dc.contributor.author | Neetu, S. | |
dc.contributor.author | Suresh, I. | |
dc.contributor.author | Shankar, R. | |
dc.contributor.author | Shankar, D. | |
dc.contributor.author | Shenoi, S.S.C. | |
dc.contributor.author | Shetye, S.R. | |
dc.contributor.author | Sundar, D. | |
dc.contributor.author | Nagarajan, B. | |
dc.date.accessioned | 2006-05-12T11:43:35Z | |
dc.date.available | 2006-05-12T11:43:35Z | |
dc.date.issued | 2005 | |
dc.identifier.citation | Science, vol. 310(5753), 1431a | |
dc.identifier.uri | http://www.sciencemag.org/content/vol310/issue5753/index.dtl | |
dc.identifier.uri | http://drs.nio.org/drs/handle/2264/102 | |
dc.description.abstract | Lay et al. (Special Section, 20 May 2005, p.1127) estimated a 600-km length for the tsunami source region. Adding tide-gauge data from Paradip, the northernmost of the Indian east-coast stations and therefore the most critical constraint on the northern extent of the source, we estimate that its length was greater by ~30%. | |
dc.format.extent | 122705 bytes | |
dc.format.mimetype | application/pdf | |
dc.language.iso | en | |
dc.publisher | American Association for the Advancement of Science | |
dc.subject | Tsunami | |
dc.subject | Source | |
dc.subject | Ray Tracing | |
dc.subject | Indian Ocean | |
dc.subject | Sumatra Earthquake | |
dc.subject | Tide Gauge | |
dc.title | Comment on "The Great Sumatra-Andaman Earthquake of 26 December 2004" | |
dc.type | Journal Article | |