Results 31 to 40 of about 115 (95)
Interaction between accretionary thrust faulting and slope sedimentation at the frontal Makran accretionary prism and its implications for hydrocarbon fluid seepage [PDF]
Using high‐resolution seismic profiles and other geophysical data, collected during R/V Meteor Cruise M74/2, we investigate the distribution patterns of shallow sediments, their structure and deformation processes, and their role in the migration, accumulation and seepage of hydrocarbon‐rich fluids.
Ding, Feng +5 more
openaire +3 more sources
Abstract Climate change, sea level fluctuations, and tectonic uplift play key roles in the evolution of sedimentary systems on continental margins. In the Arabian Sea, the Makran continental margin is suitable for studying these processes during the Holocene due to its high sedimentation rate and continuous sequence of Holocene sediments.
Wei He, Jianguo Liu, Yun Huang, Li Cao
wiley +1 more source
THE POTENTIAL OF TSUNAMI GENERATION ALONG THE MAKRAN SUBDUCTION ZONE IN THE NORTHERN ARABIAN SEA. CASE STUDY: THE EARTHQUAKE AND TSUNAMI OF NOVEMBER 28, 1945 [PDF]
Although large earthquakes along the Makran Subduction Zone are infrequent, the potential for the generation of destructive tsunamis in the Northern Arabian Sea cannot be overlooked.
George Pararas-Carayannis
doaj
Cenozoic Evolution of the North‐Eastern Mediterranean Basins
Abstract The Eastern Mediterranean lies at the junction of the African, Arabian, and Eurasian plates, a region shaped by a long and complex tectonic history. While the Levant Basin in the southern sector has been extensively studied for hydrocarbon exploration, the northern domain offshore Cyprus, Turkey, Syria, and Lebanon remains less understood.
Nicolò Bertone +6 more
wiley +1 more source
Restoring the Missing Late Cretaceous Arc of Iran
Abstract Persistent arc magmatism archives fluid transport and mantle partial melting in subduction zones. However, arc magmatism often exhibits different magmatic records along the strike, as seen in the Tethyan orogenic belt. During Neo‐Tethys subduction under Iran, there was pulsed arc magmatism with Middle Jurassic and Eocene magmatic flare‐ups ...
Yiyang Lei +10 more
wiley +1 more source
Abstract The Indo‐Burman subduction zone represents a global endmember for extreme sediment accretion and is a region characterized by ambiguous tectonic structure. The recent collection of broadband seismic data across the Indo‐Burman accretionary margin as part of the Bangladesh‐India‐Myanmar Array (BIMA) experiment provides an opportunity to ...
Christopher J. W. Carchedi +10 more
wiley +1 more source
The Makran Subduction Zone (MSZ) gained wide interest following the 1945 tsunamigenic earthquake. This three-part (A, B, and C) review provides a comprehensive and multidisciplinary synthesis of 80 years of research on tsunamigenic earthquakes associated
Mouloud Hamidatou +5 more
doaj +1 more source
Abstract To understand ophiolite emplacement mechanisms in New Caledonia, southwest Pacific, we image crustal and lithospheric structures beneath southern Grande Terre, using seismic waveform data from a network (ITOPNC) of permanent and temporary stations (October 2018–November 2019). Surface wave dispersion indicates a 1–2 km thick ophiolite nappe on
Shao‐Jinn Chin +4 more
wiley +1 more source
Abstract We use satellite‐derived high‐resolution topography and orthoimages, namely, preearthquake Advanced Land Observing Satellite World 3‐D data and postearthquake Pleiades data, to retrieve 3‐D displacements in the 2013 Balochistan, Pakistan, earthquake.
Yu Zhou +2 more
wiley +1 more source
Abstract The Fujairah basin in the Gulf of Oman experienced a complex tectonic evolution related to Late Cretaceous ophiolite obduction and Oligocene‐Miocene Zagros continental collision. The structure of the foreland basin in Oman‐UAE is well‐known, but the structure and evolution of the hinterland basin behind the obducted ophiolite and underlying ...
M. Y. Ali +5 more
wiley +1 more source

