Microbial communities of deep-sea methane seeps at Hikurangi continental margin (New Zealand). [PDF]
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]
Bates J +27 more
europepmc +1 more source
Tsunami modelling over global oceans. [PDF]
Kolukula SS +4 more
europepmc +1 more source
On the variation of b-value for Karachi region, Pakistan through Gumbel’s extreme distribution method [PDF]
Ahmed, Naseer +2 more
core +1 more source
Seismic velocities and images of the Makran subduction zone
Kopp, C. +5 more
openaire +2 more sources
Investigating the impacts of agricultural land use on soil earthworm communities: A case study of northern Zagros Mountains of Iran. [PDF]
Karimifard S +3 more
europepmc +1 more source
New Constraints for the On‐Shore Makran Subduction Zone Crustal Structure [PDF]
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]
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, 2020Abstract 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

