Carbonate platform development in a Paleoproterozoic extensional basin,Vempalle Formation,Cuddapah Basin,India     

《Journal of Asian Earth Sciences》2014

Sedimentological investigation of the late Paleoproterozoic (Orosirian) Vempalle Formation of the Cuddapah Basin, Dharwar craton, India, reveals three facies association that range from supratidal to deep subtidal. Sedimentary rocks of this succession are dominated by heterolithic carbonate mudstone, intraformational carbonate conglomerate, and a variety of columnar, domal, and stratiform microbialite facies. Deposition occurred in an extensional regime during development of a low-gradient ramp, where the distribution of microbialite facies is distinctly depth-partitioned. A gradual increase in synoptic relief of columnar stromatolites through the section, and the upward transition from stratiform to columnar microbialites, record a prolonged marine transgression with little or no influx of terrigenous detritus. Siliciclastic influx along the northeastern side of the shelf reflects the redistribution of topographic highs concomitant with large scale volcanic activity. Redistribution of topographic highs eventually led to progradation of peritidal facies and shutting down of the carbonate factory. Earthquake-induced ground shaking and voluminous volcanism experienced by this platform point to the reactivation of a deep-seated mantle-plume that resulted in thermal doming of the Dharwar crust prior to the onset of Cuddapah deposition. Isotopic and elemental chemistry of a selection of Vempalle Formation carbonate rocks record elevated Mn²⁺ and Fe²⁺ concentrations and depleted carbon isotope values in inner ramp lagoonal facies, relative to more open marine stromatolitic facies. Patterns of isotopic and elemental variation suggest the presence of geochemically distinct water masses—either within the water column or within substrate pore fluids—that resulted from a combination of globally low marine oxygenation and restricted oceanographic circulation in inner ramp environments. These data suggest that, even in the aftermath of Early Paleoproterozoic oxygenation, that ocean chemistry was heterogeneous and strongly affected by local basin conditions.  相似文献   

磨刀门水道咸潮上溯动力特性分析   总被引：1，自引：0，他引：1       下载免费PDF全文

陈文龙  邹华志  董延军 《水科学进展》2014,25(5):713-723

为研究磨刀门水道咸潮上溯的动力特性,基于非结构网格海洋模型（Finite Volume Coastal Ocean Model,FVCOM）,构建了覆盖珠江河口及其上游网河区的高分辨率三维斜压数值模型,采用实测资料对其进行率定和验证,并开展了咸潮上溯的数值模拟计算。根据计算结果和实测资料,对磨刀门水道大、中、小潮期间的盐淡水分层与混合特征、盐分物质的分层输移机制进行分析,探讨其咸潮上溯强度时空分布差异的原因。结果表明:小潮期,底层累积盐通量明显大于表层,净输移方向为陆向;大潮期,表层累积盐通量明显大于底层,净输移方向为海向;而平衡点一般出现于中潮期,这就是磨刀门水道咸潮上溯最强和最弱时刻分别出现于小潮和大潮后的中潮期的原因所在。  相似文献   

长江口拦门沙深水入海航道整治工程的研究   总被引：5，自引：1，他引：5  

王广平 《海洋工程》1994,(2)

随着国民经济的发展和上海浦东新开发区的发展，长江口深水入海航道的选择与治理，已越来越多地引起人们的关注，长江口深水入海航道的选择基本上可以分为避开拦门沙和不避开拦门沙两类。本文根据长江河口的发育模式、河口延伸、汊道演变的规律、汊道的形态与水力条件，提出长江口拦门沙深水入海航道整治规划，近期以北槽－８ｍ航槽为宜，远期可逐步开发至－１２．５ｍ  相似文献   

磨刀门水道枯季水动力特性分析   总被引：2，自引：0，他引：2       下载免费PDF全文

方神光  王少波 《水文》2013,33(5):70-74

根据2009年12月1025日磨刀门水道上至竹银下至口门近半月的同步实测水文资料,对该水道在大、中、小潮下表、中、底层的水动力特性进行了分析和探讨。结果显示,枯季磨刀门水道总体涨、落潮流速都不大,即使大潮时该水道总体表层涨落潮平均流速分别仅为0.5m/s和0.76m/s;水动力特性一般呈现:表层落潮流速显著大于涨潮流速,底层涨、落潮流速相差不大的规律;表底层涨落潮流速一般呈现随潮型增大而增大的趋势;表层涨潮历时小于落潮历时,底层涨潮历时大于落潮历时;实测结果显示,包括口门及上游河道范围内的表、底层流速出现相反的现象,时段一般出现在经过第一个长时间的落潮流之后的第二个较短落潮时间段内,且沿水深方向的转流点更为靠近表层。  相似文献   

Vertical bifurcation families from the long and short period families around the equilateral equilibrium points     

X. Y. Hou  L. Liu 《Celestial Mechanics and Dynamical Astronomy》2008,101(3):309-320

In this paper, following the increase of the mass ratio μ, the vertical stability curves of the long and the short period families were studied, and the vertical bifurcation families from these two families were computed. It is found that these vertical bifurcation families connect the long and short period families with the spatial periodic family emanating from the equilateral equilibrium points. The evolution details of these vertical bifurcation families were carefully studied and they are found to be similar to the planar bifurcation families connecting the long period family with the short period family in the planar case.  相似文献   

On particle trajectories in restricted 3-body problem including the effect of radiation: Sun-Jupiter system     

M. K. Das  Pankaj Narang  M. Yuasa  L. M. Saha 《Astrophysics and Space Science》2008,314(1-3):59-71

In this work, we have simulated orbits of a particle moving in gravitational field of the Sun-Jupiter system. The effect of solar radiation pressure, including Poynting Robertson drag, on the evolution of particle orbits in phase space have been studied for different values of the parameter β ₁ (the ratio of radiation to gravitational force) and initial conditions. Characteristics of various computed trajectories have been studied using wavelet transform (WT), Fourier transform (FT) and Poincare surface of section method. We use wavelet analysis to identify transitions of a trajectory in time-frequency plane and further apply it to classify it as regular or chaotic in phase space. Unlike the Fourier transform method (FT), we observe that the wavelet transform (WT) also provides a basis to identify ‘sticky’ trajectories in the present dynamical system.  相似文献   

浅论信息化测绘与数字航道的关系     

张国平  杨品福  陆英 《地理空间信息》2010,8(4):63-65

简要介绍了"数字航道"技术体系和构成框架,说明了信息化测绘的基本组成,初步探讨了"数字航道"与信息化测绘之间的关系,以及面向"数字航道"构建航道信息化测绘的主要内容和研究重点。  相似文献   

基于WebGIS的港口航道管理信息系统设计     

黄海  祝国瑞  林孝松 《地理空间信息》2006,4(6):44-46,47

结合澜沧江-湄公河港口航道地理信息系统开发建设实践,提出了基于WebGIS的港口航道地理信息系统的方案和实现方法,采用MapXstreme平台,利用ASP技术和脚本语言JavaScript,以及HTML技术、响应用户端的动态请求,实现对港口航道信息的查询、统计、三维显示及输出等。  相似文献   

Localizing and quantifying groundwater-surface water interactions at different scales: A tracer approach at the River Moselle,Germany     

Michael Engel  Simon Mischel  Sabrina Quanz  Sven Frei  Dirk Radny  Rike Voelpel  Axel Schmidt 《水文研究》2024,38(5):e15118

Groundwater-surface water interactions (GSI) connect rivers and streams with riparian areas and the adjacent aquifer. Although these interactions exert a substantial control of quantity and quality of both groundwater and surface water, knowledge on GSI along rivers at the regional scale, particularly for inland waterways, is still limited. We investigated GSI along the river Moselle, an important federal inland waterway in Germany, by using radon and tritium to identify gaining (water flux from the aquifer to the surface water) and losing (water flux from the surface water to the aquifer) stream conditions, respectively. Gaining stream conditions were identified by continuously measuring radon along the river during boat surveys with a high spatial resolution (every 2 km) during intermediate (October 2020) and near low flow conditions (August/September 2021). The tritium concentrations in surface water and groundwater and the resulting tritium inventories were used to characterize losing stream conditions Monthly tritium inventories from 2017 to 2022 revealed a mean loss for the whole period of 20.3 % and a mean gain of 21.8%. Both were probably triggered by a combination of losing stream conditions and flood-induced mass transfer of water from the aquifer back into the river as well as discharge fluctuations. At the investigated site Lehmen there were direct indications of an influence of surface water due to elevated tritium concentrations in the groundwater (up to 13.3 Bq L⁻¹). Using radon mass balance modelling, good agreements of simulated versus measured radon data with respect to two groundwater end-member scenarios were obtained during intermediate flow (Spearman's ρ: 0.97 and 0.99; MAE: 10.1 and 3.4 Bq L⁻¹) and near low flow (Spearman's ρ: 0.97 and 0.99; MAE: 11 and 6.5 Bq L⁻¹). Considerable groundwater inflow was limited to the meander of Detzem, where cumulated groundwater inflow of about 19 m³ s⁻¹ (9.5% of total discharge) and 4.2 m³ s⁻¹ (3.8% of total discharge) was simulated during intermediate and near low flow, respectively. However, the groundwater inflow was relatively low compared to alpine streams, for example. The study will help to better identify and quantify GSI at the regional scale and provide methodological guidance for future studies focusing on inland waterways.  相似文献   

从美因-多瑙运河谈到我国规划的湘桂运河和粤赣运河     

梁国昭 《热带地理》1998,18(1):18-23

经７０年代的建设,德国的美因－多瑙运河于１９９２年建成通航。虽然德国国内对这一宏大的工程颅有争议,但工程建设中有不少经验可供我国参考。我国已规划在２１世纪兴连接长江水系和珠江水系的湘桂运河和粤赣运河。规划的湘桂运河位于古灵渠附近;粤赣运河位于广东南雄和江西信丰之间。建设这两条运河的天然条件均优于美国－多瑙运河。为保护漓江山水资源,建议重新考虑湘桂运河的位置,提出在广西富川和湖南江化之间选址。  相似文献