Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Christine Läderach"'
Publikováno v:
Polar Science. 9:146-157
The Arctic mid-ocean ridge system constitutes the most active source of earthquakes in the north polar region. However, the characteristics of its earthquake activity at teleseismic and local scales are not well studied because of the remote location
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::049672fb979806b8208a9bd838813b9c
https://doi.org/10.1016/j.polar.2014.10.001
https://doi.org/10.1016/j.polar.2014.10.001
Publikováno v:
Geophysical Journal International. 190:429-441
The ultraslow spreading Southwest Indian Ridge (SWIR) is a prominent end member of the global mid-ocean ridge system. It spreads with a full-rate of 14 mm/y to 16 mm/y and shows several segments of various obliquities. The western SWIR consists of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0049dcc98108cf46d8ea9992188e03cf
https://doi.org/10.1111/j.1365-246x.2012.05480.x
https://doi.org/10.1111/j.1365-246x.2012.05480.x
Publikováno v:
Geophysical Journal International. 184:1354-1370
SUMMARY With its remote location in the ice-covered Fram Strait, Lena Trough is a poorly known segment of the global mid-ocean ridge system. It is a prominent member of the ultra-slow spreading mid-ocean ridges but its spreading mechanisms are not we
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6fb13aff3905b6da3ddca13111592ea9
https://doi.org/10.1111/j.1365-246x.2010.04926.x
https://doi.org/10.1111/j.1365-246x.2010.04926.x
Publikováno v:
Schwab, Marco; Läderach, Christine; Rieke-Zapp, Dirk; Schlunegger, Fritz (2007). Slip rates variability and sediment mobilization on a shallow landslide in the northern Swiss Alps. Swiss journal of geosciences, 100(2), pp. 281-292. Birkhäuser-Verlag; www.birkhäuser.ch 10.1007/s00015-007-1218-0
Geomorphic and morphometric data imply that process rates of the Schimbrig landslide, located in the Entle watershed (Central Switzerland), are still limited by the elevation of the LGM base level. At present, the Entle watershed is in a stage of adj
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b26c8a1b92667a19a42ba5d6ef09da3e
