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==Abstract==
==Abstract==


Space-geodetic techniques, such as satellite laser ranging (SLR), very long baseline interferometry (VLBI), and the Global Positioning System (GPS), provide valuable data on the relative motion between sites on the earth?s surface up to 12,000 km apart. Measurements to date are said to be in generally good agreement with the motions predicted by plate tectonics, and are widely regarded as having confirmed seafloor spreading, subduction, and continental drift.[[Category:Scientific Paper]]
Space-geodetic techniques, such as satellite laser ranging (SLR), very long baseline interferometry (VLBI), and the Global Positioning System (GPS), provide valuable data on the relative motion between sites on the earth?s surface up to 12,000 km apart. Measurements to date are said to be in generally good agreement with the motions predicted by plate tectonics, and are widely regarded as having confirmed seafloor spreading, subduction, and continental drift.
 
[[Category:Scientific Paper|problems with plate tectonics]]


[[Category:Relativity]]
[[Category:Relativity]]

Revision as of 12:56, 1 January 2017

Scientific Paper
TitleProblems with Plate Tectonics
Author(s)David Pratt
Keywords{{{keywords}}}
Published2001
JournalNew Concepts in Global Tectonics Newsletter
Number21
Pages10-24

Abstract

Space-geodetic techniques, such as satellite laser ranging (SLR), very long baseline interferometry (VLBI), and the Global Positioning System (GPS), provide valuable data on the relative motion between sites on the earth?s surface up to 12,000 km apart. Measurements to date are said to be in generally good agreement with the motions predicted by plate tectonics, and are widely regarded as having confirmed seafloor spreading, subduction, and continental drift.