Open AccessCrustal model of the Bransfield Rift, West Antarctica, from detailed OBS refraction experiments
Author(s) -
Grad M.,
Shiobara H.,
Janik T.,
Guterch A.,
Shimamura H.
Publication year - 1997
Publication title -
geophysical journal international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0956-540X
DOI - 10.1111/j.1365-246x.1997.tb05665.x
Subject(s) - geology , rift , seismometer , seismology , crust , volcano , trough (economics) , lithosphere , geophysics , tectonics , economics , macroeconomics
SUMMARY The first detailed deep seismic refraction study in the Bransfield Strait, West Antarctica, using sensitive OBSs (ocean bottom seismographs) was carried out successfully during the Antarctic summer of 1990/1991. The experiment focused on the deep crustal structure beneath the axis of the Bransfield Rift. Seismic profile DSS‐20 was located exactly in the Bransfield Trough, which is suspected to be a young rift system. Along the profile, five OBSs were deployed at spacings of 50‐70 km. 51 shots were fired along the 310 km profile. This paper gives the first presentation of the results. A detailed model of the crustal structure was obtained by modelling the observed traveltimes and amplitudes using a 2‐D ray‐tracing technique. The uppermost (sedimentary?) cover, with velocities of 2.0‐5.5 km s −1 , reaches a depth of up to 8 km. Below this, a complex with velocities of 6.4‐6.8 km s −1 is observed. The presence of a high‐velocity body, with V p = 7.3‐7.7 km s −1 , was detected in the 14‐32 km depth range in the central part of the profile. These inhomogeneities can be interpreted as a stage of back‐arc spreading and stretching of the continental crust, coinciding with the Deception‐Bridgeman volcanic line. Velocities of 8.1 km s −1 , characteristic of the Moho, are observed along the profile at a depth of 30‐32 km.