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Reinterpretation of the RRISP-77 Iceland shear-wave profiles

Reinterpretation of the RRISP-77 Iceland shear-wave profiles


Title: Reinterpretation of the RRISP-77 Iceland shear-wave profiles
Author: Menke, William
Brandsdóttir, Bryndís   orcid.org/0000-0002-4018-0697
Einarsson, Páll   orcid.org/0000-0002-6893-9626
Bjarnason, Ingi Þorleifur   orcid.org/0000-0001-5716-7053
Date: 1996-07
Language: English
Scope: 166-172
University/Institute: Háskóli Íslands
University of Iceland
School: Verkfræði- og náttúruvísindasvið (HÍ)
School of Engineering and Natural Sciences (UI)
Department: Raunvísindastofnun (HÍ)
Science Institute (UI)
Series: Geophysical Journal International;126(1)
ISSN: 0956-540X
1365-246X (eISSN)
DOI: 10.1111/j.1365-246X.1996.tb05275.x
Subject: Geophysics; Crust; Iceland; Reykjanes Rigde; S waves; Jarðeðlisfræði; Jarðskorpa; Jarðskorpuhreyfingar; Bylgjufræði; Reykjaneshryggur
URI: https://hdl.handle.net/20.500.11815/567

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Citation:

Menke, W., Brandsdóttir, B., Einarsson, P. and Bjarnason, I. Th. (1996), Reinterpretation of the RRISP-77 Iceland shear-wave profiles. Geophysical Journal International, 126: 166–172. doi: 10.1111/j.1365-246X.1996.tb05275.x

Abstract:

Two shear-wave profiles, E and G, collected during the 1977 Reykjanes Ridge Iceland Seismic Experiment have played an important role in models of the Icelandic crust. They were originally interpreted as indicating very low shear-wave velocities and abnormally low shear-wave quality factors in the 10–15 km depth range. These attributes, which are indicative of near-solidus temperatures, were used to support the hypothesis that the crust of Iceland is relatively thin (10–15 km) and underlain by partially molten material. More recent seismic data, however, contradict this hypothesis and suggest that the crust is thicker (20–30 km) and cooler. A re-examination of the RRISP-77 data indicates that the low shear-wave velocities are artefacts arising from source static anomalies (in the case of profile G) and misidentification of a secondary shear phase, SmS, as S (in the case of profile E). Furthermore, the attenuation occurs at ranges when rays from the shots pass near the Askja (profile E) and Katla and Oraefajokull (profile G) volcanoes. It may therefore have a localized source, and not be diagnostic of Icelandic crust as a whole. This new interpretation of the RRISP-77 shear-wave data is consistent with models having a thick, cold crust.

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