古鄱阳湖盆地东北缘白晋纪地层的新材料—兼论陆相地层清理后的问题讨论     

蔡雄飞  章泽军  王少锋 《江西地质》2001,15(1):45-49

古鄱阳湖盆地东北缘白垩系的田坂群历来趋向“二分”，但从对剖在再观察入手，认为田坂群纵向上经历了粗→细→粗的巨旋回，这种巨旋回与盆地演化规律，发展阶段相一致，因而“三分”显著，该剖面地学，9沉积学的一些新发现，不仅便于地层划分与对比，而且对盆内层序地层，岩相分析，构造演化阶段研究都具重要意义。  相似文献   

赣中变质岩带对该区铀成矿控制作用的研究     

胡恭任  刘丛强  余达淦  章邦桐  于瑞莲 《大地构造与成矿学》2001,25(3):296-301

本文从变质岩带的含铀性分析入手,研究了赣中变质岩带中铀矿化与变质岩带的含铀性、构造岩浆活动带、变质岩带出露的动力学机制及变质核杂岩构造的关系。研究表明:铀成矿与构造岩浆活动带以及地壳减薄、地幔上隆和在变质核杂岩边缘沿着低角度正断层的地壳伸展构造有着实质的关系。  相似文献   

River flow mass exponents with fractal channel networks and rainfall     

Brent M. Troutman  Thomas M. Over   《Advances in water resources》2001,24(9-10)

An important problem in hydrologic science is understanding how river flow is influenced by rainfall properties and drainage basin characteristics. In this paper we consider one approach, the use of mass exponents, in examining the relation of river flow to rainfall and the channel network, which provides the primary conduit for transport of water to the outlet in a large basin. Mass exponents, which characterize the power-law behavior of moments as a function of scale, are ideally suited for defining scaling behavior of processes that exhibit a high degree of variability or intermittency. The main result in this paper is an expression relating the mass exponent of flow resulting from an instantaneous burst of rainfall to the mass exponents of spatial rainfall and that of the network width function. Spatial rainfall is modeled as a random multiplicative cascade and the channel network as a recursive replacement tree; these fractal models reproduce certain types of self-similar behavior seen in actual rainfall and networks. It is shown that under these modeling assumptions the scaling behavior of flow mirrors that of rainfall if rainfall is highly variable in space, and on the other hand flow mirrors the structure of the network if rainfall is not so highly variable.  相似文献   

Mössbauer investigations and molecular orbital calculations on epidote     

M. Grodzicki  S. Heuss-Assbichler  G. Amthauer 《Physics and Chemistry of Minerals》2001,28(9):675-681

  相似文献   

Histological bone structure of Lower Cretaceous dinosaurs from southwest Istria (Croatia)     

Z. Kozari?  M. Šparica  Z. Bajraktarevi? 《Cretaceous Research》1996,17(6):741-749

Recently discovered dinosaur bones in submerged near-shore deposits of southwest Istria include one vertebra, one femur, and two rib fragments. They all show well-developed vascularization. The large amounts of primary bone tissue in the vertebral and femoral compacta as well as in one rib fragment suggest that they belong to sub-adult animals which were growing rapidly. The structure of a second rib fragment differs in that it consists of secondary bone. The absence of lines of arrested growth is evident in all investigated bones. This suggests a sustained manner of bone deposition.  相似文献   

Intracrystalline fractionation of Fe in synthetic (Fe, Mg, Zn) - bearing staurolite: a Mössbauer spectroscopic study     

M. Koch-Müller  I. Abs-Wurmbach  W. Bubenik 《Physics and Chemistry of Minerals》1999,26(4):312-321

⁵⁷Fe-Mössbauer spectra of eleven Fe-Mg-bearing staurolite samples, synthesized at 5, 20 and 25 kbar and 680°C, ranging in composition from x_Fe?=1.00 to x_Fe?=0.15, and of two Zn-Fe-bearing staurolite samples, synthesized at 20 kbar and 700°C with x_Fe?=0.10 and x_Fe?=0.32 were collected at room temperature. The spectra reveal that about 80% of Fe_tot (in case of Fe-Mg-bearing staurolite) and about 70% of Fe_tot (in case of Fe-Zn-bearing staurolite) are located as Fe²⁺ at the three subsites Fe1, Fe2 and Fe3 of the tetrahedral T2-site. The refinement of the spectra results in almost identical values for the isomer shift (IS) (±1.0 mm/s) but significantly different values for the quadropole splitting (QS) for the three subsites which is in accordance with the different distortions of these sites. About 8% of Fe_tot (in case of Fe-Mg-bearing staurolite) and 13% of Fe_tot (in case of Fe-Zn-bearing staurolite) are located as Fe²⁺ at the octahedral M4 site, while the remainder percents of Fe_tot indistinguishably occur as Fe²⁺ at the octahedral M1 and M2 sites of the kyanite-like part of the structure. Within the whole Fe-Mg-staurolite solid solution series the Mössbauer parameters QS of the sites M4 and (M1, M2) vary systematically with composition whereas IS remains constant. There is a high negative correlation of the total Mg-content with Fe-occupation of all the Fe-bearing sites indicating a continuous substitution of Fe²⁺ by Mg on all these sites. Synthetic Fe-staurolites show no increasing occupation of the octahedral sites by two-valent cations with pressure, as was assumed by several authors.  相似文献   

Modification Of The Standard ∈-Equation For The Stable Abl Through Enforced Consistency With Monin–Obukhov Similarity Theory     

Frank R. Freedman  Mark Z. Jacobson 《Boundary-Layer Meteorology》2003,106(3):383-410

A condition is derived for consistency of the standard-equation with Monin–Obukhov (MO) similarity theory of thestably-stratified surface layer. The condition is derivedby extending the procedure used to derive the analogous condition forneutral theory to stable stratification. It is shown that consistencywith MO theory requires a function of flux Richardson number, Ri_f, to be absorbed into either of two closure parameters, c ₁ or c ₂.Inconsistency, on the other hand, results if constant values of these are maintained for all Ri_f, as is done in standardapplication of the equation, and the large overpredictions ofturbulence found in such application to the one-dimensionalstable atmospheric boundary layer (1D-SBL) are traced to thisinconsistency. Guided by this, we formulate a MO-consistent-equation by absorbing the aforementioned function intoc ₁, and combine this with a Level-2.5 second-orderclosure model for vertical eddy viscosity and diffusivities.Numerical predictions of the 1D-SBL by the modified model converge to a quasi-steady state, rectifying the predictive failure of the standard -equation for the case.Quasi-steady predictions of non-dimensional variables agree stronglywith Nieuwstadt's theory. Qualitative accuracy of predictionsis inferred from comparisons to field data, large-eddy simulationresults and Rossby-number similarity relationships.  相似文献   

基于混沌时间序列的地下水位多步预测模型     

陈南祥  ;张海丰  ;李松海 《西安地质学院学报》2007,(1):66-69

利用相空间重构技术，并借助G—P算法、C-C方法和Wolf方法从宁陵地区地下水位一维时间序列中提取Lyapunov指数，结果表明此时间序列具有混沌特征。计算了宁陵地区地下水位时间序列的关联维数、时间延迟和最大Lyapunov指数，将局域加权一阶多步预测模型应用于地下水位预测。预测表明，此模型可有效应用于地下水位时间序列的多步预测。  相似文献   

Negotiating changing livelihoods: The sampan dwellers of Tam Giang Lagoon, Vi?t Nam     

Elsa DaCosta 《Geoforum》2007,38(1):190-206

Central Vi?t Nam is one of the most vulnerable areas in the country to natural disasters. In 1985 a major typhoon hit the Tam Giang Lagoon coastal area in the province of Th?a Tiên-Hu?, Central Vi?t Nam, with severe impacts on the sampan dwellers who lived there on boats and fished for their livelihoods. Since then, the government has attempted to resettle them on land in order to decrease their vulnerability to such events. Consequently, this process has changed the livelihood options as well as the social networks of the sampan dwellers. This study of the resettlement village of Th?y ?i?n analyses the social networks and different forms of social capital being utilised by the resettled sampan dwellers as part of their changing livelihoods and questions whether the social capital formed will indeed lead to a long term decrease in vulnerability. It is found that while bonding and linking social capital have been newly formed, the trust required for bridging social capital formation is still missing, and this in turn is hindering the possibilities of sustainable livelihood formation.  相似文献   

刚性桩复合地基垫层对桩土应力比影响分析     

尚琴琴  战永亮 《岩土工程技术》2007,21(1):32-35

从极限平衡理论角度对刚性桩复合地基中垫层作用机理进行分析,提出桩顶垫层厚度、垫层材料内摩擦角等参数对桩土应力分担的控制公式,推导出在已知表面应力情况下考虑桩土共同作用的桩土沉降计算公式,在此基础上提出一种桩土应力比的迭代计算方法。编制程序实现对算例的计算,总结分析计算结果并与实测值进行对比验证。  相似文献