Titlebook: Global and Regional Geodynamics; Symposium No. 101 Ed P. Vyskocil,C. Reigber,P. A. Cross Conference proceedings 1990 Springer Science+Busin

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書目名稱Global and Regional Geodynamics影響因子(影響力)




書目名稱Global and Regional Geodynamics影響因子(影響力)學(xué)科排名




書目名稱Global and Regional Geodynamics網(wǎng)絡(luò)公開度




書目名稱Global and Regional Geodynamics網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Global and Regional Geodynamics被引頻次




書目名稱Global and Regional Geodynamics被引頻次學(xué)科排名




書目名稱Global and Regional Geodynamics年度引用




書目名稱Global and Regional Geodynamics年度引用學(xué)科排名




書目名稱Global and Regional Geodynamics讀者反饋




書目名稱Global and Regional Geodynamics讀者反饋學(xué)科排名

LIEN

Plate Motions Derived from the DGFI 89 L03 Solution. The full set of 19708 data passes in that period was carefully screened and compressed into two-minute normal points. This compressed data information was used to simultaneously estimate orbital parameters, a few dynamic model corrections, five-day Earth rotation parameters, geocentric station coo

Fecundity

Plate Motions and Deformation from Lageosive geodetic parameter solution. Some of the stations in the participating network have a continuous tracking record over the full LAGEOS mission lifetime and can be used to monitor positions in a limited network for over 12 years. However, the introduction of several new stations of improved precis

歌劇等

Global Plate Motion Parameters Derived from Actual Space Geodetic Observationsfts. These data are interpreted as plate tectonic motions, and they are used to derive uniform plate rotation vectors. We use four different data sets: VLBI station coordinate shifts, VLBI baseline changes, and SLR baseline changes (all evaluated by NASA GSFC) , as well as SLR coordinate shifts from

送秋波

A Qualitative and Quantitative Comparison of Geodetic Results from SLR and VLBIsame, locations on the surface of the Earth. Two of the commonly used geologic models which describe the plate geodesic rates between locations on the Earth’s surface are the AMO-2 and the NUVEL-1..Qualitative results indicate that both the SLR and VLBI measure motion between Monument Peak and Quinc

Redundant

Geodynamic Research Using Lageos Laser Ranging Data at the Central Institute for Physics of the Earttectonic deformations, tidal deformation (LOVE numbers h. and l.), ocean tides resp, frequency-dependent LOVE number k. tailored gravity field modelling based on point masses, post-glacial rebound modelling by point masses changing with time.

Redundant

Constitution

The Effect of Model Errors on Laser Ranging Residualsuals of an orbital adjustment of Lageos laser ranging data were analyzed, and covariance and crosscovariance functions estimated and compared with the results of the preceding theoretical analysis, in order to get some insight about the physical mechanism responsible for the signal.

LEVY

Design of African Plate SLR/VLBI Network for Geodynamics and Earthquake Researchordinates of widely spaced network points. Repeated determinations of the network point coordinates enable the determination of spatial crustal movements as a tool for geodynamics and earthquake research. The Mediterranean forms the boundary zone where the African, Arabian and Eurasian tectonic plat

rectum

Displacement of a Japanese VLBI Station as an Indicator of the Island Arc ContractionLBI) station is located on the “outer arc”, that is, between the volcanic front and the Japan trench. The existence of many active faults in intraplate Japan suggests complicated crustal deformation making Kashima station somewhat unsuitable for the measurement of the tectonic plate motion itself. F