Results 51 to 60 of about 217 (124)
The Makran Accretionary Prism (SE of Iran) is part of the Alpine-Himalayan orogenic system, and it is still associated with active subduction. The Makran results from the Cretaceous to resent-day convergence between the Arabian and Eurasian plates that ...
Luciani V. +10 more
core
Fluids in subduction zones can influence seismogenic behaviour and prism morphology. The Eastern Makran subduction zone, offshore Pakistan, has a very thick incoming sediment section of up to 7.5 km, providing a large potential fluid source to the ...
Spieß, Volkhard +4 more
core +2 more sources
Subduction zone accretionary prisms are commonly modeled as elastic structures where permanent deformation is accommodated by faulting and folding of otherwise elastic materials, yet accretionary prisms may exhibit other deformation styles over ...
William Barnhart, Shaoyang Li, Guo Cheng
core +1 more source
Rare earth elements of ROV sample GeoB12338-2 from the Makran accretionary complex
Authigenic carbonates forming at an active methane-seep on the Makran accretionary prism mainly consist of aragonite in the form of microcrystalline, cryptocrystalline, and botryoidal phases. The d13Ccarbonate values are very negative (-49.0 to -44.0 per
Bach, Wolfgang +7 more
core +1 more source
Preliminary petrological and stratigraphic data on the Band-e-Zeyarat ophiolite (Makran accretionary wedge, SE Iran) [PDF]
The North Makran is the innermost structural domain of the Makran Accretionary Prism (SE Iran). It consists of an imbricated stack of south-verging tectonic units and chaotic complexes, which are (from north to south): 1) the northern ophiolites (e.g ...
Dolati A. +10 more
core +1 more source
Seismic properties of sediments are strongly influenced by pore fluids. Stiffness of unconsolidated marine sediment increases with the presence of gas hydrate and decreases with the presence of gas.
Sain, Kalachand, Ghosh, Ranjana
core +1 more source
Land subsidence analysis using synthetic aperture radar data. [PDF]
Bokhari R +7 more
europepmc +1 more source
Seamounts are topographic highs of the oceanic plates, and they are passively carried toward convergent margins where they may interact with the frontal part of the subduction complexes, modifying their shape and influencing the operating tectonic processes.
Barbero, Edoardo +7 more
openaire +1 more source
InSAR time series data for the 2014–2021 period reveal up to 20 cm of radar line‐of‐sight displacements in the area of the 2013 Mw 7.7 Balochistan earthquake northwest of the Hoshab Fault in the eastern Makran subduction zone in southwest Pakistan.
Yun Shao +5 more
core +1 more source
A snapshot of the long-term evolution of a distributed tectonic plate boundary. [PDF]
Dalaison M, Jolivet R, Le Pourhiet L.
europepmc +1 more source

