Results 91 to 100 of about 217 (124)

Remote Sensing and GIS Analysis of Spatial Distribution of Fracture Patterns in the Makran Accretionary Prism, Southeast Iran

open access: yes, 2007
This study shows that remote sensing and GIS are powerful tools in identifying geologically induced lineaments from digitally enhanced ETM+ satellite imageries and the digital elevation model (DEM) in remote areas such as the Makran accretionary prism, southeast Iran.
Pokharel, Shankar Babu
openaire   +3 more sources
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Quantitative seismic pre-stack analysis of potential gas-hydrate resources in the Makran Accretionary Prism, offshore Iran

Marine and Petroleum Geology, 2013
Abstract Gas hydrates are classified as a major unconventional resource and assumed to be a future potential energy source. High pressures, low temperature stability conditions of the hydrates restrict their occurrence to the permafrost and deep sea regions (from the continental slop to the abyssal).
Abdolrahim Javaherian
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

open access: yesJournal 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   +2 more
exaly   +2 more sources

P-T evolution of metapelites from the Bajgan complex in the Makran accretionary prism, south eastern Iran

open access: yesGeochemistry, 2017
Abstract The Bajgan Complex, one of the basement constituents of the arc massif in Iranian Makran forms a rugged, deeply incised terrain. The complex consists of pelitic schists with minor psammitic and basic schists, calc silicate rocks, amphibolites, marbles, metavolcanosediments, mafic and felsic intrusives as well as ultramafic rocks. Metapelitic
Dorani, Maryam   +3 more
openaire   +2 more sources

The western Durkan Complex (Makran Accretionary Prism, SE Iran): A Late Cretaceous tectonically disrupted seamounts chain and its role in controlling deformation style

open access: yesGeoscience Frontiers, 2021
The Durkan Complex is a key tectonic element of the Makran accretionary prism (SE Iran) and it has been interpreted as representing a continental margin succession.
Edoardo Barbero   +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

open access: yesAdvances 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.
Edoardo Barbero   +2 more
exaly   +2 more sources

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

open access: yesEarth 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 ...
Lisa C Mcneill   +2 more
exaly   +2 more sources

Drilling the Un Drillable: A Case Study of the Bela Well in Makran Accretionary Prism

SPE/IADC Middle East Drilling Technology Conference and Exhibition, 2021
Abstract The Bela Well is situated on Makran accretionary prism with several active mud volcanoes that makes conventional drilling challenging due to the extremely high pore pressure i.e. in excess of 15,000 psi and a very narrow window between pore pressure and fracture pressure. This adverse condition was observed in the 9 offset wells
Umair Ahmed Baig, Ghulam Nabi Agha
openaire   +1 more source

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) [PDF]

open access: yesLithos, 2021
The Durkan Complex in the Makran Accretionary Prism (SE Iran) has been interpreted either as a continental margin succession or a Late Cretaceous tectonically disrupted seamount chain.
Edoardo Barbero   +2 more
exaly   +2 more sources

Sediment compaction and fluid migration in the Makran Accretionary Prism

Journal of Geophysical Research: Solid Earth, 1989
The Makran continental margin in the Gulf of Oman forms the seaward extremity of an accretionary sediment prism which extends several hundred kilometers inland. A recently acquired multichannel seismic reflection profile shot across the margin imaged the structure of the prism in greater detail than was previously possible and allowed us to investigate
Tim Minshull, Robert White
openaire   +1 more source

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