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利用双差定位方法，对2013年10月—2016年12月乳山震群进行重定位，并计算乳山震群中地震集中活动区域b值，分析其深度分布变化。结果显示：地震重定位后表现为近NW向集中分布；b值在震源深度7.4 km上下最小，反映该深度处应力最强；乳山震群b值并不随震源深度增大而呈系统性减小变化，且深度10.2 km以下无有效b值，进一步证实该震群近NW向发震断裂的存在。根据b值随深度的变化特征，推测断裂活动的高应力区域集中在6.5—10.2 km深度范围内，断裂活动在深度7.4 km处应力最强，且水平分布最广；相比上下两侧地壳介质b值在5.5—6.2 km深度层位明显增大，反映该深度层位介质性质存在明显差异。 相似文献
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本文利用误差分布和概率统计分析改进了波速比计算方法.对于震源位置相对集中的震群活动,对台站震相到时进行两次差分,通过对差分后的震相数据对进行二维高斯分布拟合,可以稳健地估计震群活动震源区波速比.该方法充分利用了不同台站Pg、Sg到时差的所有信息,其优势是不需要地震事件的震源位置,并且不依赖震源区以外的速度变化,有效消除了震源区到台站的传播路径效应的影响;相对于传统的平均波速比,本文方法得到的震源区波速比,更能真实地反映震源区介质的性质.我们将该方法应用到2013—2016年的乳山震群,结果显示:震源区波速比的变化与震群活动过程密切相关,波速比的变化反映了序列活动的阶段性特征. 相似文献
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利用区域波形数据使用CAP方法反演中强地震的震源机制正逐渐得到广泛应用.本文以胶东半岛近期发生的两次显著中等地震为例,讨论了使用CAP方法反演震源机制时的误差估计,展示了反演结果的不确定性分析过程.2013年11月23日和2014年1月7日在山东莱州和乳山分别发生了M4.6和M4.3级中等地震,两次事件均造成了较大影响.我们基于CAP方法,使用自助抽样(bootstrap)技术多次重复反演过程,得到大样本量的震源机制解数据;基于这些数据,使用粒子群算法和聚类分析技术给出了优化解,估计了震源机制解的误差范围,并利用震源机制解的P、T轴给出了震源球上的概率密度分布. 相似文献
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A notable swarm occurred in Rushan, Shandong Peninsula and its activities continue since Oct. 2013 till now. Up to Sept. 30, 2014, more than 7 000 events have been recorded, in which locatable shocks exceed 2000, and 18 events with ML≥3.0. The swarm is rarely seen in East China for its extraordinary duration time and surprising high frequency of aftershocks. 18 temporary seismometers have been deployed around the swarm since May 6, 2014, and composed a seismic array for monitoring the swarm activities. Based on data from permanent networks and temporary array, we relocated the earthquake sequence by using hypoDD method. It has been shown that, there is obvious difference between permanent network results and temporary array results. The permanent network of Shandong has a relative large coverage gap(more than 200°)for this swarm. Its location results therefore should not be reliable. There are maybe other errors in the permanent network result due to some problems in the raw data, such as too few stations for most locatable events(3 stations), and relative lower proportion of located events in final result(74.3%, while 95.1% in temporary array result). It can be found by comparing location results from permanent network and temporary array that, using temporary array's data can improve the location accuracy significantly. The results of temporary array are: aftershocks distribution of Rushan swarm is in NWW direction, the dip-direction of fitted fault plane is SW, and the strike and dip angle agree with focal mechanism of the mainshock. Focal depths of aftershocks are at 4.5～8km; the swarm is restricted in a small area about 3km×3km×1km, and has some characteristics such as clustering, staged activities, and etc; the aftershock activities are in accord with crack growth behavior pattern, hence we deduced that there may be fluid intrusion in source area. Finally, we discussed the seismogenic structures and active mechanisms of this swarm combined with relative geologic knowledge. We draw some conclusions as follows: 1)Rushan swarm probably occurred at the boundary of rock bodies of Duogu Mountain and Haiyangsuo super-unit; 2)The seismogenic structure is a blind fault, which should be a part of adjacent Heishankuang-Jilincun Fault, or might be a new fault at rock body boundaries; 3)Rushan swarm might be an evidence for the existence of the disputed Shidao Fault. 相似文献
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基于高分辨率MASNUM第三代海浪模式并根据Yuan等(2009)提出的波浪破碎统计物理模型,对乳山湾外海2008年各个季节波浪特征要素(有效波高和跨零周期等)与波浪破碎参数(白冠覆盖率、卷入深度和破碎能量损耗率)进行了数值模拟。利用Janson-1卫星高度计观测资料对有效波高模拟结果进行了检验,平均误差在0.17m左右。模拟结果显示,该海域波浪参数具有明显的季节变化特征,在2008-08乳山湾邻近海域受大风天气过程影响期间,有效波高在1.0~1.8m,破碎参数变化显著,白冠覆盖率最大达4.5%,卷入深度在1.5m以上,相应的破碎能量损耗率量值在6~11kg/s3。结果表明,波浪破碎过程对该区域海洋动力环境有着重要影响,是造成乳山湾口表层高溶解氧的可能机制之一。 相似文献
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胶东乳山金矿区原生晕地球化学特征及深部成矿预测 总被引：1，自引：0，他引：1
英格庄金矿以相对富As、Co、Ni而三甲和铜锡山金矿则以相对富Cu、Pb、Zn、Ag为特征.聚类分析显示,英格庄金矿具Bi+Hg、As+Sb+Co与Pb+Zn组合,三甲金矿具Bi+Hg+As+Sb+Co、Pb+Zn与Ag+Cu+Au组合,而铜锡山金矿则显示Bi+Hg+Sb+Pb+Ag、Cu+Au+Zn+As及Mo+Ni组合.结合Ni、Co、Mo与Ag、Hg、As、Sb等的相关特征,认为上述三个金矿均有成矿头尾晕叠加现象.Au、Ag、Cu、Pb、Zn、As、Sb、Bi、Hg、Mo等元素垂向变化规律显示,英格庄金矿在-200m标高以下、三甲金矿在-500m标高以下尚有成矿富集段存在.其中,所确定的英格庄金矿的靶位在16勘探线附近,三甲金矿的靶位则在16～20勘探线间. 相似文献
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基于2012-2016年乳山市建设用地利用与经济社会发展的时间序列数据,构建乳山市建设用地利用与经济社会发展耦合协调度模型,研究乳山市在2012-2016年期间建设用地和经济社会之间的关系。首先选取评价指标建立指标体系,采用熵值法确定指标体系权重,然后对两者的耦合协调度进行定量分析。结果表明:2012年建设用地利用水平、经济社会发展水平综合评价值分别为0.4394,0.1907;而2016年综合评价值增加到0.6716,0.9315,乳山市建设用地利用水平与经济社会发展水平都有大幅度增长。两者的耦合协调度由2012年0.3805增加到2016年0.6289,耦合关系逐年优化。最后针对建设用地规模过大,土地集约利用程度较低等问题,提出继续提高土地集约利用水平、优化产业结构等建议。 相似文献
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胶东乳山金矿蚀变岩中绢云母40Ar/39Ar年龄及其对金成矿事件的制约 总被引：7，自引：1，他引：7
胶东乳山金矿是我国单脉金储量最大的矿床,金的成矿具有多期多阶段的特点。为了研究早期矿化的时代,利用绢云母40Ar/39Ar法测定了乳山金矿含矿脉体旁围岩蚀变带中的绢英岩年龄。结果表明,围岩花岗岩的强烈绢英岩化蚀变年龄为129 Ma,比金发生大规模沉淀的成矿时间早约10 Ma,表明乳山金矿是多期热液成矿事件的产物,但这一事件也发生于120±10 Ma,从而证明乳山金矿与胶东其他地区金矿一样都是在中生代构造机制转折、岩石圈强烈减薄的构造背景下集中成矿的,这为进一步认识乳山金矿的成因机制和成矿动力学背景提供了新的证据。 相似文献
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Fluid evolution in the Rushan lode gold deposit of Jiaodong Peninsula, eastern China 总被引：2，自引：0，他引：2
Fang-Fang Hu Hong-Rui Fan Ming-Guo Zhai Cheng-Wei Jin 《Journal of Geochemical Exploration》2006,89(1-3):161
The Rushan gold deposit in the Jiaodong Peninsula is currently the largest lode gold in China. Gold occurs mainly in pyrite- and polymetallic sulfide–quartz vein/veinlet stockworks. Fluid inclusions in the deposit are divided into three main types, namely CO2–H2O, H2O–CO2 ± CH4 and aqueous ones. Microthermometric data show that the pre-gold fluids were CO2-dominant (XCO2 up to 0.53), and the total homogenization temperatures fall in the range of 298377 °C. These fluids, modified by fluid/wallrock reactions, gradually evolved into fluids with less CO2 (XCO2 = 0.010.19) in the main ore-forming stage, and the total homogenization temperatures range from 170 to 324 °C. Hydrogen and oxygen stable isotope data suggest that ore-forming fluids were mixture of magmatic and meteoritic origin. Co-occurrence of gold and sulfides implies that gold was most likely transported in the form of gold–sulfide complexes. The wide distribution of CO2 inclusions means that the pH variation during gold transportation was controlled by CO2 buffering. 相似文献