C-, Sr-isotope and Hg chemostratigraphy of Neoproterozoic cap carbonates of the Sergipano Belt,Northeastern Brazil     

Alcides Nobrega Sial  Claudio Gaucher  Marinho Alves da Silva Filho  Valderez P. Ferreira  Marcio M. Pimentel  Luiz D. Lacerda  Emmanoel V. Silva Filho  Wilker Cezario 《Precambrian Research》2010

Two cap carbonates overlying glaciogenic diamictites crop out extensively in the eastern Vaza Barris Domain of the Sergipano Belt, northeastern Brazil. They are represented by carbonates of the Jacoca Formation, resting on top of diamictite of the Ribeiropolis Formation, and by the Olhos D’Agua Formation (carbonates, organic-rich towards the top), which overlies diamictite of the Palestina Formation. These two sequences were deformed and metamorphosed at sub-greenschist facies-conditions during the Brasiliano cycle (650–600 Ma).  相似文献   

1m红外太阳望远镜光电导行系统中像场旋转的分析     

邓林华  许骏  宋腾飞  黄善杰  向永源 《天文研究与技术》2010,7(3)

云南天文台1m红外太阳望远镜(YNST)光电导行系统是基于检测太阳像在面阵CMOS图像传感器上的偏移量作为反馈控制信号的高精度闭环跟踪系统[1]。由于YNST是一个地平式装置,在太阳像偏移检测量中存在着像场旋转量,为了获取稳定清晰的太阳像,必须对检测量进行消旋[2]才能达到光电导行系统的跟踪要求。根据球面天文学及天体测量学的知识并结合导行镜的光学系统,推导了光电导行系统中像场旋转的变化规律并对其进行模拟分析。  相似文献   

球体内点位错产生的球型位移场：II．位错Love数          下载免费PDF全文

孙文科  大久保修平 《地球物理学报》1995,38(1):70-82

本文进一步研究了ＳＮＲＥＩ地球模型内位错所产生的球型位移场问题．作为特例，讨论了位错位于地表时的解和计算技巧．对于１０６６Ａ地球模型进行了具体计算．给出了深度分别为５，１０，３２，１００，３００和６３７ｋｍ的４种类型位错的位错Ｌｏｖｅ数的结果．  相似文献   

南极洲乔治王岛柯林斯冰帽的温度分布          下载免费PDF全文

韩建康  温家洪  尚新春  金会军 《极地研究》1995,7(1):62-69

钻孔内温度实测表明，柯林斯冰帽积累区大部分呈温性，消融区可能呈冷性。冰帽活动层温度明显受气温季节变化的影响，降水暖渗浸对冰的增温作用显著，雪盖对温度分布也显示了一定的影响。测量显示，冰帽纵深层的温度大都接近融点，而小冰穹顶附近十数米范围内温度变化较大。小冰穹顶附近，钻进时３０ｍ以下孔中出水现象显著，可能是冰内径流、差异运动和较高盐度等因素共同作用的结果。  相似文献   

中国地区地磁场的球冠谐和分析   总被引：12，自引：11，他引：12  

安振昌 《地球物理学报》1993,36(6):753-764

本文根据中国及其邻近地区的地磁三分量绝对测量资料,利用球冠谐和分析方法,计算出中国地区地磁剩余场的冠谐模型,地磁剩余场△X,△Y,△Z的模型均方根偏差分别为106.9,89.7,137.6 nT.提出由地磁场的国际参考地磁场和地磁剩余场的冠谐模型组成的联合模型作为中国参考地磁场的模型,它能较好地表示中国地磁场的分布.以地磁场的联合模型为正常背景场,计算出三分量磁异常的冠谐模型,并分析了磁异常的基本特征,它将为深入研究中国岩石层结构提供新证据.  相似文献   

南极洲乔治王岛柯林斯冰帽冰芯层位和密度变化的一般特征   总被引：1，自引：0，他引：1       下载免费PDF全文

韩建康  康建成  温家洪  尤贝拉斯  Ｆ．罗德里格斯 《极地研究》1994,6(1):43-49

柯林斯冰帽两支冰芯层位记录证实了该冰帽主冰穹顶部（海拔约７００ｍ）属暖渗浸带，小冰穹顶部（海拔约２５０ｍ）属渗浸带。雪、冰的层位分布和密度变化包含了一定的测年信息。主冰穹顶冰芯密度－深度曲线在表层呈现韵律性变化，与层位记录中的融化冻结现象相对应，据此粗略划分年层，断定当地年积累雪层厚度为３－３．５ｍ，折合水当量１６５０－１９２５ｋｇ／ｍ２ａ，年平均积累速率约为２．０ｍ／ａ（冰当量）。主冰穹顶成冰深度为３８－３９ｍ，此深度以上密度自上而下缓慢增加，但以下由于含水层的出现，密度迅速升高，在５－６ｍ区间达到９００ｋｇ／ｍ３。小冰穹冰芯除表层外，密度基本在８００－９００ｋｇ／ｍ３之间，冰芯中雪冰互层，存在污化面，４０ｍ以下发现很厚的火山灰沉积物。小冰穹平均年积累率约为０．７ｍ／ａ（冰当量），成冰深度７－８ｍ，成冰年限为１０年左右  相似文献   

Asymptotic theory for calculating deformations caused by dislocations buried in a spherical earth: geoid change   总被引：2，自引：0，他引：2  

W. Sun 《Journal of Geodesy》2003,77(7-8):381-387

An asymptotic theory is presented for calculating co-seismic potential and geoid changes, as an approximation of the dislocation theory for a spherical Earth. This theory is given by a closed-form mathematical expression, so that it is mathematically simple and can be applied easily. Moreover, since the asymptotic theory includes sphericity and vertical structure effects, it is physically more reasonable than the flat-Earth theory. A comparison between results calculated by three dislocation theories (the flat-Earth theory, the theory for a spherical Earth and its asymptotic solution) shows that the true co-seismic geoid changes are approximated better by the asymptotic results than by those of a flat Earth. Numerical results indicate that the sphericity effect is obvious large, especially for a tensile source on a vertical fault plane. AcknowledgementsThe author is grateful to Dr S. Okubo for his helpful suggestions and discussions. Comments by anonymous reviewers are also greatly acknowledged. This research was financially supported by JSPS research grants (C13640420) and Basic design and feasibility studies for the future missions for monitoring Earths environment.  相似文献   

Évolution pression–température des amphibolites de la zone axiale au cours du métamorphisme hercynien des Pyrénées orientales     

Claude Triboulet  Gérard Guitard  Ildiko Katona  Marina Navidad 《Comptes Rendus Geoscience》2005,337(14):1244-1249

Thin levels of amphibolites from the Canigou, Albères and Cap de Creus massifs have been studied in order to investigate their pressure and temperature evolution during time. P and T values have been calculated using the amphibole–plagioclase–quartz thermo-barometer. Si, Al, Mg and Fe of zoned amphiboles have been analysed from core to rim by microprobe. By combining the results obtained from several (or different) crystals, P–T–t paths have been determined using the amphibole-plagioclase-quartz equilibriums. In the Canigou Massif, the amphibolites have recorded anti-clockwise P–T–t paths around a peak of metamorphism located at about 650?°C–6.1 kbar, whereas in the Albères Massif, the calculated P–T–t paths of amphibolites near the paragneisses are retrograde only, from 600?°C–5 kbar to 450?°C–2.5 kbar, but one cummingtonite-bearing amphibolite has also recorded an anti-clockwise evolution around 650?°C–4.5 kbar. The retrograde P–T–t paths recorded for amphibolites from the ‘Cap de Creus’ Massif are retrograde only, from 650?°C–6 kbar and 400?°C–1 kbar. To cite this article: C. Triboulet et al., C. R. Geoscience 337 (2005).  相似文献   

500 hPa球函数谱异常用于我国东部汛期降水预测的尝试   总被引：1，自引：0，他引：1       下载免费PDF全文

周晓霞  王盘兴  周春华  李丽平 《气象科学》2004,24(1):88-94

用北、南半球500hPa月平均位势高度场球函数系数资料代替格点资料，用区域降水指数表示华北、江淮、华南五区汛期(6～8月)降雨。通过引进复相关系数和构造复相关系数场模．分析了半球500hPa环流与我国东部汛雨异常的同时和时滞相关联系。在此基础上．选取5月份北半球、1月份南半球球函数系数与东部汛期降水作时滞的奇异值分解。由此得到的预测关系在1998～2001年汛期降水预报试验中取得了一定效果，从而对500hPa环流的球函数系数资料在区域月、季长期天气预报中的应用作了有益的尝试。  相似文献   

The compatibility conditions in altimetry–gravimetry boundary value problems     

R.S. Grebenitcharsky  M.G. Sideris 《Journal of Geodesy》2005,78(10):626-636

The role of compatibility conditions for altimetry–gravimetry boundary value problems (AGBVPs) is quite complicated by way of: guaranteeing the existence of the solution; smoothing the data (boundary conditions) at the boundary; and providing a higher level of regularization and smoothness to the solution. Pseudo-differential operators (PDOs) can be applied not only for the reformulation of AGBVPs in a simple way, but also for imposing compatibility conditions at the coastline. It is shown here that spherical PDOs can be combined with the theory of spherical harmonics and spherical wavelets to obtain a numerical solution for AGBVPs with compatibility conditions along the coastline. The role of compatibility conditions, is summarized and emphasized and compatibility conditions are given in an explicit form based on the combined representation of functionals of the disturbing potential in terms of spherical harmonics, spherical PDOs and wavelets. Numerical aspects of the application of the compatibility conditions to a case-study area in Canada are discussed.  相似文献