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131.
苏里格气田苏6井区下石盒子组盒8段沉积相特征 总被引:35,自引:2,他引:35
苏6井区是鄂尔多斯盆地苏里格气田主要产气区,主产层为中二叠统下石盒子组第8段,其沉积相类型及特征长期倍受众多研究机构和学者的争议。根据钻井、测井及岩芯分析化验资料,结合前人研究成果,认为苏6井区盒8段属河流沉积体系,其中盒8下段为辫状河,盒8上段为曲流河。在深入细致的微相分析基础上,分别建立了缓坡型辫状河与多河道低弯度曲流河两种沉积模式,认为最有利的储集砂体主要为高能水道心滩和边滩叠置砂体,其次为河床滞留砂体。上述沉积相类型划分和沉积模式的建立为包括苏6井区在内的整个苏里格气田储集相带预测、储层评价以及大规模开发奠定基础。 相似文献
132.
We report oxygen isotope data from a 108-yr (1885–1993) sequence with annual laminae of bio-induced authigenic calcite in a frozen core from Baldeggersee, a small lake in Central Switzerland. These isotope results provide proxy data on the isotopic composition of past precipitation in the Baldeggersee catchment region and are quantitatively compared with instrumental climate data (i.e. mean annual air temperature and atmospheric circulation pattern indices) to evaluate climatic controls on oxygen isotopes in precipitation.Monitoring the isotope hydrology of Baldeggersee demonstrates that the oxygen isotopic composition of the lake water is controlled by the isotopic composition of local atmospheric precipitation (18Op) and that the isotopic signal of precipitation is preserved, albeit damped, in the lake calcite oxygen isotope record (18Oc). Comparison of the calcite oxygen isotope proxy for 18Op in the catchment with historical mean annual air temperature measurements from Bern, Switzerland confirms that authigenic calcite reliably records past annual air temperature in the region. This 18Oc/temperature relationship is calculated to be 0.39/°C for the period 1900–1960, based on an isotope mass-balance model for Baldeggersee. An exception is a 0.8 anomalous negative shift in calcite 18O values since the 1960s. Possible explanations for this recent 18Oc shift, as it is not related to mean annual air temperature, include changes in 18Op due to synoptic circulation patterns. In particular, the 0.8 negative shift coincides with a trend towards a more dominant North Atlantic Oscillation (NAO) index. This circulation pattern would tend to bring more isotopically more negative winter precipitation to the region and could account for the 0.8 offset in 18Oc data. 相似文献
133.
Astrid Holstad 《Computational Geosciences》2000,4(2):103-139
We formulate mathematical and numerical models for multispecies, multi-phase and non-isothermal reactive fluid flow in porous
media focusing on the chemical reactions and the transport of solutes. Mass conservation and stability in the time integration
are emphasized. We use cell-centered finite volume differencing in space and an implicit Runge-Kutta method in time. Assuming
two space dimensions, we introduce flux approximation for arbitrarily shaped convex quadrilaterals. On equidistant and variable
sized rectangular grids we choose limited κ=
related schemes to approximate the advective flux and the central difference scheme for the diffusive flux. On non-rectangular
grids we recommend the VF9 scheme for the estimation of the diffusive flux. Our model exists as a code.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
134.
《Journal of Atmospheric & Ocean Science》2005,10(4):389-405
A wave forecasting system developed by Puertos del Estado (The Spanish holding of harbours) to predict waves at the coast is run in a twice a day cycle with a forecasting horizon of 72 h. This system is driven by wind fields supplied by the Spanish Meteorological Service from the HIRLAM model. Nested within this model a set of local forecasting systems, one for each harbour, covering an area of around 25 × 25 km, has been developed. The narrowness of the Spanish continental shelf requires very high resolution grids to be applied to localised regions near the coast. This fact involves the use of modelling techniques that makes this forecasting system different from other systems implemented in other regions. This article describes the wave forecasting system and the different techniques developed at Puertos del Estado to implement it. 相似文献
135.
利用钻井取心、薄片鉴定、粒度分析、古生物鉴定及测井解释等资料和手段,对济阳坳陷南部古近系孔一段到沙四段底部沉积特征进行研究.结果表明,济阳坳陷在孔一段至沙四段沉积早期处于湖盆裂陷初期,沉积作用明显受季节性洪水注入影响,在东营、惠民两凹陷形成洪水-漫湖沉积体系.其主要岩性特征为:岩石类型以反映氧化环境的浅色碎屑岩类为主,成熟度较低,粒度分布和沉积构造反映其兼有重力流和牵引流的沉积特点,植物碎屑贫乏而生物扰动构造丰富且具周期性,砂体呈环带状分布.该沉积体系分为洪水水道末端、泥坪、砂坪、砂泥混合坪和漫湖风暴等5个微相和侧缘远源、近岸远源两类相层序. 相似文献
136.
刘桥二矿在开采4煤过程中,七含突水次数达38次之多,严重影响煤矿安全生产。文章在系统地分析刘桥二矿七含涌突水概况的基础上,提出了该矿七含涌突水的主要机理为断裂构造的控制作用和矿山压力的促进作用;指出了砂岩含水层的裂隙发育程度和富水性强弱、煤层的厚度、断层的作用以及4煤与含水层之间隔水层厚度的大小等,是影响工作面涌水的主要因素。研究结果对煤矿砂岩水害的有效防治具有重要的指导意义。 相似文献
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