- Abstract:
-
Average a priori shear velocity models are constructed for the Tien Shan, Tarim basin, Pamir-Hindu Kush, Himalaya and NE India. These models are shown to account for most of the lateral velocity heterogeneity at wavelengths > 1000 km. Interevent fundamental mode Rayleigh and Love wave phase velocities were measured in the period range 32-200 s and were inverted for path-averaged shear velocity structures. These, in turn, were regionalized to estimate average, isotropic structures beneath t...
Expand abstract - Publication status:
- Published
- Publisher copy:
- 10.1029/96JB03182
-
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- Journal:
- JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
- Volume:
- 102
- Issue:
- B6
- Pages:
- 11789-11813
- Publication date:
- 1997-06-10
- DOI:
- ISSN:
-
2169-9313
- URN:
-
uuid:486bd1d2-8f7d-4301-bbb9-89890c39d34f
- Source identifiers:
-
166339
- Local pid:
- pubs:166339
- Copyright date:
- 1997
Journal article
Crust and upper mantle shear velocity structure beneath the Tibetan plateau and surrounding regions from interevent surface wave phase velocity inversion
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