谈谈地质资料档案的标准化著录

在简要论述地质资源档案标准化著录含义的基础上，详细阐述了地质资料档案的著录项目，著录根据，著录用标识符及使用说法，著录条目格式，著录标目法，以及题名目录，责任者目录，主题目录，分类目标的编制。意在引导地质资料档案管理部门，进一步做好地质资料档案著录这一基础性工作。     

南极地区数百年来气候变化的冰芯记录对比研究

随着国际横穿南极科学考察计划的实施, 近年来开展了沿中山站-Dome A考察路线的冰芯研究, 获得了伊丽莎白公主地250 a来气候环境变化的高分辨率记录. 通过与Lambert冰川流域西侧有关研究结果的对比, 揭示了该冰川谷地为东南极洲重要气候分界线的特征. 综合南极地区其它地点冰芯记录和冰盖变化研究结果, 发现以小冰期为代表的寒冷期在东南极洲较为明显, 在西南极洲则不明显, 甚或恰好相反, 表现为温暖阶段. 就东南极洲来说, 也存在明显的区域差异: 以Lambert冰川谷地为界, 东部地区, 如Wilkes Land (Law Dome), Victoria Land北部(Hercules Neve)等地, 小冰期冷期比较突出;西部地区, 如Dronning Maud Land和Mizuho高原, 情况不是很明确. Lambert冰川流域是非常特殊的地方, 虽然小冰期冷期也存在, 但1850年前后的显著高温和近100多年来的降温与南极洲其它地方都不一样, 而与南极半岛北侧一冰芯所给出的400 a温度变化记录极为相似, 我们尚不能解释为何如此遥远的两个地点具有很好的一致性而与其它地方则不一致.     

青藏高原腹地湖泊沉积纪录的“仙女木期”古气候颤动事件

通过对青藏高原腹地钻孔岩心剖面的最新研究,用层序地层学与年代地层学和气候地层学相结合的方法,分辨出可可西里地区苟弄措湖泊沉积记录(孔深7.25 m)约30 ka BP以来的古气候变化,并在孔深3.32～1.98 m处识别出“仙女本期”的3个气候颤动事件,即:①老仙女术事件(孔深3.32～2.62 m);②中仙女本事件(孔深2.62～2.43 m);③新仙女本事件(孔深2.43～1.98 m)。这3个气候颤动事件都是以冷干时段开始、以冷湿时段结束的,并有越向后期其冷干的时段越长的变化趋势,而其后的冷湿时段却具有等时的变化趋势。岩心沉积物的有机碳、有机氮和磁化率以及化学元素含量的变化,都与仙女本期气候变化具有十分吻合的变化态势。仙女术期气候在湖泊沉积物中的响应,在青藏高原环境演化中还是首次发现,为研究第四纪末次冰期冰消期以来的气候变化提供了新的信息。     

长春腰分水岭黄土剖面常量化学元素特征及其气候意义

长春腰分水岭中更新世晚期黄土剖面的野外观察和常量化学元素分析结果表明：各层中常量化学元素的规律性变化不仅能够揭示出剖面沉积时气候干冷－湿暖的多次波动，而且与野外各层的宏观特征具有良好的对应性；该项研究对于恢复中更新世晚期古气候及其变化具有重要意义，也为松辽平原东部第四纪地层的划分与对比提供了重要证据。     

A replicated 3000 yr proxy-climate record from Coom Rigg Moss and Felecia Moss,the Border Mires,northern England

Quantitative plant macrofossil and colorimetric humification analyses have been used to reconstruct proxy-climate from two paired ombrotrophic bogs in northern England (Coom Rigg Moss and Felecia Moss). Detrended correspondence analysis was used to transform the raw floral data into indices of mire surface wetness. The chronology of each peat profile was determined by radiocarbon assay, supported by pollen correlations. Palaeoclimatic reconstructions have been made by linking documented historical changes in climate, and other proxy-climate records, to those inferred from the sites investigated in the study region. Both sites contain a sensitive palaeoclimatic record, as ten periods of increased effective precipitation have been detected between ca. cal. ad 1770–1800, ad 1400–1470, ad 1110–1260, ad 920–1060, ad 550–670, ad 210–360, 30 bc to ad 80, 180–130 bc, 590–520 bc and 760–710 bc. Copyright © 1999 John Wiley & Sons, Ltd.     

NCDSN台站地震监测系统实时监视软件

阐述NCDSN台站连续波形数据断记问题的一种解决办法,软件安装及其使用方法,方法简便易行,便于推广。     

An uncertainty parameter of historical earthquakes – the record threshold

In this study we use the term record threshold of a historical earthquake for the seismic intensity (EMS92) in an area where a given percentage P of the serial sources of places have recorded the event as been noticed there. The record threshold is understood as a limiting measure, below which warranted statements about the intensity cannot be given. P defines the acceptable uncertainty and can be chosen according to the demands of the special task, for instance, 10%. It is shown that the record threshold of historical earthquakes is not the same as the human perceptibility threshold of earthquakes of the 20th Century. The historical sources have to be selected using criteria such as completeness and homogenity of data. This demand is approximately met by inquiries for sources covering an area greater than the expected felt area of the historical earthquake.The Friuli event of 25 January 1348 is presented as an example. It is compared with the well known Friuli event of 6 May 1976 in order to calibrate its intensity. The record threshold of the 1348 event was probably IV or less than IV EMS92 for P = 10%. The method, properly modified, can be applied to different cultural epochs and areas. This result throws a light on the possible error in determining the felt area of historical events.     

2020年1月19日新疆伽师MS6.4地震强震动记录特征初步分析

2020年1月19日新疆伽师发生M S6.4地震,新疆强震动观测台网共获取44组强震动记录,西克尔强震台获得本次地震最大峰值加速度633.3×10-2 m·s-2。本文对获取到的强震动记录进行初步整理、分析,拟合得到本次地震地震动峰值加速度衰减关系,在300 km范围内与经验性衰减关系相差不大。计算分析了峰值加速度大于100×10-2 m·s-2的5个典型强震台站加速度反应谱,并与设计反应谱进行对比分析,同时计算了这5个台站地震动70%及90%能量持时,两者相差较大,反映出地震主要能量释放集中在相对较短的时间内。     

中更新世以来青藏高原RH孔和洛川黄土记录的比较研究

根据若尔盖盆地ＲＨ孔的研究成果,具体地将该孔的２１个阶段和洛川黄土记录进行对比,分析其异同点,探讨了高原不同降升阶段自身环境特点及其对邻近西北干旱区的影响。     

Pulse-like versus non-pulse-like ground motion records: Spectral shape comparisons and record selection strategies

Pulse-like records are well recognized for their potential to impose higher demands on structures when compared with ordinary records. The increased severity of the structural response usually caused by pulse-like records is commonly attributed to the spectral increment around the pulse period. By comparing the building response to sets of spectrally equivalent pulse-like and ordinary records, we show that there are characteristics of pulse-like records beyond the shape of the acceleration response spectrum that affect the results of nonlinear dynamic analysis. Nevertheless, spectral shape together with the ratio of pulse period to the first-mode structural period, T_p/T₁, are confirmed as “sufficient” predictors for deformation and acceleration response metrics in a building, conditioned on the seismic intensity. Furthermore, the average spectral acceleration over a period range, AvgSA, is shown to incorporate to a good proxy for spectral shape, and together with T_p/T₁, form an efficient and sufficient intensity measure for response prediction to pulse-like ground motions. Following this latter route, we propose a record selection scheme that maintains the consistency of T_p with the hazard of the site but uses AvgSA to account for the response sensitivity to spectral shape.