Abstract
Measurements of surface displacements using GPS constrain the motion and deformation of India and India-Eurasia plate boundary deformation along the Himalaya. The GPS velocities of plate-interior sites constrain the pole of the angular velocity vector of India with respect to Eurasia to lie at 25.6 ± 1.0° N 11.1 ± 9.0° E, approximately 6° west of the NUVEL-1A pole of < 3 Ma plate motion. The angular rotation rate of 0.44 ± 0.03° Myr-1 is 14% slower than the long-term rate of 0.51° Myr-1. Insignificant velocities between plate interior sites indicate that the exposed Indian plate is stable to within 7 · 10-9 yr1. The observed contraction vector across the Himalaya (≤ 20 mm/yr) veers from ~N20°E in the northwest Himalaya to ~N25°W in east Nepal, consistent with east-west extension of southern Tibet.
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CITATION STYLE
Paul, J., Bürgmann, R., Gaur, V. K., Bilham, R., Larson, K. M., Ananda, M. B., … Kumar, D. (2001). The motion and active deformation of India. Geophysical Research Letters, 28(4), 647–650. https://doi.org/10.1029/2000GL011832
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