Zobrazeno 1 - 10
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pro vyhledávání: '"Bergthóra S. Thorbjarnardóttir"'
Plain Language Summary Iceland hosts a predominantly rifting plate boundary that is offset by two ∼east-west trending, horizontally sliding (transform-faulting) segments, one in the north and the other in the south. The southern segment, known as t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3ad13ed5817138aabfac4e1c67547d2c
https://hdl.handle.net/20.500.11815/4128
https://hdl.handle.net/20.500.11815/4128
Publikováno v:
Journal of Geophysical Research: Solid Earth. 125
Publisher's version (útgefin grein)
The Ölfus seismic belt lies at the western end of the ~E‐W sinistral transform shear zone in South Iceland, called the South Iceland Seismic Zone (SISZ), where most seismicity and surface faulting show ~N
The Ölfus seismic belt lies at the western end of the ~E‐W sinistral transform shear zone in South Iceland, called the South Iceland Seismic Zone (SISZ), where most seismicity and surface faulting show ~N
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6fee210d8cd2f500ec858c66eb3a2700
https://doi.org/10.1029/2019jb019203
https://doi.org/10.1029/2019jb019203
Western South Iceland Seismic Zone (SISZ) plate boundary lies adjacent to the Hengill central volcano. The sinistral SISZ connects the two arms of the divergent Mid-Atlantic Ridge (MAR) plate boundaries (Western and Eastern Volcanic Zones; WVZ, EVZ),
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::610adea1db1e9b50a970bb4639c91cd9
https://doi.org/10.5194/egusphere-egu2020-8521
https://doi.org/10.5194/egusphere-egu2020-8521
The Great Geysir is within a tectonically active region bordering the eastern flank of the Western Volcanic Zone (WVZ), south of Langjökull glacier. The geothermal area has been active at least throughout the Holocene (Torfason, 1985). It is a high-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5134493e6256283ceaa1ae28375ef056
https://doi.org/10.5194/egusphere-egu2020-16388
https://doi.org/10.5194/egusphere-egu2020-16388