Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Wiebke Heise"'
Autor:
Gerard Muñoz Soler, Wiebke Heise, C. Paz, E. Almeida, Fernando Monteiro Santos, Jaume Pous i Fábregas
Publikováno v:
Geologica Acta, Vol 3, Iss 3 (2005)
The south-western part of the Iberian Peninsula, including the southern branch of the Iberian Massif, has recently been the subject of several magnetotelluric (MT) studies. This area is made up of three different tectonic terranes: the South Portugue
Externí odkaz:
https://doaj.org/article/85124a8f58d74b95a822fc6d97c42493
Autor:
Wiebke Heise, D. H. Mac Manus, Craig J. Rodger, Malcolm Ingham, E. Bertrand, Michael Dalzell, Tim Divett, K. Mukhtar, Tanja Petersen
Publikováno v:
Space Weather. 18
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::35781a6c8edb2bb654db2ad2ac4542ef
https://doi.org/10.1029/2020sw002580
https://doi.org/10.1029/2020sw002580
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
Publikováno v:
Geothermics. 59:188-204
Since a previous review in 1995, improved geophysical networks and techniques have substantially improved our understanding of the Taupo Volcanic Zone (henceforth TVZ), and particularly why its central portion has such high outputs of magma and heat,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbc9691fa060bd45825cebdecc0dca37
https://doi.org/10.1016/j.geothermics.2015.09.008
https://doi.org/10.1016/j.geothermics.2015.09.008
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
Autor:
Susan Ellis, Wiebke Heise
Publikováno v:
Surveys in Geophysics. 37:81-107
Magnetotelluric (MT) studies represent the structure of crust and mantle in terms of conductivity anomalies, while geodynamic modelling predicts the deformation and evolution of crust and mantle subject to plate tectonic processes. Here, we review th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb2eeb7a46675656fbb966040f4879cf
https://doi.org/10.1007/s10712-015-9334-2
https://doi.org/10.1007/s10712-015-9334-2
Publikováno v:
Geophysical Research Letters. 42:5212-5218
Lazufre volcanic center, located in the central Andes, is recently undergoing an episode of uplift, conforming one of the most extensive deforming volcanic systems worldwide, but its magmatic system and its connection with the observed uplift are sti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bf29bd684ff2e47bd06ae89666438828
https://doi.org/10.1002/2015gl064426
https://doi.org/10.1002/2015gl064426
Publikováno v:
New Zealand Journal of Geology and Geophysics. 57:453-458
The effect of crustal melt on extension in the central Taupo Volcanic Zone, New Zealand is investigated using a 3D numerical model of rifting. Partial melt bodies are directly inferred from magnetotelluric imaging, and are used to determine heat flow
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b1458018c90f5cd8453048207eef6d3
https://doi.org/10.1080/00288306.2014.972961
https://doi.org/10.1080/00288306.2014.972961