Results 21 to 30 of about 3,754 (159)
Identification of Gas Accumulation Adjacent to the Gas Hydrate Bearing Zone by Inversion Utilizing AVO Attribute [PDF]
The presence of gas hydrate and associated gas in the Makran Accretionary Prism, offshore Iran, has been confirmed by various seismic indicators, including the bottom-simulating reflector (BSR), amplitude blanking, and bright spot. The pre-stack analysis
Effat Behboudi +2 more
doaj +1 more source
Abstract The Greater Antilles islands of Cuba, Hispaniola, Puerto Rico and Jamaica plus the Virgin Islands host fragments of the fossil convergent margin that records Cretaceous subduction (operated for about 90 m.y.) of the American plates beneath the Caribbean plate and ensuing arc‐continent collision in Late Cretaceous‐Eocene time.
H. Y. Hu +3 more
wiley +1 more source
New Constraints for the On‐Shore Makran Subduction Zone Crustal Structure
Abstract The 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. Receiver function/
Keith Priestley +6 more
wiley +1 more source
Abstract Shallow slip on the plate‐boundary fault during the 2004 Mw 9.2 Aceh‐Andaman Earthquake, offshore North Sumatra, has been linked to thick incoming sediments on the oceanic plate with advanced diagenetic and sediment property changes at the depths of plate boundary fault development.
Duncan E. Stevens +2 more
wiley +1 more source
Assessment of gas-hydrate saturations in the Makran accretionary prism using the offset dependence of seismic amplitudes [PDF]
We estimate the saturations of gas hydrate and free gas based on measurements of seismic-reflection amplitude variation with offset (AVO) for a bottom-simulating reflector coupled with rock-physics modeling. When we apply the approach to data from a seismic line in the Makran accretionary prism in the Arabian Sea, the results reveal lateral variations
M. Ojha, K. Sain, T. Minshull
semanticscholar +4 more sources
Abstract The Semail ophiolite, a thick thrust sheet of Late Cretaceous oceanic crust and upper mantle, was obducted onto the previously rifted Arabian continental margin in the Late Cretaceous, and now forms part of the United Arab Emirates (UAE)‐Oman mountain belt.
S. Pilia +5 more
wiley +1 more source
Crustal Deformation and Fault Strength of the Sulawesi Subduction Zone
Abstract This paper investigates the seismicity and rheology of the North‐Sulawesi subduction zone. Body‐wave modeling is used to estimate focal mechanisms and centroid depths of moderate magnitude (M5–M6.5) earthquakes on the North Sulawesi megathrust and surrounding region.
T. Greenfield +5 more
wiley +1 more source
Effects of mass waste events on thrust wedges: Analogue experiments and application to the Makran accretionary wedge [PDF]
Olistostromes cover large portions of active thrust wedges like Makran, Gulf of Cadiz, and offshore Borneo. Olistostrome emplacement by submarine mass flow represents an instantaneous and massive mass redistribution that may influence thrust wedge ...
Burg, J.P. +3 more
core +2 more sources
Tectonics of the Papua‐Woodlark Region
Abstract The Papua‐Woodlark region exemplifies many plate tectonic processes, from active continental breakup to double plunging subduction zones. We present a synthesis of geological and geophysical data from the region and interpret these data to characterize the present plate boundaries.
Elizabeth K. Benyshek, Brian Taylor
wiley +1 more source
Release of mineral-bound water prior to subduction tied to shallow seismogenic slip off Sumatra [PDF]
Plate-boundary fault rupture during the 2004 Sumatra-Andaman subduction earthquake extended closer to the trench than expected, increasing earthquake and tsunami size.
Abby R. Kenigsberg +35 more
core +5 more sources

