沂沭带形变、重磁场时空变化特征与地震活动   总被引：3，自引：0，他引：3  

燕乃玲  潘纪顺  郭玉莲  李建奎  唐廷梅 《地震研究》2001,24(2):126-130

综合利用流动水准和流动重磁复测资料,分析沂沭断裂带上地壳形变场和地球物理场的时空强变化特征,揭示沂沭断裂带活动特征是以鲁中隆起的继承性活动为主,沂沭带北端的双山-李家庄断裂两盘的垂直形变受区域断裂控制并与区域地震活动有关,与1983年荷泽地震和1995年苍山地震有较好对应关系;沂水附近地磁场有“窗口效应”,尤其与南黄海地震活动及沂沐断裂带上的小震活动有关。  相似文献   

Pulsar activity and the morphology of supernova remnants     

V. Radhakrishnan  G. Srinivasan 《Journal of Astrophysics and Astronomy》1980,1(1):25-32

We use the recently introduced concept of a ‘window’ of magnetic field strengths in which pulsars can be active to explain the variation in morphology of supernova remnants. The striking difference between shell-type and filled-type remnants is attributed to differences in he magnetic field strengths of the neutron stars left by the respective Supernovae. Field strengths of a value permitting pulsar activity result in particle production and Crab-like centrally concentrated remnants. Other field values lead to strong magnetic dipole radiation and consequent shell formation (e.g. Cas A). Several apparent inconsistencies concerning pulsar-supernova associations appear to find a logical explanation on the basis of this hypothesis.  相似文献   

霍山"震情窗"地区流动地磁S异常与华东中强地震相关性的研究   总被引：1，自引：0，他引：1  

刘义高  郑志坤  翟义勇  张毅 《华北地震科学》2002,20(4):34-39

以霍山“震情窗”地区流动地磁测线的S值变化,预测霍山“震情窗”相关地区－华东地区中强地震,研究结果表明：“震情窗”地区流动地磁测线的S值异常与距离霍山“震情窗”R＜500km的华东中强地震有明显的相关性。  相似文献   

Numerical Simulation of the High-Latitude Non-Stationary Ionospheric Alfvén Resonator During an IPDP Event     

Prikner  K.  Mursula  K.  Kangas  J.  Feygin  F. Z.  Kerttula  R. 《Studia Geophysica et Geodaetica》2002,46(3):507-526

The ionospheric Alfvén resonator (IAR) was numerically simulated under non-stationary ionospheric and magnetospheric conditions of the IPDP event of December 4, 1986. The full numerical wave method was applied using height profiles of the ionospheric plasma parameters obtained from the Scandinavian EISCAT radar measurements close to the Ivalo latitude. An attempt to model the inverse problem of numerical simulation—prolongation of the electron density profiles at altitudes above the ionospheric F layer—was made on the basis of the IAR simulation in correlation with the IPDP frequency increase. The change of the IAR wave characteristics during the substorm was illustrated by height profiles of the total wave amplitude and various polarization characteristics, taking into consideration the ordinary L-mode and the extraordinary R-mode waves for parallel and non-parallel incidence with respect to the magnetic field line.  相似文献   

Stratospheric N2O5, CH4, and N2O profiles from IR solar occultation spectra     

C. Camy-Peyret  J. -M. Flaud  A. Perrin  C. P. Rinsland  A. Goldman  F. J. Murcray 《Journal of Atmospheric Chemistry》1993,16(1):31-40

Stratospheric volume mixing ratio profiles of N₂O₅, CH₄, and N₂O have been retrieved from a set of 0.052 cm^–1 resolution (FWHM) solar occultation spectra recorded at sunrise during a balloon flight from Aire sur l'Adour, France (44° N latitude) on 12 October 1990. The N₂O₅ results have been derived from measurements of the integrated absorption by the 1246 cm^–1 band. Assuming a total intensity of 4.32×10^–17 cm^–1/molecule cm^–2 independent of temperature, the retrieved N₂O₅ volume mixing ratios in ppbv (parts per billion by volume, 10^–9), interpolated to 2 km height spacings, are 1.64±0.49 at 37.5 km, 1.92±0.56 at 35.5 km, 2.06±0.47 at 33.5 km, 1.95±0.42 at 31.5 km, 1.60±0.33 at 29.5 km, 1.26±0.28 at 27.5 km, and 0.85±0.20 at 25.5 km. Error bars indicate the estimated 1- uncertainty including the error in the total band intensity (±20% has been assumed). The retrieved profiles are compared with previous measurements and photochemical model results.Laboratoire associé aux Universités Pierre et Marie Curie et Paris Sud.  相似文献   

Detection of Cyclic Patterns Using Wavelets: An Example Study in the Ormskirk Sandstone, Irish Sea     

Nestor A. Rivera  S. Ray  Jerry L. Jensen  Andrew K. Chan  Walter B. Ayers 《Mathematical Geology》2004,36(5):529-543

This study shows how wavelet analysis can be used on well log and drill core data to identify cyclicity in sedimentary sequences. Three possible methods for determining wavelength were investigated: the Morlet wavelet, the Fourier transform, and the semivariogram. When applied to several hypothetical signals similar to those observed in petrophysical measurements in hydrocarbon reservoirs, all three methods could identify the presence of cyclicity. Only the wavelet scalogram, however, gave a clear indication of when the cyclic element was present and where frequency changes occurred in the signal. To illustrate the wavelet analysis, we processed well log and core data from a well in the Ormskirk Sandstone and determined the wavelet coefficients for each zone and the wavelengths of the strongest cyclicities. The cyclicities observed corresponded well with sedimentary features of the formation (e.g., channels and channel sets). Also, ratios of the cyclicity wavelengths corresponded with ratios of the Milankovitch precession, obliquity, and eccentricity periods. This result is in agreement with other investigators, who have proposed that Milankovitch-driven climate changes exercised an important control on Ormskirk Sandstone deposition.  相似文献   

Interpretation of the short period variations in geomagnetic anomalies of Shaanxi region     

范国华  姚同起  韩克礼 《地震学报(英文版)》1999,12(6):684-689

1BriefintroductionoftheanomaliesofshortperiodgeomagneticvariationsinShaanxiAtemporarymeasurementprofilecomposedofmeasurementsitesofShiquan,Foping,Banfangzi,Zhouzhi,Wugong,Qianling,BinxianandNingxian,whichisbasicalalongnorth-southdirectionfromShiquaninthesouthernpartofShaanxitoNingxianinGansu,wassetupandsimultaneousobservationofthree-componentgeomagneticshortperiodvariationswereperformedateightsitesduringSeptemberof1996.Observationalresultsshowthatthereisareversalaxisofgeomagneticverticalv…  相似文献   

广义Radon变换的正交展开和反演     

王金平 《CT理论与应用研究》1999,8(4):14-19

本文具体给出了广义Ｒａｄｏｎ变换在函数空间Ｌ＾２（Ｒ＾ｎ,Ｗｎ）上的正交函数展开形式,由此得到了广义Ｒａｄｏｎ变换的反演公式,从而推广了Ｌｏｕｉｓ和Ｄａｖｉｓｏｎ的工作。  相似文献   

A migration model of magmatism explaining a ridge subduction, and its details on a statistical analysis of the granite ages in Cretaceous Southwest Japan     

Osamu Kinoshita 《Island Arc》1999,8(2):181-189

A migration model of magmatism based on the granite ages in Southwest Japan is proposed to explain the ridge subduction beneath the Eurasia continent as the cause of the along-arc and across-arc youngings of the granite ages and the very high activity of the magmatism in the Cretaceous. For the construction of the magmatic model, the localities of the granite age samples are denoted by the cartesian coordinates X and Y, which are measured along and normal to the Median Tectonic Line (MTL), respectively, and their ages are set corresponding to the coordinate Z vertical to the X–Y plane. The age trend is then formulated by a regression plane of Z on X and Y, which inclines in both directions along and normal to the MTL, and approximates the ages with the very high multiple correlation coefficient 0.91. Evaluating the magmatic trend by such a method, various characteristics of the activities can be taken easily; for example, the isochronous line of the magmatism, which is an intersection of the regression plane and an arbitrary horizontal plane, is found to extend landward obliquely across the continental margin. The migrating rate of the isochronous line along the MTL is also taken to be 2.8 cm/year as a reciprocal of the inclination of the along-arc younging. The isochronous line is speculated to be the out-cropped manifestation of the subcrustal linear heat source. Such a migrating linear heat source is probably due to the subduction of an active ridge, the Kula (or Izanagi)–Pacific ridge in the Cretaceous. The migration model of magmatism harmonizes very well with the plates and the ridge motions in the East Asia area during the late Mesozoic. The ridge subduction is one of the important phenomena that explain the unusually active arc magmatism and the migrating slab window; it is important to grasp dynamically the geological messages issued from the system.  相似文献   

TROPICAL SEA SURFACE TEMPERATURE ANOMALY AND INDIAN SUMMER MONSOON^*          下载免费PDF全文

Zhu Yafen  Qian Weihong  Ye Qian 《Acta Meteorologica Sinica》1999,13(2):154-163

The time series of the sea surface temperature(SST) anomaly,covering the eastern (western) equatorial Pacific,central Indian Ocean,Arabian Sea.Bay of Bengal and South China Sea(SCS),have been analyzed by using wavelet transform.Results show that there exists same interdeeadal variability of SST in the tropical Pacific and tropical Indian Ocean,and also show that the last decadal abrupt change occurred in the 1970s.On the interannual time scale,there is a similar interannual variability among the equatorial central Indian Ocean and the adjacent three sea basins(Arabian Sea.Bay of Bengal and South China Sea).but the SST interannual changes of the Indian Ocean lagged 4-5 months behind that of the equatorial central-east Pacific.Meanwhile,the interannual variability and long-range change between SST anomaly and Indian summer monsoon rainfall in recent decades have been explained and analyzed.It indicates that there existed a wet(dry) period in India when the tropical SST was lower(higher)than normal,but there was a lag of phase between them.  相似文献