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Large-Scale Absolute Gravity Control in Brazil comparative measurements at absolute and relative stations, the instrument has been employed for absolute gravity control in fundamental and geodynamic networks in central and northern Europe. At approximately 100 gravity determinations at about 60 different stations an average station precision of

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Contribution of the Gravity Probe B Mission to Geodesy and to Satellite Navigationextremely important effects of Einstein’s general theory of relativity as observed with gyroscopes in Earth orbit. These are respectively the . exerted by a spinning body (the Earth) on an angular momentum vector (the set of gyroscopes), and the . resulting from the motion of the gyroscope in its or

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paleolithic

Gravity Field of Phobos and its Long Term Variationsobos boundary topography was established by Turner (197B), based on the Mariner 9 television pictures. Provided that Phobos is a homogeneous body, Sagitov et al. (1981), evaluated the Stokes parameters of the external gravitational field by numerical integration. An independent analytical approach b

半球

“Feldgrav” A Data Bank System for High Precision Gravity ObservationsPASCAL. A data logging system allows automatic data collecting within the data bank system. The software runs on IBM compatible portable Personal computers (PC). The ad hoc status of the system is described, whereby special emphasis is given to the adjustment procedure. Advantages of the system are

枯萎将要

Digital Compilation of Gravity Data Over the Japanese Islandshave many summits of 3,000 meters in elevation, comparable with the Alps. The length of the islands is about 2,000 km. The topographic relief is so great that roads are largely restricted to river courses, and large areas around high mountains remain difficult to access for gravity measurements.

Restenosis

Gravity Measurement on the Bottom of Toyama Trougha, 1983). The assumed boundary is located from Fossa Magna along the Toyama Trough, Sado Ridge, Okushiri Ridge towards the western egde of Okhotsk Sea (Fig.1). Some features of subducting slab, that is, thrust faulting, are observed by seismic profiling survey in several places along the line, (Naka

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