洞庭湖盆地沉积环境分析方法探索   总被引：2，自引：0，他引：2  

皮建高  张国梁 《湖南地质》1993,12(3):196-199

本文利用洞庭湖盆经定量化处理后的定性资料,探索了一种用水流能量指数来定量研究沉积环境的方法。按此法研究后提出,更新世早期古沅水从桃源向北流经临澧湖盆,再进入澧县湖盆的新认识。  相似文献   

1995年云南孟连西7.3级地震前震序列特征及其与主震的关系     

刘祖荫  钱晓东  张俊伟 《湖南地质》1998,(4)

在分析１９９５年云南孟连西７３级地震的前震序列时,发现跟踪最大前震６２级的余震序列中,有一组较大震级的地震呈现出随时间的增长不断线性递增的特点,这种特点在云南其他震例中也曾多次出现过。利用修正的大森公式ｎ（ｔ）＝ｋ／（ｔ＋ｃ）ｐ拟合该序列,在获得的参数重新构造的频度－线性化时间坐标中,这一组地震显示出与海城前震序列随时间变化震级出现非线性增强的共同特征。采用表征物质加速应变而失稳的方程ｄ（∑Ｍ０１／２）／ｄｔ＝ｃ／（ｔｍ－ｔ）ｎ,对孟连西前震序列多方面进行跟踪定量分析,预测主震的发生时间平均比实发时间仅推迟２６ｍｉｎ,震级相差０１７级。  相似文献   

库车前陆褶皱冲断带中段第三系盐枕构造   总被引：16，自引：10，他引：16  

汤良杰  贾承造  金之钧  皮学军  陈书平  谢会文 《地质科学》2003,38(3):281-290

本文旨在探讨库车前陆褶皱冲断带盐枕构造的类型、分布、成因机制及其与油气聚集的关系。通过地震反射剖面的解释和石油地质条件综合分析,认为库车前陆褶皱冲断带由北而南依次发育残留盐枕、非稳态盐枕和稳态盐枕等 3类盐枕构造,沿克拉苏构造带和西秋立塔克构造带呈长条形带状分布,其成因受重力滑动、重力扩展、区域挤压和塑性流动作用的联合控制。从盐枕构造的演化序列和分布特征看,该区盐枕构造的主要特点表现为:北部盐枕形成较早,稳定性差,出现残留盐枕,盐枕规模较小;南部盐枕形成较晚,稳定性较强,形态相对完整,规模较大。库车前陆褶皱冲断带盐枕构造与油气聚集密切相关,伴随盐枕构造的形成,发育大量盐相关油气圈闭构造,沿盐枕构造成带状分布,同时盐枕构造巨厚的盐岩层为油气聚集提供了良好的封闭条件。  相似文献   

Characterisation and modelling of marine dissolved organic matter interactions with major and trace cations     

Yoann Louis  Cédric Garnier  Véronique Lenoble  Dario Omanović  Stéphane Mounier  Ivanka Pižeta 《Marine environmental research》2009,67(2):100-107

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The Composite Effect of Nanometer MnO2 Mixed with the Electrolytic MnO2     

杨超刘卓钦  田熙科皮振邦 王圣平 《中国地质大学学报(英文版)》2007,18(2):172-176

The nanometer MnO2 has outstanding electrochemical performance theoretically, but it is not suitable for actual utilization, which may result in capacity decrease and resource waste. In this study we have utilized the characterizations of the nanometer material, synthesized a type of nanometer α-MnO2 through KMnO4 and KNO3 with hydrothermal method, and mixed the products into micron electrolytic manganese dioxide （EMD） to enhance the electrochemical performance of the electrode.The cyclic voltammogram and galvanostatical discharge measurements of the samples were investigated. It is found that the 50﹪ nanometer MnO2 mixed electrode has the best electrochemical performance. The electrochemical performance improvement mechanism of the sample nanometer MnO2 mixed into micron EMD was discussed. With the existence of electrolyte, the nanometer MnO2 particles filled into the interspaces of the micron EMD particles, the mass and charge transfer conditions of the electrode reaction were improved, and the electrode polarization was diminished.  相似文献   

Detection of Extended Thermal Infrared Emission around the Vega-like Source HD 141569     

Fisher RS  Telesco CM  Piña RK  Knacke RF  Wyatt MC 《The Astrophysical journal》2000,532(2):L141-L144

We report the detection of extended IR emission at 10.8 and 18.2 μm around the Vega-like source HD 141569. Mid-IR imaging with OSCIR on Keck II shows emission from dust extending out to 100 AU from the B9.5 Ve star. Our modeling of the dust places an upper limit of approximately 2 μm on the diameter of the mid-IR-emitting particles if they are Mie spheres of astronomical silicates. Comparison of our mid-IR images to the near-IR (1.1 μm) NICMOS images of HD 141569 (Weinberger et al. 1999) shows that the mid-IR emission originates at smaller distances from the star than the scattered near-IR light, as also previously observed for the archetype Vega-like source beta Pictoris.  相似文献   

Comparative validation of statistical and dynamical downscaling models on a dense grid in central Europe: temperature     

Radan Huth  Jiří Mikšovský  Petr Štěpánek  Michal Belda  Aleš Farda  Zuzana Chládová  Petr Pišoft 《Theoretical and Applied Climatology》2015,120(3-4):533-553

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编制岩土工程勘察纲要若干问题探讨     

刘玉德  陈建强  孙桂林  张丕  艾云峰 《吉林地质》2011,30(4):107-109

本文论述了岩土工程勘察评价中勘察纲要的重要性、岩土工程勘察阶段和工程类型,重点阐述了编写勘察纲要应注意的问题,这对指导岩土工程勘察具有实际意义。  相似文献   

Automated suitable drainage network extraction from digital elevation models in Taiwan's upstream watersheds     

Wen‐Tzu Lin  Wen‐Chieh Chou  Chao‐Yuan Lin  Pi‐Hui Huang  Jing‐Shyan Tsai 《水文研究》2006,20(2):289-306

Automatically extracting drainage networks from digital elevation models coupled with the constant stream threshold value is a regular method. These extracted networks can be verified by comparing the channel initiation points with those from real networks. From the results analysed, the differences in channel initiation points will affect the network geometries, geomorphological indices and hydrological responses. This paper develops two automatic algorithms, the headwater‐tracing method and the fitness index, to trace the flow paths from headwaters to the outlet and to calculate the reasonable stream threshold. Instead of the method determined by trial and error or field survey, the accurate channel initiation points can be obtained from airborne photographs coupled with high‐resolution SPOT images for suitable drainage network extraction. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献   

Climatic and tectonic controls on carbonate deposition in syn‐rift siliciclastic fluvial systems: A case of microbialites and associated facies in the Late Jurassic          下载免费PDF全文

Concha Arenas  Laura Piñuela  José Carlos García‐Ramos 《Sedimentology》2015,62(4):1149-1183

This work provides new insights to assess the factors controlling carbonate deposition in the siliciclastic fluvial systems of rift basins. Sedimentological and stable‐isotope data of microbialites and associated carbonate facies, along with regional geological information, are shown to reveal the influence of climate and tectonics on the occurrence and attributes of carbonate deposits in these settings. The Vega Formation – a 150 m thick Lower Kimmeridgian siliciclastic fluvial sequence in Asturias Province (northern Spain) – constitutes a candidate for this approach. This unit includes varied facies (stromatolites; rudstones, packstones and wackestones containing oncoids, intraclasts, charophytes and shell bioclasts; marlstones and polygenic calcareous conglomerates) that formed in a low‐gradient fluvial–lacustrine system consisting of shallow, low‐sinuosity oncoid‐bearing channels and pools within marshy areas, with sporadic coarse alluvial deposition. The sedimentological attributes indicate common erosion by channel overflow and rapid lateral changes of subenvironments caused by water‐discharge variations. The carbonate fluvial–lacustrine system developed near uplifted marine Jurassic rocks. The occurrence of the system was conditioned by normal faults (active during the deposition of the unit) that favoured: (i) springs of HCO₃–Ca‐rich water from a Rhaetian–Sinemurian carbonate rock aquifer; and (ii) carbonate deposition in areas partially isolated from the adjacent siliciclastic fluvial system. The microbialite δ¹³C and δ¹⁸O values support deposition in a hydrologically open system, fed by ambient‐temperature meteoric water, with riparian vegetation. Three types of lamination in the stromatolites and oncoids reflect distinct morphological types of cyanobacterial communities. The textural pattern of lamination parallels δ¹³C and δ¹⁸O changes, suggesting short‐term cycles of precipitation and temperature. A moderately to strongly contrasted seasonal and/or pluriannual precipitation regime is inferred from the cyclic δ¹³C pattern of the lamination and from the discontinuous and asymmetrical growth of oncoids. Thus, the isotopic and sedimentological attributes of the carbonate deposits were linked to short‐term climate changes associated with semi‐arid conditions, consistent with the studied climatic zone.  相似文献