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Mode of the strain release along the Gibbs fracture zone, Mid-Atlantic ridge

Kanamori, Hiroo and Stewart, Gordon S. (1976) Mode of the strain release along the Gibbs fracture zone, Mid-Atlantic ridge. Physics of the Earth and Planetary Interiors, 11 (4). pp. 312-332. ISSN 0031-9201. https://resolver.caltech.edu/CaltechAUTHORS:20150218-073106036

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Abstract

The Gibbs fracture zone (52°N, 35°W) is one of the major transform faults in the Atlantic. A large earthquake (m_b = 5.8, M_s = 6.9) occurred on October 16, 1974 on this fracture zone. This earthquake was preceded by similar large earthquakes along the fracture zone in 1967 (m_b = 5.5, M_s = 6.5), 1954 (M_s = 6.5), 1941 (M_s = 6.25) a 1923 (M_s = 6.5). Detailed analyses of seismic body waves and surface waves over the period range from several seconds to 200 sec are made for the 1967 and 1974 events. The major conclusions are: (1)|In addition to the obvious disparity in the m_b vs. M_s relation, the excitation of long-period waves by these earthquakes is also anomalously large. The seismic moments determined by using the long-period (40–200 sec) G_1 and R_1 waves are 3.4 · 10^(26) and 4.5 · 10^(26) dyne · cm for the 1967 and 1974 events, respectively. (2)|Wave form analyses of body waves suggest a fault length of 60 km for the 1967 event and 70 km for the 1974 event. The point dislocation particle velocity of about 20 cm/sec obtained for both events is about an order of magnitude smaller than for other earthquakes of comparable magnitude. The large fault length and the slow particle velocity explain the disparity between m_b and M_s, and Ms and seismic moment. (3)|The amount of dislocation (about 170 cm) together with the fault length and the repeat time (13 years on the average) suggest a seismic slip rate of about 2.6 cm/year along the Gibbs fracture zone — a rate which is comparable to that for sea-floor spreading in the northern Atlantic. This agreement suggests that the slip along the fracture zone is primarily seismic at least to a depth of 10 km, the plates moving in jerks once every 13 years on the average, rather than in continuous creep. (4)|Seismic activity along the ridge crest was very high during the 5-year period before the 1974 event, while activity along the fracture zone was very high during the 3-year period prior to the 1967 event. The seismic activity became very low after the 1967 event. This pattern may be interpreted in terms of an intermittent upwelling at the ridge which subsequently triggered, either directly or indirectly, the fracture zone events. The sudden release of stress in these events may lead to an initiation of the next episode of upwelling and eventually renewed seismic activity along the ridge—fracture zone system.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/0031-9201(76)90018-2DOIArticle
http://www.sciencedirect.com/science/article/pii/0031920176900182PublisherArticle
ORCID:
AuthorORCID
Kanamori, Hiroo0000-0001-8219-9428
Additional Information:© 1976 Published by Elsevier B.V. Received 25 November 1975, Accepted 16 December 1975, Available online 16 October 2002. Contribution No. 2683, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, U.S.A. We would like to thank all the WWSSN stations that were kind enough to send us seismograms for the October 1974 event. Useful discussions with Sean Solomon are acknowledged and Charles Langston is thanked for the use of his P- and S-wave synthetic computer programs. We are especially grateful to the National Geographic Society, Washington, D.C., for allowing us to publish Fig. 1. This research was supported by the Advanced Research Projects Agency of the Department of Defense and was monitored by the Air Force Office of Scientific Research under Contract No. F44620-72-C-0078 and National Science Foundation Grants GA 38715 and DES 74-22489.
Funders:
Funding AgencyGrant Number
Advanced Research Projects Agency (ARPA)UNSPECIFIED
Air Force Office of Scientific Research (AFOSR)F44620-72-C-0078
NSFGA 38715
NSFDES 74-22489
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences2683
Issue or Number:4
Record Number:CaltechAUTHORS:20150218-073106036
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20150218-073106036
Official Citation:Hiroo Kanamori, Gordon S. Stewart, Mode of the strain release along the Gibbs fracture zone, Mid-Atlantic ridge, Physics of the Earth and Planetary Interiors, Volume 11, Issue 4, June 1976, Pages 312-332, ISSN 0031-9201, http://dx.doi.org/10.1016/0031-9201(76)90018-2. (http://www.sciencedirect.com/science/article/pii/0031920176900182)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:54911
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:18 Feb 2015 15:52
Last Modified:09 Mar 2020 13:18

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