基于X射线连续谱的光子计数探测器能量标定方法          下载免费PDF全文

李中浩  贠明凯  姜小盼  张志都  程志威  魏存峰  史戎坚  魏龙  王哲 《CT理论与应用研究》2018,27(3):363-372

随着探测器技术的发展，具有能量分辨能力的光子计数探测器在X射线能谱CT成像中应用越来越广泛。能量与阈值的对应关系对能谱CT成像具有重要意义，受到实验条件的限制，目前的光子计数探测器的能量标定方法有一定的局限性。针对光子计数探测器的单像素标定问题，本文提出一种基于X射线光机连续谱的能量标定方法，通过建立和分析X光谱模型，利用光机连续谱中高能端的能量信息，得到阈值与能量之间的关系。实验结果表明该方法操作方便，对探测器单像素标定结果较为准确，对其他类型光子计数探测器的标定具有参考意义。   相似文献   

Structural architecture of Neoproterozoic rifting depression groups in the Tarim Basin and their formation dynamics   总被引：1，自引：0，他引：1  

Bizhu HE  Cunli JIAO  Taizhu HUANG  Xingui ZHOU  Zhihui CAI  Zicheng CAO  Zhongzheng JIANG  Junwen CUI  Zhuoyin YU  Weiwei CHEN  Ruohan LIU  Xiaorui YUN  Guangming HAO 《中国科学:地球科学(英文版)》2019,(3)

The Tarim Basin is the largest, oil-bearing, superimposed basin in the northwest of China. The evolution and tectonic properties of the initial Tarim Basin have been hotly disputed and remain enigmatic. The Neoproterozoic basin is covered by a vast desert and a huge-thickness of sedimentary strata, has experienced multiple tectonic movements, had a low signal to noise ratios(SNRs) of deep seismic reflection data, all of which have posed critical obstacles to research. We analysed four field outcrops, 18 wells distributed throughout the basin, 27 reprocessed seismic reflection profiles with higher SNRs across the basin and many ancillary local 2D and 3D profiles and aeromagnetic data. We found about 20 normal fault-controlled rifting depressions of the Cryogenian and Ediacaran scattered throughout the basin, which developed on the Precambrian metamorphic and crystalline basement. The structural framework is clearly different from that of the overlying Phanerozoic. The rifting depressions consist of mainly half grabens, symmetrical troughs and horst-grabens. From the northeast to southwest of the basin,they are divided into three rifting depression groups with the WNW, ENE, and NW-trends that are mainly controlled by normal faults. The maximum thicknesses of the strata are up to 4100 m. From the Cryogenian to Ediacaran, most of the main inherited faults to active and eventually ceased at the end of the Ediacaran or Early Cambrian, while subsidence centres appeared and migrated eastward along the faults. They revealed that the different parts of the Tarim continental block were in NNE-SSWoriented and NNW-SSE-oriented extensional paleo-stress fields(relative to the present) during the Neoproterozoic, and were accompanied by clockwise shearing. According to the analysis of the activities of syn-sedimentary faults, filling sediments,magmatic events, and coordination with aeromagnetic anomalies, the tectonic properties of the fault depressions are different and are primarily continental rifts or intra-continental fault-controlled basins. The rifting phases mainly occurred from 0.8–0.61 Ga.The formation of the rifting depression was associated with the initial opening of the South Altun-West Kunlun Ocean and the South Tianshan Ocean, which were located at the northern and southern margins of the Tarim Block, respectively, in response to the break-up of the Supercontinent Rodinia and the initial opening of the Proto-Tethys Ocean.  相似文献   

基于天地图的农业农村信息共享服务模式     

黄玉青  郭朝阳  白穆  贠建明  王凯 《北京测绘》2021,35(7):900-905

针对省级农业农村厅专题数据较多且无统一规范、分布广泛、信息孤岛化、数据更新手段落后、跨部门共享困难等问题,在收集、整合、分析宏观分布的业务信息和应用需求基础上,利用地理信息、分布式多源信息集成、海量数据的存储、处理与分析等技术,开展农业农村地理信息共享服务模式研究,设计并实现了省级农业地理信息共享服务平台,包括门户、一张图综合分析、数据管理、服务管理、自助制图等子系统.实现了农业农村信息资源与测绘地理信息资源跨部门的整合、应用与共享,借助于国家、省级基础测绘和"天地图·陕西"成果,保证了农业农村地理信息的权威性、可靠性、鲜活性.通过示范应用的引领作用,推动省农业农村工作的信息化,满足厅机关及直属单位、社会公众、其他部门的应用需求,提高农业农村数据的共享能力,为农业决策提供了空间分析和可视化方法,在农业农村部门日常监管和应急决策中发挥了辅助决策作用.  相似文献   

基于信息化测绘体系的测绘业务管理平台应用     

黄玉青  白穆  张靖  贠建明 《北京测绘》2021,35(10):1288-1293

依据陕西省测绘地理信息局信息化测绘体系建设总体设计方案,针对当前测绘业务管理模式存在的流程多、复杂、效率低等问题,以自然资源部陕西基础地理信息中心信息化测绘业务管理平台建设为例,设计并实现了有序、规范、实时、高效的信息化测绘业务管理解决方案,为提高信息化生产效率、协同管理水平、节约运营成本、促进文化和信息知识体系建设等提供了有力保障,满足了单位办公更加广泛化、精细化的应用需求.该解决方案能对其他单位信息化测绘体系建设具有一定借鉴意义.  相似文献   

汶川地震断裂作用研究新认识   总被引：2，自引：0，他引：2  

王焕  李海兵  司家亮  孙知明  付小方  刘栋梁  裴军令  李成龙  张佳佳  宋圣荣  郭力伟  MORI James  薛莲  BRODSKY E. Emily  云锟  龚正 《地球学报》2015,36(3):257-269

2008年汶川地震后,人们不得不思考问题是:大地震是如何发生的?下一次大地震什么时候发生?也就是涉及地质学家和地球物理学家一直未解决的科学问题:断层是如何破裂的?震后断裂是如何愈合的?我们试图通过对汶川地震断裂带结构、断裂摩擦行为和断裂愈合过程的研究来回答这些问题。本文将介绍通过对地表露头和汶川地震断裂科学钻探一号孔(WFSD)岩心中汶川地震主滑移带的详细研究,以及钻孔中长期温度监测来分析有关汶川地震断裂动态弱化和摩擦行为,并结合钻孔中长期水文监测计算所得断裂带渗透率变化,分析震后断裂愈合过程,进而探讨和认识汶川地震断裂作用所涉及的上述问题。经过详细研究,确定了汶川地震断裂带(映秀—北川断裂带)宽105~240 m、具有五个不同断裂岩组合的内部结构,是一条经常发生大地震、具多种弱化机制的断裂带;发现了汶川地震不仅具有同震石墨化作用,而且测量到目前世界上最低的动态摩擦系数(≤0.02),同时首次记录到大地震后断裂快速愈合信息。这些研究结果不仅直接回答了一直困扰在地震地质和地震物理学领域几十年的关键问题,而且对完善地震断裂理论和认识汶川地震机制具有极其重要的意义,为防震减灾提供了理论依据。  相似文献   

基于时空域混合法利用Kaula正则化精确和快速解算GOCE地球重力场   总被引：6，自引：1，他引：5       下载免费PDF全文

郑伟  许厚泽  钟敏  员美娟  周旭华 《地球物理学报》2011,54(1):14-21

为了研究卫星重力梯度技术对中高频地球重力场反演精度的影响,本文基于时空域混合法,利用Kaula正则化反演了250阶GOCE地球重力场.模拟结果表明:第一,时空域混合法是精确和快速求解高阶地球重力场的有效方法;第二,Kaula正则化是降低正规阵病态性的重要方法;第三,基于改进的预处理共轭梯度迭代法可快速求解大型线性方程组...  相似文献   

2008年汶川地震(Ms8.0)非对称同震破碎带的确定:来自WFSD-1随钻流体的证据          下载免费PDF全文

龚正 李海兵劳昌玲  唐力君罗立强李成龙  云锟  张佳佳  王雷振 《中国地质》2015,(2):480-494

地震过程中相当可观的一部分能量消耗于裂隙的活化与形成,来自汶川地震断裂带科学钻探一号孔(WFSD-1)的随钻流体表明,地震新形成的裂隙对应有较强的流体异常,它们为流体的入侵提供了良好的通道。随钻流体呈非对称性分布于主滑移面的两侧,主要的流体异常带集中在主滑移带下方须家河组顶部120 m范围内,该带中气体的含量以及变动的频率明显高于上部相同的宽度范围以及下部沉积岩层,来自地球物理测井的资料同样显示这一带破碎严重并伴随有大量水的侵入,暗示汶川地震形成的裂隙具有非对称性分布的特征。这一特征可能同时受控于断裂上盘彭灌杂岩与下盘须家河组岩层的力学性质差异以及地震破裂过程中形成的非对称性应力分布。  相似文献   

青海共和盆地中三叠世花岗岩组合岩石成因:地球化学、锆石U-Pb年代学及Hf同位素约束   总被引：1，自引：1，他引：0  

陈希节  贠晓瑞  雷敏  蔡志慧  张盛生  刘若涵  李毅兵  何碧竹 《岩石学报》2020,36(10):3152-3170

青海共和盆地位于青藏高原东北缘，以往有关共和盆地及邻区早-中三叠世岩浆岩成因机制的认识分歧较大，且研究主要集中在露头岩石方面。本文以共和盆地干热岩GR1井深部花岗岩岩芯样品作为研究对象，对其进行岩石学、长石电子探针、主微量元素地球化学、锆石U-Pb年代学及Lu-Hf同位素研究。矿物组成及长石电子探针测试结果显示花岗岩主要为奥长花岗岩、英云闪长岩及花岗闪长岩。锆石U-Pb测年结果表明，奥长花岗岩的结晶年龄为236.5±1.7Ma，英云闪长岩的岩浆结晶年龄为241.6±3.0Ma。主、微量元素地球化学显示这些花岗岩主要为准铝质，属于高钾钙碱性系列。全岩Ta-Nb-Hf等不相容元素图解及锆石Hf同位素数据表明共和盆地的236.5~241.6Ma花岗岩显示火山弧及同碰撞花岗岩成分特征，说明中三叠世共和地区发生俯冲-碰撞转换。结合本文数据与区域背景资料，作者认为：共和盆地早-中三叠世花岗岩组合的形成与印支期宗务隆洋的南向俯冲作用密切相关，此时，在宗务隆-青海南山-西秦岭北缘存在统一的大陆边缘弧环境；在236~241Ma时发生俯冲-碰撞转换；晚三叠世时宗务隆-青海南山-西秦岭北缘已处于碰撞期和后碰撞期。  相似文献   

Formation of the Neoproterozoic Rifting Depression Groups of the Tarim Basin and its Hydrocarbon Potential: Responded to the Initial Opening of the Proto-Tethy Ocean     

HE Bizhu  JIAO Cunli  LIU Ruohan  HUANG Taizhu  CAI Zhihui  CAO Zicheng  YUN Xiaorui  Lan Mingjie  JIANG Zhongzheng  ZHU Ding  YANG Yujie  CUI Junwen  HAO Guangming 《《地质学报》英文版》2020,94(Z1):16-16

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3D gravity modelling for Anyongbok Seamount in the East Sea     

Moo Hee Kang  Hyun-Chul Han  Hyesu Yun  Gee Soo Kong  Kyong O. Kim  Youn Soo Lee 《Marine Geophysical Researches》2007,28(3):257-269

A seamount chain with an approximately WNW trend is observed in the northeastern Ulleung Basin. It has been argued that these seamounts, including two islands called Ulleung and Dok islands, were formed by a hotspot process or by ridge related volcanism. Many geological and geophysical studies have been done for all the seamounts and islands in the chain except Anyongbok Seamount, which is close to the proposed spreading ridge. We first report morphological characteristics, sediment distribution patterns, and the crustal thickness of Anyongbok Seamount using multibeam bathymetry data, seismic reflection profiles, and 3D gravity modeling. The morphology of Anyongbok Seamount shows a cone shaped feature and is characterized by the development of many flank cones and flank rift zones. The estimated surface volume is about 60 km³, and implies that the seamount is smaller than the other seamounts in the chain. No sediments have been observed on the seamount except the lower slope, which is covered by more than 1,000 m of strata. The crustal structure obtained from a 3D gravity modeling (GFR = 3.11, SD 3.82 = mGal) suggests that the seamount was formed around the boundary of the Ulleung Plateau and the Ulleung Basin, and the estimated crustal thickness is about 20 km, which is a little thicker than other nearby seamounts distributed along the northeastern boundary of the Ulleung Basin. This significant crustal thickness also implies that Anyongbok Seamount might not be related to ridge volcanism.  相似文献