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991.
基于FFT分形滤波的地球化学异常信息提取   总被引:1,自引:0,他引:1  
本文尝试采用多重分形方法分析地球化学数据作快速傅里叶变换后的功率谱数据,确定区域背景和局域背景的截止频率,并使用此频率对原始数据分别做低通滤波处理以提取异常信息.传统统计方法确定的异常范围最大,且在测区东部出现了一条南北走向的异常区,主要原因是前期对原始数据进行了迭代剔除,异常下限的确定并非由全部数据而是由背景数据确定;区域背景提取由于背景值是动态的,可以还原测区地球化学场的空间结构,提取的异常范围更小,浓集趋势更明显;局域背景提取的异常由于受高背景值控制,出现在测区东部的异常消失,异常范围和强度也均不及区域背景提取的异常大.  相似文献   
992.
辽西建昌盆地九佛堂组珍稀化石层的划分与对比   总被引:1,自引:0,他引:1  
为研究热河生物群的鸟类、爬行类和被子植物的早期演化、辐射迁移、生物多样性及其协同进化,笔者在建昌盆地测制了九佛堂组剖面,并系统采集了以珍稀化石为重点的生物化石。结合前人研究成果,将九佛堂组自下而上分为第一段至第三段,其中九佛堂组第一段西店层含鸟类、爬行类和龟类等珍稀化石,尚见介形类化石Cypridea decorosa,C.jianchanensis,Yumenia jianchanensis,Limnocypridea slundensis,L.levigata,L.rara等,表明该层的介形类化石与喀左九佛堂小孤山—烧锅地剖面及朝阳县波罗赤小北山—黄道营子剖面的九佛堂组第一段下部介形类化石组合面貌基本一致,其所在层位亦应相当。  相似文献   
993.
NS-trending dikes which contain dioritic enclaves widely occur in the Miaoergou pluton, West Junggar, Xinjiang. The dikes are composed of quartz diorite and quartz diorite porphyrite. LA-ICP-MS zircon U-Pb ages of the quartz diorite and diorite are 298.0±3.7 Ma and 299.4±2.5 Ma, respectively, corresponding to the end of the Late Carboniferous to beginning of the Early Permian. The dikes and enclaves have similar geochemical properties with island arc features. They are calc-alkaline, with moderate SiO2 (53.58% to 57.89%), high MgO (3.09% to 4.83%, Mg# values ranging from 44.69 to 54.12), TiO2 (1.17% to 1.66%), Cr (51.24×10-6 to 126.1×10-6), Ni (35.91×10-6 to 57.55×10-6) contents and K/Na ratios (0.35 to 0.70). Moreover, all samples are enriched in large-ion lithophile elements (LILEs: e.g. K, Rb, Ba and U) and light rare earth elements, but strongly depleted in high field strength elements (HFSEs: e.g. Nb, Ta and Ti), with insignificant Eu anomalies (δEu=0.67 to 1.08). In contrast, the dikes and enclaves in the Miaoergou pluton show geochemical signatures similar to those of the Cenozoic sanukitoids in Setouchi volcanic belt of SW Japan and the sanukitoids in the Hatu area, West Junggar. The source of the dikes might be the depleted mantle previously metasomatized by fluids released from subduction slabs. These sanukitic dikes may be generated by interaction of the mantle wedge with fluids derived from dehydration of the subducting oceanic slab, resulting in 2% to 5% partial melting of amphibole-spine peridotite. The identification of the sanukitic dikes in the Miaoergou pluton, together with previous studies, suggest that the southern West Junggar region was still dominated by subduction-related island arc setting at the beginning of the Early Permian, and multi-stage subduction-accretionary orogeny may account for the difference of subduction duration between the north and the south of West Junggar. © 2018, Science Press. All right reserved.  相似文献   
994.
The experimental study of fatigue damage to coal under cyclic loading is important for guiding the design of pillars in underground coal mines where the pillars may be affected by repeated mining activity. In this paper, the strength, deformation, energy dissipation, and fatigue of samples of coal from a mine in China are studied using cyclic loading with a servo-controlled rock mechanical test system. The results indicate that coal is more likely to suffer fatigue damage than other, harder, rock lithologies. Under uniaxial cyclic loading, the fatigue failure “threshold value” for the coal samples studied is less than 78% of its uniaxial strength, but there is also a certain amount of fatigue damage when the cyclic loading/unloading experiments are carried out below the threshold value for fatigue failure. Axial deformation during the tests can be divided into three stages: initial deformation, constant steady deformation, and accelerated deformation. Transversal deformation can be divided into two stages: stable deformation and accelerated deformation. During cyclic loading experiments, imminent sample failure is signaled when transversal deformation increases significantly and quickly and the deformation recovers little when the load is removed. With an increasing number of loading/unloading cycles, a graph of energy dissipation per unit volume versus number of cycles presents an L-shaped curve when the coal samples do not suffer fatigue failure. However, for the coal samples that do rupture due to fatigue, the curve is U-shaped. Under cyclic loading, the evolution of compaction, strain hardening, strain softening, and failure of coal can be revealed in great detail by fatigue damage experiments.  相似文献   
995.
Li  Yi  Fang  Weihua  Duan  Xiaogang 《Natural Hazards》2019,98(2):507-533

Tropical cyclone (TC) disasters have frequently caused casualties in the coastal areas of China. According to the statistics of dead and missing people due to TCs from 1951 to 2014, the number of fatalities has been significantly decreasing over time. However, deadly TC events have still caused great losses of life in recent years, which are characterized as significant abrupt fluctuations superimposed along the downward trend of the long-term fatality time series. The numbers of fatalities caused by TC disasters are influenced by variables such as the intensity of TC hazards, the population exposed to TCs and the vulnerability of people to TC hazards. It is thus of great significance to analyze their temporal characteristics and understand the forces driving these changes. First, the time series of the TC wind, precipitation, spatial distribution of population, fatality and disaster risk reduction (DRR) measures of China from 1951 to 2014 are reconstructed. Second, the improved power dissipation index, total precipitation, integrated intensity and index of exposed population are calculated, and the population vulnerability indices, including mean and relative fatality rates, are derived. Third, the change trend of each index is detected using the Mann–Kendall test. Finally, the main driving factors of the long-term change trend and fluctuations of the TC fatalities are analyzed by a negative binomial regression model and standard deviation statistics. It is found that the decrease in vulnerability based on the improvement in structural and non-structural measures is the main driving force of the decreases in fatalities over the past six decades. Although the total population and exposure have increased dramatically in the coastal areas of China, their contributions to the increase in the fatality risk were counteracted by the decrease in vulnerability. Abrupt and catastrophic disasters were mostly caused by TCs with hazards of high intensity that surpassed the capacity of structural measures; the lack of forecasting or early warning, as well as improper emergency response actions, may also have triggered the great loss of lives. To reduce the fatalities of future TCs, especially those that may exceed the capacity of structural measures, the enhancement of non-structural measures and the adaptation of resilience strategies should be priorities for future people-centered disaster management.

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996.
为了综合分析增强型地热系统各参数对系统采热性能的影响,以及参数相互之间的影响规律,以云南腾冲热海热田为地质背景,利用正交设计思想通过数值模拟方法对井间距、注入流量、注入温度、储层渗透率等因素的变化进行了分析。结果表明:注入流量是影响系统采热性能的关键因素,并对注入温度、井间距的确定有显著影响;注入流量越大,系统稳定采热时间和运行寿命越短,且注入流量较小的变化(提高0.06 m3/s)会对系统采热温度产生较大的影响(降低47℃);增加注入温度可以提高系统的采热温度和运行寿命,但注入温度升高30℃、运行50 a后采热温度只提高10℃,效果有限;井间距、渗透率、开采压力对系统采热性能的影响相近,且远小于注入流量。  相似文献   
997.
残余热应力是影响聚晶金刚石复合片(PDC)性能好坏的最重要因素之一。考虑聚晶金刚石层(PCD)与硬质合金层厚度比以及PDC压制过程中烧结温度的波动对聚晶金刚石复合片残余热应力的影响,在ANSYS中建立PDC模型,运用热-结耦合法分析PDC的残余热应力。计算表明,随着PCD层与硬质合金层厚度比由0.067增加到0.333,PCD层表面中心的压应力由1.61 GPa降低到380 MPa,PCD层最大径向压应力由1.61 GPa降低1.03 GPa左右,而PCD层边缘靠近界面附近最大轴向拉应力逐渐增大;随着PDC压制过程中烧结温度由1000℃升高到1500℃,PCD层的最大径向压应力、最大轴向拉应力以及最大剪应力等均逐渐增大。认为,在研究PDC合成新工艺过程中,应在保证PDC使用寿命的前提下尽量降低PCD层与硬质合金层厚度比;必须尽量切断原材料以及人为操作对温度的影响。  相似文献   
998.
Gu  Xiaoqiang  Li  Youhong  Hu  Jing  Shi  Zhenhao  Liang  Fayun  Huang  Maosong 《Acta Geotechnica》2022,17(8):3229-3243

Natural clays usually show anisotropic stiffness due to their deposition process and anisotropic in situ stress state. The stiffness anisotropy depends on both of the stress anisotropy and fabric anisotropy, while the latter can be quantified by the stiffness anisotropy at isotropic stress states. This paper measures the K0 value (i.e., stress anisotropy) and elastic shear stiffness anisotropy of natural Shanghai clay in a triaxial apparatus with horizontal and vertical bender elements. The results show that the K0 value of Shanghai clay lies in the range of 0.40–0.66, and an empirical equation is proposed to estimate the K0 value based on the plasticity index and initial void ratio. The fabric anisotropy of natural Shanghai clay lies in the range of 1.2–1.4 with a stronger fabric in the horizontal plane. Moreover, the experimental data of the stiffness anisotropy and fabric anisotropy of different clays in the literature are reviewed and analyzed. It reveals that the stiffness anisotropy generally increases, while the fabric anisotropy remains nearly the same during K0 consolidation. For normally consolidated clay, the fabric anisotropy generally lies in the range of 1.1–1.7. For overconsolidated clays, the fabric anisotropy generally increases as the overconsolidation ratio increases. Empirical equations are proposed to approximately estimate the fabric anisotropy of clays based on its stress normalized elastic shear stiffness.

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999.
香花岭岩浆底辟伸展构造及其控矿的研究   总被引:5,自引:0,他引:5  
香花岭穹隆是一个岩浆底辟伸展构造,它的结构与变质核杂岩、剥离断层的结构相似,由核部、滑动系统及盖层构造三部分组成,核部为隐伏花岗岩体和寒武系变质岩系。滑动系统为隐伏岩体与其上覆盖层之间的高温韧性剪切带和沿泥盆系与寒武系之间的不整合面发育的剥离断层。盖层构造为发育于泥盆系一石炭系中的阶梯状缓倾斜正断层和大量层间滑脱断层,香花岭岩浆底辟伸展构造是在区域伸展作用的背景下,由岩浆底辟上隆,并引起上覆盖层下滑而形成的。香花岭锡、铬、锌多金属矿的矿田、矿床及矿体构造都受该伸展构造控制。  相似文献   
1000.
华北地区是我国最大的矽卡岩型富铁矿床集中区,但目前对区域铁矿床的成矿年代学研究尚不系统和全面,从而制约了对其成矿构造背景的理解。山东莱芜张家洼矽卡岩型铁矿床是华北克拉通东部最重要平炉富铁矿产地之一,铁矿体主要赋存于早白垩世矿山岩体与中奥陶统碳酸盐岩的接触带、石炭系本溪组与奥陶系间不整合面的层间构造破碎带。金云母是张家洼铁矿床最主要的含水矽卡岩矿物,且与磁铁矿密切共生,对其进行40Ar/39Ar定年可为张家洼铁矿床的成矿时代提供约束。本文对张家洼铁矿床I号矿区和港里矿区的两件金云母单矿物样品进行了激光阶段加热40Ar/39Ar同位素分析,获得很好的坪年龄,分别为129. 7±0. 8 Ma和131. 5±1. 2 Ma (2σ)。上述年龄数据与矿山岩体的锆石和矽卡岩中热液榍石的U- Pb年龄一致,证实张家洼铁矿床的成矿时代为130 Ma左右。对张家洼及华北克拉通其他矽卡岩型铁矿床现有同位素年龄数据的综合分析表明,整个华北克拉通内的矽卡岩型铁矿成矿作用具有同时性和爆发性,绝多大数矿床均形成于130 Ma左右,指示华北地区大规模矽卡岩型铁成矿作用是对华北克拉通岩石圈减薄和破坏的响应。  相似文献   
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