Results 61 to 70 of about 142,515 (77)

The Topography and the Geological Structure of the Accretionary Prism in the northern part of Nansei-syoto Trench Topography and the Geological Structure of the Accretionary Prism

, 1996
Hydrographic Department of Japan (JHD) has been conducting geological and geophysical surveys by S/V TAKUYO under the Continental Shelf Surveys Project since 1983 in the southern waters of Japan.
Kato, Yukihiro
core  

The structure and fault activity of the Makran accretionary prism

Journal of Geophysical Research: Solid Earth, 2012
The Makran Subduction Zone has the highest incoming sediment thickness (up to 7.5 km) of any subduction zone. These sediments have formed a wide accretionary prism (~400 km). Seismicity in the Makran is generally low; however the margin experienced an Mw
Timothy Henstock, Lisa C McNeill
exaly   +2 more sources

Geochemistry of basaltic blueschists from the Deyader Metamorphic Complex (Makran Accretionary Prism, SE Iran): New constraints for magma generation in the Makran sector of the Neo-Tethys

Journal of Asian Earth Sciences, 2022
The North Makran Domain in the Makran Accretionary Prism consists of an imbricate stack of Mesozoic Neo-Tethyan ophiolitic and metaophiolitic units. The Deyader Complex is an important metamorphic unit of this Domain and includes tectonic slices of HP-LT
Emilio Saccani, Asghar Dolati, Michele Marroni   +2 more
exaly   +2 more sources

Fluid generation and distribution in the highest sediment input accretionary margin, the Makran

Earth and Planetary Science Letters, 2014
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 ...
Volkhard Spiess, Timothy Henstock, Lisa C McNeill   +2 more
exaly   +2 more sources

New Geochemical and Age Data on the Bajgan Complex (Makran Accretionary Prism, SE Iran): Implications for the Redefinition of Its Tectonic Setting of Formation from a Paleozoic Continental Basement to a Cretaceous Oceanic Domain

Advances in Science, Technology and Innovation, 2023
The Bajgan Complex (BC) in the North Makran Domain (Makran Accretionary Prism, SE Iran) has been considered a remnant of a Paleozoic metamorphic continental basement detached from the southernmost edge of the Lut Block.
Emilio Saccani, Asghar Dolati, Michele Marroni   +2 more
exaly   +2 more sources

Seismic quality factors across a bottom simulating reflector in the Makran Accretionary Prism, Arabian Sea

Marine and Petroleum Geology, 2011
The hydrate-bearing sediments above the bottom simulating reflector (BSR) are associated with low attenuation or high quality factor (Q), whereas underlying gas-bearing sediments exhibit high attenuation.
Kalachand Sain
exaly   +2 more sources

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Power-Law Viscoelastic Flow of the Lower Accretionary Prism in the Makran Subduction Zone Following the 2013 Baluchistan Earthquake

Journal of Geophysical Research: Solid Earth, 2022
Shaoyang Li, Guo Cheng
exaly  

Characteristics of major and trace elements in surface sediments of the Makran Accretionary Prism and their implications for natural gas hydrates

China Geology, 2021
Syed Waseem Haider, Jian-Wen Chen
exaly  

New evidence for Late Cretaceous plume-related seamounts in the Middle East sector of the Neo-Tethys: Constraints from geochemistry, petrology, and mineral chemistry of the magmatic rocks from the western Durkan Complex (Makran Accretionary Prism, SE Iran)

Lithos, 2021
Emilio Saccani, Asghar Dolati, Michele Marroni   +2 more
exaly  

Compressional and Shear Wave Pre-Stack Analysis of Gas-Hydrate Resources in the Makran Accretionary Prism

Energy Exploration and Exploitation, 2014
Abdolrahim Javaherian
exaly