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51.
20起地震监测设施和观测环境保护行政执法案例特征分析 总被引:2,自引:0,他引:2
运用法学原理,结合地震监测设施和观测环境保护法律、法规,对《地震行政执法案例选编》中提供的20起地震监测设施和观测环境保护行政执法案例进行了综合统计分析,探讨了实际工作中涉及到的若干法律问题。 相似文献
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<正>Objective The nearly parallel N–S-trending rifts in southern Tibet represent the E–W extension of the Tibet Plateau.Most data which constrained the age of the extensional deformation come from isotopic dating of the dikes probably related to the activity of the nearly N–S faulting and micas from hydrothermal activity and the lowtemperature thermochronology of plateau uplift.Previous 相似文献
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随着经济社会的发展,海洋环境监测受到越来越多的关注。针对当前海洋环境监测中,采用海洋水质集成在线监测系统,开展现场自动化监测的实际需求,以国家海洋技术中心自主研发的四参数水质仪、浊度传感器和营养盐自动分析仪为基础,开发岸基海洋水质集成在线监测系统。按照海洋水质集成在线监测系统的总体工作顺序,将工作流程划分为多个状态进行管理。应用LabVIEW编程语言,采用队列状态机,对各状态进行合理安排,最终实现了岸基海洋水质集成在线监测系统工作流程的有序调度以及可靠控制。 相似文献
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介绍了一种具有多个测量装置的水质监测仪器集成控制系统的开发设计方案。该设计方案针对5套功能相似但相互独立的水质测量装置,以嵌入式系统为控制核心,灵活运用Modbus RTU通信协议及RS485总线,并自主开发通信协议,实现控制核心与触摸屏、PC机以及5套测量装置的通信连接;进而采用多任务的处理架构,对上述外围设备操作任务进行分时处理,最终成功将5套测量装置集成为一台水质监测仪器,并支持PC机和触摸屏双终端进行显示和控制。实际应用效果表明,该设计方案稳定、可靠。 相似文献
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胶东金矿集中区构造体系多层次控矿规律研究 总被引:10,自引:3,他引:7
提出中新生代东亚大陆与西太平洋带活动带相互关联的构造剪切带即是NNE向新华夏系巨型构造带。胶东金矿集中区产生于洋-陆过渡关联的该NNE向构造剪切带。对胶东构造体系进行了进一步研究,指出胶东中生代主要发育新华夏体系和华夏式构造系,而纬向构造体系,即EW向构造不发育。在此基础上,对胶东金矿集中区构造控制矿带、矿床、矿脉、地球化学分布和物理化学条件等不同层次特征加以分析,提出了胶东金矿成矿期构造具有多层次控矿特点,新华夏系NEE向泰山式构造控制胶东区域金矿带的展布;新华夏系NNE向区域剪切带控制金矿田产生部位;构造带断裂性质控制金矿矿床类别;构造断裂带的产状控制矿床矿体的倾伏侧伏规律;剪切构造两盘的运移特点和断裂组合形式控制矿脉的分布规律;构造变形岩相带控制构造地球化学特征;构造控制水岩系统成矿物理化学条件等认识。成矿构造研究、测量和资料分析证实,成矿阶段构造应力场最大主应力和最小主应力轴面是近于水平的,而中间主应力接近于垂直;区域成矿期应力场呈水平反钟向扭动剪切状,具有新华夏系应力场特征。从中生代应力场分析发现,除了区域反钟向挤压剪切构造特征外,主要成矿阶段构造环境还表现出应力松弛和拉张的特点,有普遍的断裂上盘下滑的构造成矿的特征。 相似文献
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HA Guang-hao WU Zhong-hai MA Feng-shan ZENG Qing-li ZHANG Lu-qing GAI Hai-long 《地震地质》2019,41(2):436-446
In the interior of the Tibetan Plateau, the active tectonics are primarily marked by conjugate strike slip faults and north-trending rifts, which represent the E-W extension since late Cenozoic of the plateau. The conjugate faults are mainly composed of NE-trending left-lateral strike-slip faults in Qiangtang terrane and NW-trending right-lateral strike-slip faults in Lhasa terrane. While, the rifts mainly strike N, NNW and NNE within southern Tibet. However, it is still a debate on the deformational style and specific adjustment mechanism of E-W extension. One of key reasons causing this debate is the lack of detailed investigation of these active faults, especially within the northwestern plateau. Recently, we found a 20km long, NNW-trending active fault at Bero Zeco in northwestern Tibet. This fault is presented as fault sag ponds, channel offsets and fault scarps. Displacement of channels and geomorphic features suggested that the Bero Zeco Fault(BZF)is a dextral strike-slip fault with a small amount of normal slip component, which may result from the E-W extensional deformation in the interior of Tibet. BZF strikes N330°~340°W, as shown on the satellite image. The main Quaternary strata in the studied area are two stages alluvial fans around the Bero Zeco. From the satellite images, the old alluvial fans were cut by the lake shoreline leaving many of lake terraces. And the young fans cut across the lake terraces and the old fans. By contrasting to the "Paleo-Qiangtang Huge Lake" since late Quaternary, these old alluvial fans could be late Pleistocene with age ranging from 40ka to 50ka. And the young fans could be Holocene. The sag ponds along the BZF are distributed in the late Pleistocene alluvial fans. Also, the BZF displaced the late Pleistocene fans without traces within Holocene fans, suggesting that the BZF is a late Pleistocene active fault. The fault scarps are gentler with the slope angle of around 10° and the vertical offset is about 2m by field measurement. Reconstruction of the offset of channels suggested that the accumulated dextral offset could be about 44m on the late Pleistocene alluvial fans. Therefore, we infer that the dextral slip-rate could be around 1mm/a showing a low-rate deformation characteristic. The angle between the strike of BZF and principal compressive stress axis(σ1)is around 30°, which is significantly different to the other faults within the conjugate strike-slip fault zones that is 60°~75°. Now, the deformation mechanisms on these conjugate faults are mainly proposed in the studies of obtuse angle between the faults and σ1, which is likely not applicable for the BZF. We infer that the BZF could be the northward prolongation of the north-trending rifts based on the geometry. This difference suggests that the conjugate strike-slip faults may be formed by two different groups:one is obtuse angle, which is related to block extrusion or shear zones in Lhasa and Qiangtang terranes possibly; the other is acute angle, which may represent the characteristics of new-born fractures. And more studies are needed on their deformation mechanisms. 相似文献
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风蚀地貌形态与过程研究进展 总被引:4,自引:0,他引:4
辨析了雅丹、风蚀坑等主要风蚀地貌的概念,雅丹是典型的风蚀正地貌形态,通过回顾雅丹地貌形态与过程的研究历史与进展,发现目前对其发育过程的认识尚不清楚,并且只关注了对残存土墩的观测和分析,没有充分重视凹槽的形态动力学过程;风蚀坑是典型的风蚀负地貌形态,特别是草原景观转变为沙地景观的临界阈现象,目前已经对独立风蚀坑的形态、气流特征、沉积物粒度以及植被演替过程等方面进行了初步研究,但由于风蚀坑形态是多因素共同作用的结果,需要由单因素观测转向综合分析其形态动力学过程.认为对风蚀过程机理及其模拟的研究中,在利用风洞模拟实验、野外观测等手段对风蚀过程微观尺度进行研究的同时,也需要加强通过遥感和GIS手段从景观尺度对风蚀地貌发展变化过程进行分析. 相似文献