NASA NTRS · 19810018959
Time and frequency stability for the Crustal Dynamics Project
Abstract
Very long base interferometry (VLBI) and laser ranging to artificial satellites and the Moon were used to determined vector baselines between stations with precisions of about one part in 10 to the 8th power. Deformations and strain accumulations in active earthquake regions were determined by making frequent measurements of baselines between many stations in active areas near plate boundaries.
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Coates, R. J., Ryan, J., Herring, T.. 1981-03-01. Time and frequency stability for the Crustal Dynamics Project. https://ntrs.nasa.gov/citations/19810018959
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