QBO Features of Tropical Pacific wind Stress Field with the Relation to El Nino     

Zhang Qin  Zhu Yufeng  Ni Yunqi 《大气科学进展》1995,12(1):87-94

Analysis has been implemented of 1970-1992 tropical Pacific wind stress anomaly and sea surface temperature anomaly (SSTA) datasets, indicating that quasi-biennial oscillation (QBO) of the tropical Pacific WS and SSTA is featured both by a standing and a progressive form, the former emerging in the most intense centers of action and the latter travelling east- or west-ward out of the SSTA sources. Results show that the SSTA is in the warm (cold) phase as zonal component of euqatorial wind stress anomaly gets weakened (reinforced) and the QBO of wind stress anomaly is well related to the El Nino cycle.  相似文献   

全息地层学原理与方法综述   总被引：2，自引：0，他引：2       下载免费PDF全文

吴智勇  姜衍文 《地质论评》1995,41(5):426-431

全息地层学是以全球旋回地层学和高分辨率事件地层学为基础，综合生物地层学、磁性地层学、化学层学以及构造地层学等地层学各个分支的研究结果，以崭新的思路，全方位地开发和提取出沉积记录中所蕴涵的各类地层学信息，从而以极高的时间精度划分对比地层的综合性地层学。  相似文献   

兰村煤矿沉积体系特征及其对含煤性的控制     

刘正根 《湖南地质》1995,(2)

攸县兰村煤矿区晚二叠世的充填沉积，可划分为滨海粉砂淤泥盆地、海湾泻湖、三角洲、障壁坝－泻湖及浅海钙泥质台地等５个沉积体系。本文分析了海进海退旋回对沉积体系含煤性的控制。  相似文献   

18．6年地震轮回及其成因初探   总被引：10，自引：4，他引：10       下载免费PDF全文

杜品仁 《地球物理学报》1994,37(3):362-369

将全球地震高发地区分成１３个研究区，分析各区浅源大地震（１８９７－１９９０年）与１８．６年月亮交点运动周期的关系，发现各区均有明显的１８．６ａ地震轮回存在：活跃期为１２．４ａ，平静期为６．２ａ．提出了软流层岩浆潮的概念，分析１８．６ａ地震轮回的成因是软流层岩浆潮的调制作用，并把这种解释称为岩浆潮假设．全球火山活动的１８．６ａ准周期性和各地震活跃期中心时间分布的规则性是对岩浆潮假设的支持．地震轮回可认为是全球或某一地区对地球内部和外部的非线性相互作用的响应或自组织过程．  相似文献   

地层对比的地质地球化学新方法——兼论武当山—安康—勉略—带中上元古界的对比     

汪东波  张本仁  马振东  夏松饶  雷和平 《矿产与地质》1993,(1)

全面地介绍了同位素地质年代学、马尔柯夫过程分析(极限概率、熵分析、置换性分析)和元素地球化学在古老地层对比研究中的应用.并以武当山—安康—勉略—带中上元古界为例,系统地剖析了区内中上元古界的时代、层序、岩石组合类型、沉积旋回特征、岩石表明,分布于勉略一带的碧口群同武当山群、郧西群、耀岭河群存在显著差异,难以对比;武当山和安康两地的耀岭河群基本上可以对比,而郧西群仅相当于武当群的一部分.  相似文献   

Spatial and temporal variations of methanesulfonic acid and non sea salt sulfate in Antarctic ice     

M. Legrand  C. Feniet-Saigne  E. S. Saltzman  C. Germain 《Journal of Atmospheric Chemistry》1992,14(1-4):245-260

A simultaneous glaciochemical study of methanesulfonic acid (MSA) and non-sea-salt sulfate (nss-SO₄ ^-) has been conducted on the Antarctic plateau (South Pole, Vostok) and in more coastal regions. The objective was to investigate marine sulfur emissions in very remote areas. Firstly, our data suggest that MSA and nss-SO₄ present in antarctic ice are mainly marine in origin and that DMS emissions have been significantly modulated by short term (eg. El Nino Southern Oscillation events) as well as long term climatic changes in the past. Secondly, our study of spatial variations of these two sulfur species seems to indicate that the atmosphere of coastal antarctic regions are mainly supplied by local DMS emissions whereas the atmosphere of the high plateau is also influenced by DMS emissions from more temperate marine latitudes. Thirdly, our study of the partitioning between MSA and nss-SO₄ suggest that the temperature could have been an important parameter controlling the final composition of the high southern latitude atmosphere over the last climatic cycle; colder temperature favoring the formation of MSA. However, our data also support a possible role played by changes in the transport pattern of marine air to the high antarctic plateau.  相似文献   

数据库应用系统通用模块的研究     

Gao Wenpei 《吉林大学学报(地球科学版)》1989,(3)

通过对各种数据库管理应用系统的研究,寻求其通用的部分,把它们研制成通用的管理模块,反过来用到各种管理系统中去。 这样避免了轶件开发过程中低水平的重复性劳动;为了提高软件的质量,提高开发某一应用系统的速度,研制出一套适合于各种各样用途的工具模块,当需开发一个新的管理系统时,用这些工具模块很快就可以编制出一个较大的程序;通用模块的开发是站在软件工程的高度,遵循结构程序设计原理,按照自顶向下,逐步求精的原则和方法进行研制的,便于移植和维护,使各种管理系统走向标准化。  相似文献   

冀东滦县地区前寒武纪铁矿与火山喷发沉积旋回的关系     

Yang Changming 《地球科学》1986,(1)

本区原岩建造是-套基性—酸性火山凝灰岩（主要）+铁硅质岩+沉积岩组合。整个层序反映了一个较完整的火山喷发沉积旋回。含铁建造与沉积旋回在时空和物源上存在着密切的成因联系。铁矿的形成及分布并非受控于某一种岩石,而是受控于火山喷发沉积旋回。本文从岩浆分异、火山活动、沉积作用及构造运动等的发生、发展、演化的角度较全面地分析了火山喷发沉积旋回的控矿作用。  相似文献   

New production and mixed-layer physics     

Shubha Sathyendranath  Trevor Platt 《Journal of Earth System Science》1994,103(2):177-188

We treat the ocean carbon cycle as a coupled physical-biogeochemical process. The interactions between mixed-layer dynamics and growth of phytoplankton in the layer are discussed, and the formal relationship between phytoplankton accumulation and new production is examined. A coupled biological-physical model is presented for studying the classical spring bloom in the N. Atlantic, and possible differences in the mechanisms that drive the seasonal phytoplankton blooms in the N. Atlantic and the Arabian Sea are discussed. Finally, recommendations are made for observational programs to improve our understanding of the biologically-mediated carbon cycle in the Arabian Sea.  相似文献   

Extraction of sedimentological information via computer-based image analyses of gray shales in carboniferous coal-bearing sections of Indiana and Kansas, USA     

Allen W. Archer 《Mathematical Geology》1994,26(1):47-65

Fine-scale fabric within shales can be used to interpret environments of deposition. In particular, systematic variations in lamina thicknesses can be used to suggest the presence or absence of specific sedimentological controlling factors, such as tides. Herein, shale fabric is analyzed from Carboniferous coal-bearing and siliciclastic-rich formations in Indiana and Kansas. The shales exhibit well developed, normally graded lamina. Sediment grain sizes range from silt and sand at the base of the lamina up to silt and clay at the top. Computer-based optical scanning of prepared shale samples was undertaken so that the lamina thicknesses could be extracted automatically and then used for thickness-series analysis. The sands and silts tend to be very light in color because they consist of well sorted, quartz-rich sands. Conversely, the silt and clay that cap the laminae tend to be dark because of the small grain size; such fine-grained layers also contain large amounts of macerated and coalified plant material. Grain size and sedimentological differences within the laminae can be detected by optical properties and this facilitates automated image processing. Extraction of laminae thicknesses and harmonic analyses of laminae-thickness series can then be used to test the reasonability of specific environmental processes, such as tidal forcing, that were operative during the formation of these shales.  相似文献