The survey systematically gives the temporal and spatial distribution characteristics of ISWs in the SCS-WPAC-EIND and focuses on the analysis of the ISW characteristics in main areas in the SCS-WPAC-EIND, thereby providing basic data for further research on ISWs.  相似文献   

Impact of faulting in depocentres development,facies assemblages,drainage patterns,and provenance in continental half-graben basins: An example from the Fanja Basin of Oman     

Camilla L. Würtzen  Alvar Braathen  Miquel Poyatos-Moré  Mark J. Mulrooney  Lina H. Line  Ivar Midtkandal 《Basin Research》2023,35(2):705-743

Fault throw gradients create transverse folding, and this can influence accommodation creation and sedimentary routing and infill patterns in extensional half-graben basin. The Fanja half-graben basin (Oman) offers an excellent outcrop of an alluvial fan succession displaying cyclical stacking and basin-scale growth-fold patterns. These unique conditions allow for an investigation of fault-timing and accommodation development related to fault-transverse folding. Our study combines geological mapping, structural analysis, sedimentary logging and correlation, and bulk mineralogical compositions. Mapping reveals that the basin is bounded by a regional-scale fault, with local depocentres changing position in response to transverse syncline and anticline development ascribed to fault-displacement gradients. The alluvial Qahlah Formation (Late Cretaceous) is unconformably overlying the Semail Ophiolite, and is in turn overlain by the marine Jafnayn Formation (Late Palaeocene). Facies and stratigraphic analysis allows for subdivision of the Qahlah Formation into four informal units, from base to top: (i) laterite in topographic depressions of the ophiolite, (ii) greenish pebbly sandstones, deriving from axially draining braided streams deposited in the low-relief half-graben basin. This green Qahlah grades vertically into the red Qahlah, formed by alluvial fanglomerates and floodplain mudstones, with drainage patterns changing from fault-transverse to fault-parallel with increasing distance to the main fault. The red Qahlah can be divided into (iii) the Wadi al Theepa member, found in a western basin depocentre, with higher immaturity and sand: mud ratio, suggesting a more proximal source, and (iv) the Al Batah member, located in the eastern part of the basin. The latter shows better sorting, a lower sand: mud ratio, and more prominent graded sub-units. It also shows eastward expansion from an orthogonal monocline, ascribed to accommodation developed in a relay ramp. Changes in sedimentary facies and depositional patterns are consistent with differential mineralogical composition. The Green Qahlah is composed of quartz and lithic mafic rock fragments, sourced from the ophiolite and schists of the metamorphic basement. The Red Qahlah is composed of chert and kaolinite sourced from the Hawasina Nappe succession in the footwall of the master fault. These changes in source area are linked to unroofing of fault-footwalls and domal structures during the extensional collapse of the Semail Ophiolite. The novelty of this study resides in linking sedimentology and fault-displacement events controlling fault-perpendicular folding, and its influence on depocentre generation and stratigraphic architecture. This is an approach seldom considered in seismic analysis, and rarely analysed in outcrop studies, thus placing the results from this study among the key outcrop-based contributions to the field.  相似文献