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991.
滇西石鼓变质带基本特征 总被引:4,自引:1,他引:4
石鼓变质带延伸约100多公里,可划分为绿泥石带、黑云母带、铁铝榴石带、十字石带、蓝晶石带及夕线石带。红柱石-蓝晶石稳定共生,属低—中压变质相系的区域变质带。主要变质时期为海西晚期(K-Ar年龄为258Ma)。 相似文献
992.
庐山东南麓冰川作用表皮构造特征及其意义 总被引:4,自引:1,他引:4
庐山东南麓第六阶地基座上,发现了早更新世冰川作用表皮构造。按其形态与成因可分为巨砾压入基岩、小型倒转构造与不协调褶皱、逆冲-贯入构造、大型片麻岩包裹体等四种类型。早更新世初期之庐山,确实多次发生过山麓冰川作用。 相似文献
993.
M. H. Shapiro A. Rice M. H. Mendenhall J. D. Melvin T. A. Tombrello 《Pure and Applied Geophysics》1984,122(2-4):309-326
Four techniques (pattern recognition, Fourier transformation, cross-correlation, and multiple linear regression) have been used to recognize nontectonic environmental factors affecting groundwater radon data collected by the Caltech automated geochemical network. Several factors, including air temperature, rainfall, water level, carbon dioxide concentration in the water, and barometric pressure, were found to correlate with radon level at some stations in the network. For example, approximately 60% of the variance in radon signal at one site studied (Pacoima) could be accounted for by nontectonic influences. However, it was not possible to correlate all the observed changes in radon concentration with nontectonic environmental variables. Some of the observed radon anomalies did appear to be related to either regional changes in tectonic strain or some individual earthquakes. A model is developed to account for spike-like increases in radon caused by carbon dioxide emission. 相似文献
994.
A well-known but rarely used powerful method to investigate the presence of harmonic signals in time series is the Phasor Walkout method (other names are: Graphical Fourier Transform, Summation Dial, Complex Demodulation). At a given test frequency the complex contributions (phasors) to the Fourier Transform of each sample in an equidistantly sampled series are added vectorially in the complex plane. The resulting pattern, the walkout, reveals information about the properties of the signal which is not easy to obtain by other methods. Synthetic examples are used to demonstrate the resolving power of the method. The following geophysical examples for the application of this method are shown: determination of the frequency of the breathing mode0
S
0 of the earth after a large earthquake; the study of superconducting gravimeter records after a large deep earthquake used in the core mode interpretation of a spectral peak, the study of the residualS
3 (8 h period) signal in a tidal record and the bichromatic Rayleigh-waves from Mount Pinatubo on June 15, 1991. 相似文献
995.
Because multidimensional ARMA processes have great potential for the simulation of geological parameters such as aquifer permeability, it was important to resolve which of two proposed alternative methods should be used for determining the two-dimensional weighting parameter, , for a unilateral ARMA (1, 0) process on a square net. Practical simulations demonstrates that the correct formulation is: =10/(1+
10
2
where r,s is the correlation between lattice points at lagsr and s. When the simulations are performed with correlations of 0.8 or more a residual bias was detected which was found to be caused by a difference in the variance between the one- and two-dimensional models. This can be rectified by modifying the two- dimensional model as follows: zij=(zi–1, j + zi, j–1) + aij where
2=1/(1 +
10
2
). 相似文献
996.
997.
Li Shengrong Key Laboratory of Lithospheric Tectonics Lithoprobing Technology China University of Geosciences Ministry of Education Beijing China Gao Zhenmin Institute of Geochemistry Chinese Academy of Sciences Guiyang China Shen Junfeng Key Laboratory of Lithospheric Tectonics Lithoprobing Technology China University of Geosciences Ministry of Education Beijing China 《中国地质大学学报(英文版)》2004,15(1):84-90
INTRODUCTIONPlatinum group element (PGE)oredepositsofmag maticliquationoriginwereidentifiedtobethemaintype ,oreventheonlytypeofPGEoredeposits .Theorebodiesoc curdirectlyintheultramafic maficigneousrocksorthecon tactzonebetweentheigneousrocksandtheirwall rocks .Theformingtemperatureofthedepositswasabout 4 0 0 - 5 0 0℃orevenhigher.Foralongtime ,therefore ,ithadbeenconsideredthattheenrichment,mineralizationandtransfer enceofPGEcouldonlyoccurinultramafic maficigneousrocksathightemperature… 相似文献
998.
长江中下游地区早白垩世埃达克质岩的大地构造背景及其成矿意义 总被引:28,自引:22,他引:28
长江中下游地区是中国重要的铜资源基地之一。该成矿带广泛发育与Cu-Au成矿作用密切相关的早白垩世火成岩。大多数与成矿有关的中酸性侵入岩具有类似埃达克岩的地球化学特征,即富集Sr而贫HREE(如:Y和Yb);但它们具有负的εNd(t)值和相对富集的Sr同位素初始比值(>0.704.),因此,被称为埃达克质岩。根据岩石化学数据,研究区埃达克质侵入岩多数属于高钾钙碱性系列,部分属于钙碱性系列;而火山岩和A型花岗岩类由于其高钾和富铁特征而属于钾质碱性系列。岩石地球化学资料显示,与成矿作用有关的中酸性埃达克质侵入岩经历了复杂的成岩过程,至少包括在深位岩浆房(>35~40 km深度)的分离结晶和在高位岩浆房内的分离结晶或AFC过程两个阶段。同时不排除有下地壳直接熔融形成的埃达克质熔体参与的可能性。富钾的火山岩则是原生岩浆在深位岩浆房(>40-50 km深度)经镁铁矿物的分离结晶过程演化而来。基于长江中下游地区及其邻区的区域地质构造、早白垩世岩浆岩的岩石化学和地球化学特征和岩浆活动的时空演变特征的综合分析,推测该成矿带在早白垩世早期处于大陆边缘岩浆弧内陆一侧,岩浆活动与古太平洋板块的斜向俯冲作用有关;晚期由于俯冲板片迁移(变陡),岩浆岩具有弧后环境特征。俯冲板片上部所释放的超临界流体提高了地幔 相似文献
999.
Nathaniel Bensoussan Jean-Claude Romano Bouazza El-Haikali Michel-Guy Lafont 《Comptes Rendus Geoscience》2004,336(10):909-918
Semi-continuous (1/30 min) records of physicochemical parameters (T,S, DO and pH) have been measured at 1.50 m in Mediterranean coastal waters (Marseilles) from 1998 to 2000, together with meteorological parameters. Physicochemical data were studied in order to synthesise the information at different time scales (inter-annual, season, day, hour), particularly the semi-conservative DO and pH response to hydroclimatic variables. At a daily time scale, important circadian dynamic has been measured under all circumstances with a strong reactivity to irradiance change under the influence of biological activity. This work may contribute to the definition of new tools for coastal waters observation. To cite this article: N. Bensoussan et al., C. R. Geoscience 336 (2004). 相似文献
1000.