Zobrazeno 1 - 10
of 19
pro vyhledávání: '"S. L. Bennie"'
Autor:
Wiebke Heise, S. L. Bennie, Edward A. Bertrand, Todd G. Caldwell, Stephen Bannister, Hiroshi Ichihara, Yasuo Ogawa
Publikováno v:
Geophysical Research Letters. 44:9261-9266
The observation of slow-slip, seismic tremor, and low-frequency earthquakes at subduction margins has provided new insight into the mechanisms by which stress accumulates between large subduction (megathrust) earthquakes. However, the relationship be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0b670eed58b652031ffbc96ef4cd44cc
https://doi.org/10.1002/2017gl074641
https://doi.org/10.1002/2017gl074641
Publikováno v:
Journal of Volcanology and Geothermal Research. 314:39-48
Magnetotelluric data were recorded in a 45 × 10 km band crossing the Rotorua and Waimangu geothermal fields in the northern part of the Taupo Volcanic Zone in the central North Island of New Zealand. 3-D inverse modelling of these data show that ben
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91b10c771d2786d9682d536f143d9833
https://doi.org/10.1016/j.jvolgeores.2015.10.017
https://doi.org/10.1016/j.jvolgeores.2015.10.017
Autor:
Yasuo Ogawa, Erin L. Wallin, T. Grant Caldwell, Graham Hill, Harry Keys, S. L. Bennie, H. M. Bibby, Edward A. Bertrand, Wiebke Heise
Publikováno v:
Earth Planet. Sci. Lett.. 432:115-125
The dynamics of magma reservoirs (the main repositories for eruptible magma) play a fundamental role in the style and behaviour of volcanic systems. A key first step in understanding these systems is to identify their location and size accurately. We
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::037fe326e81a50b6adfbc85ae6598299
http://t2r2.star.titech.ac.jp/cgi-bin/publicationinfo.cgi?q_publication_content_number=CTT100697516
http://t2r2.star.titech.ac.jp/cgi-bin/publicationinfo.cgi?q_publication_content_number=CTT100697516
Autor:
S. Soengkono, S. L. Bennie, Wiebke Heise, Graham Hill, Stephen Bannister, Edward A. Bertrand, Todd G. Caldwell
Publikováno v:
Journal of Volcanology and Geothermal Research. 305:63-75
Magnetotelluric (MT) data from 169 locations covering a 700 km 2 region in the southeastern part of the Taupo Volcanic Zone, New Zealand, are used to generate a 3-D resistivity inversion model to a depth of 10 km. Isolated zones of low-resistivity (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::92f28a380057c67617a419f381e90b4f
https://doi.org/10.1016/j.jvolgeores.2015.09.020
https://doi.org/10.1016/j.jvolgeores.2015.09.020
Publikováno v:
Journal of Volcanology and Geothermal Research. 268:36-45
Closely-spaced broadband MT (magnetotelluric) data measured on a profile through the Ohaaki geothermal system show that the basement greywacke directly beneath the geothermal field is resistive. There is no evidence in these MT data for the existence
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f5d48c18e82da432f26640fe6fc228c6
https://doi.org/10.1016/j.jvolgeores.2013.10.010
https://doi.org/10.1016/j.jvolgeores.2013.10.010
Publikováno v:
Geophysical Research Letters. 40:5029-5033
[1] Interplate coupling on the Hikurangi subduction margin along the east coast of New Zealand's North Island changes north to south from almost uncoupled to locked. Clay-rich sediments and aqueous fluids at the subduction interface have been invoked
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cfa0309c858057419471a661e4a82a81
https://doi.org/10.1002/grl.50959
https://doi.org/10.1002/grl.50959
Publikováno v:
Exploration Geophysics. 44:215-227
Shallow warm water resources associated with low enthalpy geothermal systems are often difficult to explore using geophysical techniques, mainly because the warm water creates an insufficient physical change from the host rocks to be easily detectabl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3873fe6447aa7a9eded7d6cad5e3bf12
https://doi.org/10.1071/eg13036
https://doi.org/10.1071/eg13036
Publikováno v:
Preview. 2011:37-40
Shallow warm water resources associated with low enthalpy geothermal systems are often difficult to explore usinggeophysicaltechniques,mainlybecausethewarmwatercreatesaninsufficientphysicalchangefromthehostrockstobe easily detectable. In addition, of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72cc78c72068c333d585ff0e43b93b43
https://doi.org/10.1071/pvv2011n153p37
https://doi.org/10.1071/pvv2011n153p37
Autor:
Yasuo Ogawa, H. M. Bibby, K. A. Jones, S. Dravitzki, Todd G. Caldwell, Wiebke Heise, Malcolm Ingham, P. Cairns, S. L. Bennie
Publikováno v:
Geophysical Journal International. 179:887-904
SUMMARY Mt Ruapehu is an active andesite cone volcano, which marks the southern termination of the Kermadec volcanic arc. Results from 40 broad-band magnetotelluric soundings have been analysed using the phase tensor. This approach provides a way of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9bfe1ebbf0a667cd61774e90bd0a9170
https://doi.org/10.1111/j.1365-246x.2009.04317.x
https://doi.org/10.1111/j.1365-246x.2009.04317.x
Publikováno v:
Tectonophysics. 463:77-85
A magneto-telluric (MT) pilot study is used to investigate the Taranaki Fault, a major thrust along the eastern margin of the Taranaki Basin, New Zealand. Analysis of the survey data (MT phase tensor analysis and 2D models), along a 25 km east–west
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe05a46b7bbfb703f6542fad2d2cd85b
https://doi.org/10.1016/j.tecto.2008.09.035
https://doi.org/10.1016/j.tecto.2008.09.035