伽玛能谱参数与金矿找矿

γ能谱测量方法是一种简便、有效、快速的间接找金的方法,不同类型的金矿其伽玛能谱特征并不相同。与深成脉岩活动有关的脉状金矿,具有明显的伽玛能谱Ｋ／Ｕ参数异常;与中浅成中酸性侵入发杂岩体有关的金矿,具有Ｋ／Ｕ,Ｋ／Ｔｈ参数正异常;而与浅成－超玫成偏碱性杂岩体有关的隐爆角砾岩型金矿,则具有一致的Ｕ,Ｔｈ,Ｋ及Ｆ参数正异常。本介绍了在山东东部乳山地区及临沂西部地区,利用没的伽玛能谱参数进行不同类型的金矿     

大桥水库地震遥测台网持续时间震级的研制

由于大桥水库地震台网各子台台基和地下结构的特殊性, 造成震级计算上的较大偏差。为此, 利用该台网各子台同一型号地震仪的垂直向速度量记录, 测量了震级为０５ ～５４ 的４６２ 次地震的振动持续时间, 制作了该台网的持续时间震级公式和便查表。在方法上, 不同于通常的按一次或二次曲线的拟合, 而采取计算机自动分段按折线拟合的方法, 以阻尼最小二乘法完成其计算。先进行分台拟合, 比较异同之后, 合并数据再拟合, 最后给出了适宜于鲁坝、瓦吉木两台和大石头、凉风岗、瓦坡支和彝海子４ 个台使用的两套平均持续时间公式和便查表, 以供大桥水库地震台网测震分析使用。     

磁变仪布局的研究

本文提出了改进磁变仪布局的必要性和布局标准,对磁变仪定向及其稳定性、标度值稳定性和分量仪间允许的最小间距进行了研究,提出了可以提高磁变仪记录质量的改进布局和满足布局全部标准的新布局,改进布局特别是新布局可以显著提高磁变仪保持定向、抗干扰能力,获得记录标度值稳定的较理想的磁照图。     

地震期间的地磁脉动效应

１９９６年１１月１７日至１１月２９日在新疆喀仁地区８次地震期间观测到的震前发生的高频地磁脉动现象,文中对每次地震前的Ｐｃｌ－２脉动的形态,以及脉动的起动时刻,持续时间,Ｈ分量和Ｄ分量的平均振幅随北京地方时的分布进行了详细研究分析,对这种震前观测到的高频地磁脉动的激发机制也做了深入的讨论,事实表明,这种震前发生的高频地磁脉动的地震的短期预报上可能有广泛的应用前景。     

Seismicity acceleration model and its application to several earthquake regions in China

With the theory of subcritical crack growth, we can deduce the fundamental equation of regional seismicity acceleration model. Applying this model to intraplate earthquake regions, we select three earthquake subplates: North China Subplate, Chuan-Dian Block and Xinjiang Subplate, and divide the three subplates into seven researched regions by the difference of seismicity and tectonic conditions. With the modified equation given by Sornette and Sammis (1995), we analysis the seismicity of each region. To those strong earthquakes already occurred in these region, the model can give close fitting of magnitude and occurrence time, and the result in this article indicates that the seismicity acceleration model can also be used for describing the seismicity of intraplate. In the article, we give the magnitude and occurrence time of possible strong earthquakes in Shanxi, Ordos, Bole-Tuokexun, Ayinke-Wuqia earthquake regions. In the same subplate or block, the earthquake periods for each earthquake region are similar in time interval. The constant αin model can be used to describe the intensity of regional seismicity, and for the Chinese Mainland, α is 0.4 generally. To the seismicity in Taiwan and other regions with complex tectonic conditions, the model does not fit well at present.     

CT诊断胸部平片隐匿部位肿瘤的检出价值

本文对２２７例胸部肿瘤中的３４例Ｘ线不易发现的肿瘤进行了Ｘ线与ＣＴ诊断的对照分析,此组病例共占胸部肿瘤的１４．９％,胸部隐匿部位的肿瘤在传统Ｘ光正位胸片上受组织重叠的影响是不易看到的,容易漏诊,须通过ＣＴ扫描检查方可观察到,ＣＴ扫描是诊断胸部隐匿部位肿瘤的最好,最有效的检查方法之一。     

中国及邻区岩石层密度三维结构

利用中国及邻区２×２Ｓ波速地震三维层析成像和３０’×３０’重力资料．首先采用密度差与Ｓ波速差的经验关系式,建立起中国及邻区的岩石层密度初始模型,再利用布格重力异常进行阻尼最小二乘法反演,得到该区岩石层三维密度分布结果．反演结果表明：１．中国地区密度异常分布与大地构造分区有着明显的相关性,高密度区对应古老地块,低密度区对应高原及山区,在不同块体边界存在着密度异常梯级带;２．岩石层地幔密度分布与地壳密度分布特征不一致．     

关于中国煤层瓦斯区域分布的几点认识

据１９９４￣１９９６年连续３年的统计,全国煤矿瓦斯灾害伤亡人数占煤矿伤亡总人数的４０％以上,瓦斯涌出规律、瓦斯涌出量预测、瓦斯突出预测仍是煤矿安全技术的难题,在加强对瓦斯灾害综合治理的同时,把瓦斯作为煤层气资源积极进行开发利用,是当前的研究方向,瓦斯区域分布规律研究可以概括为建立在煤层瓦斯生成条件、保存条件基础上的高斯赋存量,高瓦斯涌出量,低瓦斯赋存量,低瓦斯涌出量区域分布规律研究;建立在高瓦斯赋     

研究季风区历史时期湖泊环境演化的意义

本文首先讨论了历史时期季风区湖泊环境演化研究在古全球变化研究中的地位及其意义,着重强调人与自然相互作用研究以及进行定量研究是该领域的关键所在。综合中国近年来在湖泊沉积与古全球变化研究中取得的成果,提出在该领域研究的一些新的认识与亟待解决的问题。     

A 15-year-Long catalog of seismicity in the Eastern Tennessee Seismic Zone (ETSZ) using matched filter detection

We present a detailed catalog of 13 671 earthquakes in the Eastern Tennessee Seismic Zone (ETSZ) that spans January 1, 2005 to July 31, 2020. We apply a matched filter detection technique on over 15 years of continuous data, resulting in arguably the most complete catalog of seismicity in the ETSZ yet. The magnitudes of newly detected events are determined by computing the amplitude ratio between the detections and templates using a principal component fit. We also compute the b-value for the new catalog and comparatively relocate a subset of newly detected events using XCORLOC and hypoDD, which shows a more defined structure at depth. We find the greatest concentration along and to the east of the New York-Alabama Lineament, as defined by the magnetic anomaly, supporting the argument that this feature likely is related to the generation of seismicity in the ETSZ. We examine seismicity in the vicinity of the Watts Bar Reservoir, which is located about 5 ?km from the epicenter of the M_W 4.4 December 12, 2018 Decatur, Tennessee earthquake, and find possible evidence for reservoir modulated seismicity in this region. We also examine seismicity in the entire ETSZ to search for a correlation between shallow earthquakes and seasonal hydrologic changes. Our results show limited evidence for hydrologically-driven shallow seismicity due to seasonal groundwater levels in the ETSZ, which contradicts previous studies hypothesizing that most intraplate earthquakes are associated with the dynamics of hydrologic cycles.