Stream-scanning laser system, electric sensing counter and settling grain size analysis: a comparison using reference materials and marine sediments     

Emanuela Molinaroli  Giovanni De Falco  Sandro Rabitti  Rosana Asunta Portaro 《Sedimentary Geology》2000,130(3-4):269-281

Surface and deep-sea core sediments and two sets of standards were measured by three different techniques — Galai Cis-1 laser system, Coulter Counter TA II, and Micromeritics SediGraph 5000D — in order to compare the Galai results with the other two. The differences between the three types of measuring device turned out to be greater in sediments than in standards, and were attributed to the physical properties, shape, density and composition of the particles (complexity of the matrix). Comparison of moment statistics showed that the Galai determines coarser grain sizes than the Coulter and finer than the SediGraph, particularly as regards analysis of surface sediments. The relationships between Galai and SediGraph were estimated using analysis of variation/residuals within individual intervals. The analysis showed a higher variability of residuals for the coarser fractions (8–16 μm and 16–32 μm) with respect to the finer (2–4 μm and 4–8 μm) fractions. The <2 μm SediGraph fraction, with a cut-off at 0.49 μm, showed good correspondence with the <2.5 μm Galai analysis.  相似文献   

松辽盆地徐家围子断陷营城组火山岩相和火山机构分析   总被引：47，自引：0，他引：47  

陈建文  李长山 《地学前缘》2000,7(4):371-379

徐家围子断陷营城组火山岩极为发育。文章通过对火山岩的岩芯观察、薄片鉴定、岩芯测试及测井资料、二维、三维地震资料的综合分析 ,将营城组火山岩盆地分为 3大相区 ,即火山喷发区、过渡区和沉积区。火山喷发区岩性由各种熔岩、火山碎屑岩和少量砂砾岩组成 ;过渡区岩性以火山碎屑岩与沉积岩互层为特征 ,夹少量火山熔岩 ;沉积区岩性包括砂砾岩、砂岩、粉砂岩和泥岩。火山喷发区内可识别出 8种类型的火山岩相 (空落相、溢流相、基底涌流相、火山碎屑流相、火山泥石流相、火山沉积相、次火山相、隐爆角砾岩相 )和 3种类型的火山机构 (层火山、微型盾火山和渣锥火山 )。不同类型的火山机构具有不同火山作用、岩相分布特征和含油气性。因此火山岩相及火山机构分析对火山作用研究和油气勘探均有重要意义。  相似文献   

Evolution of the Academician Ridge Accommodation Zone in the central part of the Baikal Rift, from high-resolution reflection seismic profiling and geological field investigations   总被引：4，自引：0，他引：4  

V. D. Mats  O. M. Khlystov  M. De Batist  S. Ceramicola  T. K. Lomonosova  A. Klimansky 《International Journal of Earth Sciences》2000,89(2):229-250

 New high-resolution seismic reflection data from the central part of Lake Baikal provide new insight into the structure and stratigraphy of Academician Ridge, a large intra-rift accommodation zone separating the Central and North Baikal basins. Four seismic packages are distinguished above the basement: a thin top-of-basement unit; seismic-stratigraphic unit X; seismic-stratigraphic unit A; and seismic-stratigraphic unit B. Units A and B were cored on selected key locations. The four packages are correlated with a series of deposits exposed on the nearby western shores: the Ularyar Sequence (Oligocene); the Tagay Sequence (Lower to Middle Miocene); the Sasa Sequence (Upper Miocene to Lower Pliocene); the Kharantsy Sequence (Upper Pliocene); and the Nyurga Sequence (Lower Pleistocene). Based on stratal relationships, sedimentary geometries, distribution patterns and principal morphostructural elements – both onshore and offshore – we propose a new palaeogeographic evolution model for the area. In this model progressive tectonic subsidence of the Baikal basins and successive pulses of uplift of various segments of the rift margins lead to: (a) formation of the ridge as a structural and morphological feature separating the Central and North Baikal basins during the Middle to Late Miocene; (b) gradual flooding of the main parts of the ridge and establishment of a lacustrine connection between the two rift basins during the Late Miocene; and (c) total submergence of the top parts of the crest of the ridge during the latest Pleistocene. This new model helps to better constrain numerous phases in the structural evolution of the Baikal Rift, in which the Academician Ridge as an accommodation zone plays a crucial role. Received: 26 November 1999 / Accepted: 12 March 2000  相似文献   

Source ambiguity from an estimation of the scaling exponent of potential field power spectra     

Tatiana Quarta  Maurizio Fedi  & Angelo De Santis 《Geophysical Journal International》2000,140(2):311-323

An analysis of the field scaling power spectrum yields useful information about the source distribution, but it is uncertain whether deterministic, random, fractal or mixed approaches have to be used for the interpretation. To this end, the scaling properties of potential field spectra are analysed for a number of different source models of geological interest. Besides the models of Naidu (purely random sources) and Spector and Grant (gross block statistical ensembles) we consider other types of density and magnetization distributions with spectral exponents in the fractal range, such as a single homogeneous body with a random white source distribution. Spectral slopes in the fractal range are obtained.
We also study the effects of important natural sources, such as salt domes and sedimentary basins, representing them with simple Gaussians or combinations of Gaussian signals. The same spectral slopes as for gravity signals generated by 3-D fractal source distributions are found for them. Hence the power law decay of the field is not a characteristic only of fractal source models.
If a 3-D fractal source distribution is assumed a priori , a way of verifying the goodness of the model is to examine the whitened field at source level. The probability that the whitened field derives from a random white population is estimated for synthetic and real anomalies by applying the usual statistical tests.  相似文献   

How galaxies disguise their ages     

Roberto De Propris 《Monthly notices of the Royal Astronomical Society》2000,316(1):L9-L12

We calculate the contribution to Balmer line indices from far ultraviolet component sources. We find that this is significant, and may lead to identification of spurious age differences of the order of a total span of ∼6 Gyr or ∼15 per cent size bursts observed a few Gyr after star formation stops. We suggest that claims for intermediate-age populations in early-type galaxies may need to be reconsidered in the light of this new evidence.  相似文献   

Reply to “Comments on ‘Calibration of a chalcogenide glass membrane ion-selective electrode for the determination of free Fe in seawater: I. Measurements in UV photooxidised seawater’ by De Marco and Mackey (Marine Chemistry 68 () 283–294)” by Constant M.G. van den Berg     

R. De Marco  D. J. Mackey 《Marine Chemistry》2000,71(3-4)

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几种理化因子对斑节对虾白斑杆状病毒(WSBV)感染力的影响   总被引：8，自引：0，他引：8  

谢数涛  邱德全  何建国  杨晓明  江静波 《海洋科学》2000,24(3):52-54

将部分纯化的ＷＳＢＶ暴露于不同理化条件下,通过人工感染的方法测定ＷＳＢＶ的感染力。结果表明,病毒在纯水中１ｈ能保持感染活性,全在３ｍｏｌ／Ｌ ＮａＣｌ的高盐溶液中１ｈ失去感染力;ＷＳＢＶ在３０℃中４ｈ感染活性丧失,在７０～９０℃中１０ｍｉｎ均失去感染力;当环境ｐＨ值为５以下或１２．６以上时,ＷＳＢＶ在１ｈ后丧失感染活性;ＮＰ０－４０,Ｔｒｉｔｏｎ－Ｘ－１００,ＣｌＯ２或甲醛等均能灭活ＷＳＢＶ。  相似文献   

配电网GIS的一种开发模式探讨   总被引：3，自引：0，他引：3  

刘德刚  陆洪智 《地球科学》2002,27(3):326-328

开发配电GIS主要有3种组织: GIS厂商及GIS二次开发商、配电自动化厂商、电力系统单位.分析了他们在开发中的优势与劣势, 提出一种把配电GIS系统分层, 由GIS厂商开发配电GIS平台, 自动化厂商及电力系统单位在该平台上进行2次开发的模式.论述了配电GIS平台的功能范围及海量数据管理、拓扑关系管理、设备库、按设备分层的拓扑关系模型、组件技术等关键技术, 并介绍了这种模式的一个实例.   相似文献   

长沙市防洪建设中若干重要问题探讨     

毛德华  夏军  龚重惠 《地理研究》2003,22(6):716-724

探讨了全国重点防洪城市长沙市防洪建设中的若干重要问题:防洪标准、设计洪水位、防洪大堤高度等的确定;建设方针与程序、整体防洪能力建设、防洪建设与基础设施建设和景观建设协调发展等。长沙设计洪水位的确定应综合考虑以下几个方面:湘江长沙段洪水与其支流和东洞庭湖洪水不存在高标准洪水同期遭遇问题,更不存在同频率洪水遭遇问题;湘江洪水流量与水位关系不是长沙洪水设计的主要依据;而南洞庭湖洪水位顶托和河道槽蓄量减少是影响长沙洪水位高低的动、静态因素。目前,长沙城市堤防设防高度偏高,减少了大堤的稳定性,造成了无效投资,影响了城市景观。防洪工程建设应分期实施、先除险后加固、注重整体防洪能力的提高,并处理好与城市基础设施建设和景观建设的关系。  相似文献   

本世纪西北气候可能转型的依据和原因分析   总被引：21，自引：4，他引：17  

汤懋苍  高晓清  朱德琴 《冰川冻土》2003,25(2):170-173

西北气候是否正在或已经转型不仅是个科学问题,它也与该地区甚至全国的生态建设和国民经济的可持续发展密切相关.从地球系统科学的角度出发,对西北地区气候转型问题进行了探讨.利用太阳活动周期长度、孢粉及冰芯等资料,在分析了西北气候变化的周期规律后指出,西北气候已经完成了由冷到暖的“转型”;推测西北的“千年湿期”将从22世纪开始;西北东部气候转为湿型可能要发生在2020年以后.  相似文献