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11.
用改进的数学公式,便于用单钻孔资料和岩层复平求面理倾斜、求岩层厚度、求地层断距等多个课题。 相似文献
12.
天然叶蜡石及其热处理产物的电子顺磁共振(EPR)研究 总被引:7,自引:2,他引:7
利用EPR研究了18个天然叶蜡石样及其4个热处理产物。发现天然叶蜡石有三个EPR吸收带:A(g有效≈11.4),B(g有效≈4.3)和C(g有效≈2.0),其中A是叶蜡石的特征谱。A在>400℃热处理时与B在强度上呈消长关系;<400℃热处理时A和B均随温度升高而加强;900℃时A消失,B的强度远远大于原样中的A;C附有超精细结构谱(g″=2.04,g┴=1.96,A″≈A┴=19.5×10^-4T),C在热处理时呈现复杂的变化。结果表明,A吸收带属于叶蜡石八面体AI(Fe)-O4(OH)2中的Fe^3 ,B吸收带归于八面体AI(Fe)-O2(OH)4中的Fe^3 ,C吸收带是无机自由基(如AI-O^-Si)和有机自由基的叠加谱;900℃热处理后八面体层中配位发生了变化:AI(Fe)-O4(OH2)→AI(Fe)-O5 H2O↑,AI(Fe)-O2(OH)4→AI(Fe)-O4 H2O↑;类质同象置换AI^3 的不仅有Fe^3 ,而且有Fe^2 离子。 相似文献
13.
14.
通过对广东西部沿海高速公路路面基层现场压实度检测过程的详细观察,并在不同的条件下反复进行试验、分析比较,找出了影响压实度现场检测精度的主要非理想因素,即标准砂密度、试样含水量和路面基层平整度,并提出了解决方法。 相似文献
15.
华南地区栖霞组菊花状天青石的交代及其地质意义 总被引:4,自引:0,他引:4
本文在收集大量菊花石标本的基础上,通过岩石薄片镜下鉴定及X射线衍射分析,识别了华南地区栖霞组菊花石假象内矿物的成因类型,建立了矿物交代序列,并通过对菊花石假象内各种矿物成分的电子探针分析和对交代方解石,脉方解石及其围岩的氧,碳同位素分析,探讨了菊花石交代过程中的成岩环境,合理地解释了菊花石内正延性玉髓和栖霞组内海泡石的成因。 相似文献
16.
钠长石岩分布不太广泛 ,研究程度较低。通过研究 ,本文将钠长石岩分为接触带型、层状型、顺层角砾岩型、脉型及岩体型 5类。其中以层状钠长石岩型分布较广 ,意义较大。层状及与之紧密相伴的顺层角砾状钠长石岩有特定的矿物组合、化学成分及岩石组合 ,层状及角砾状钠长石岩产在一定的地层层位中 ,形成于特殊的沉积环境 ,且有一定的时空分布规律 ,并伴有特殊的 Au,Cu,Pt- Zn- Ag,Ba,Fe,B等矿产。因此笔者认为钠长石岩系特定地质条件下的产物。目前对其成因有岩浆岩、热液交代 +充填、热水沉积等不同认识 ;热水来源也有岩浆水、地下水、变质水等多种观点。本文作者认为层状及角砾状钠长石岩为热水沉积形成的 ,成岩流体属含 Na- Mg- Si- Al± Fe,Ba,B的 HCO3- ,CO32 - 碱性溶液 ,成岩物质来自基底富钠岩石。 相似文献
17.
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
18.
Plagioclase replacement textures in partially eclogitised gabbros from the Sanddal mafic-ultramafic complex, Greenland Caledonides 总被引:1,自引:0,他引:1
The Sanddal mafic‐ultramafic complex (SMUK) is a cluster of variably eclogitised mafic and ultramafic bodies that comprise the westernmost known eclogite facies locality in the North‐East Greenland eclogite province (NEGEP). Although there are no true eclogites in the SMUK, we interpret three distinct textural types of plagioclase replacement to record sequential stages in adjustment of SMUK olivine gabbro‐norites to eclogite facies conditions. The earliest stage, in which plagioclase was replaced by omphacite/spinel symplectite before nucleation of garnet (Type 1A & 1B) has not previously been described. Documentation of this texture provides clear evidence that, at least in some cases, garnet nucleation is delayed relative to nucleation of omphacite and is a rate‐limiting step for eclogitisation. Type 1C domains were produced by scattered nucleation of garnet in the same sample. In Type 2 domains, plagioclase was replaced by a layered corona with an outer layer of garnet, an inner layer of omphacite and an interior of inclusion‐rich plagioclase. In Type 3 domains, the omphacite layer was overgrown by the garnet rim, and omphacite is preserved only as inclusions in garnet. In more coarse grained leucogabbros, recrystallization was more complete, plagioclase replacement textures were less localised, and could not be divided into distinct stages. Plagioclase replacement in SMUK samples was not isochemical, and required diffusion of at least Mg and Fe from replacement of mafic phases in the surroundings. Strong compositional gradients in garnet reflect disequilibrium and were controlled by the different diffusion rates of Mg/Fe and Ca, different local chemical environments, and progress of the plagioclase breakdown reaction. The presence of small amounts of hydrous minerals (amphibole, phlogopite and clinozoisite) in local equilibrium in plagioclase domains of most SMUK samples indicates that a small amount of H2O was present during high pressure metamorphism. 相似文献
19.
Oliver Wild Oliver V. Rattigan Roderic L. Jones John A. Pyle R. Anthony Cox 《Journal of Atmospheric Chemistry》1996,25(2):167-199
The Cambridge 2-D Eulerian model has been used to study the potential atmospheric distributions and lifetimes of a number of CFC replacement compounds and their degradation products. The study has focused on HFC 134a and HCFCs 123, 141b and 142b and the major products formed by their atmospheric degradation. The loss of these compounds and their products by hydroxyl radical attack, photolysis and in-cloud hydrolysis have been investigated. The study has shown that HCFCs 141b and 142b have sufficiently long lifetimes to enter the stratosphere in significant quantities, where degradation leads to an increase in the total stratospheric chlorine concentration. The study has also highlighted areas where further experimental work would be valuable, in particular characterisation of the product channels for the degradation reactions and determination of the removal rates of the products in the aqueous phase. 相似文献
20.
对L波段探空系统在使用过程中出现近地层斜距因受地物回波影响而失真的情况,探讨软件所提供代替方法的合理性。 相似文献