Results 161 to 170 of about 1,464 (199)

Microbial communities of deep-sea methane seeps at Hikurangi continental margin (New Zealand). [PDF]

open access: yesPLoS One, 2013
Ruff SE   +6 more
europepmc   +1 more source

Early to Mid-Holocene land use transitions in South Asia: A new archaeological synthesis of potential human impacts. [PDF]

open access: yesPLoS One
Bates J   +27 more
europepmc   +1 more source

Tsunami modelling over global oceans. [PDF]

open access: yesR Soc Open Sci
Kolukula SS   +4 more
europepmc   +1 more source

Seismic velocities and images of the Makran subduction zone

open access: yes, 1999
Kopp, C.   +5 more
openaire   +2 more sources

Cold Vents - die kalten Quellen der Tiefseegräben [PDF]

open access: yes, 1996
Bohrmann, Gerhard, Suess, Erwin
core  

New Constraints for the On‐Shore Makran Subduction Zone Crustal Structure [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 2022
AbstractThe Makran Subduction Zone is the primary seismic/tsunami hazard of the northwestern Indian Ocean, but little is known of its on‐shore seismic structure. We derived a shear wave velocity model extending to 100 km depth beneath a ∼400 km‐long seismic profile oriented parallel to the convergence vector of the Arabian Sea Plate.
Keith Priestley   +2 more
exaly   +2 more sources

Thermal structure and megathrust seismogenic potential of the Makran subduction zone [PDF]

open access: yesGeophysical Research Letters, 2013
The Makran subduction zone experienced a tsunamigenic Mw 8.1 earthquake in 1945 and recent, smaller earthquakes also suggest seismicity on the megathrust; however, its historical record is limited and hazard potential enigmatic. We have developed a 2‐D thermal model of the subduction zone.
Lisa C Mcneill, Kelin Wang, Tim Henstock
exaly   +4 more sources
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Deep structure of the western coast of the Makran subduction zone, SE Iran

Tectonophysics, 2020
Abstract The Makran subduction zone is one of the world's least well documented active subduction zones. We investigate the geometry of subsurface velocity interfaces across the western coastal Makran by means of teleseismic data for the first time. The data were gathered by two permanent and four temporary seismic stations.
Esmaeil Shabanian
exaly   +2 more sources

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