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Salt Diapir sentence examples within Buried Salt Diapir
This study employs Interferometric Synthetic Aperture Radar (InSAR) data sets to monitor the surface deformation of the Nasr-Abad buried salt diapir in the Central Basin of Iran.
This study employs Interferometric Synthetic Aperture Radar (InSAR) data sets to monitor the surface deformation of the Nasr-Abad buried salt diapir in the Central Basin of Iran.
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ABSTRACT This study employs interferometric synthetic aperture radar (InSAR) data sets to monitor the surface deformation of the Nasr Abad buried salt diapir in the Central Basin of Iran.
ABSTRACT This study employs interferometric synthetic aperture radar (InSAR) data sets to monitor the surface deformation of the Nasr Abad buried salt diapir in the Central Basin of Iran.
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Salt Diapir sentence examples within Large Salt Diapir
The development is located on the flank of a large salt diapir and the wells calibrated the seismic response and the structural configuration of the salt flank.
The development is located on the flank of a large salt diapir and the wells calibrated the seismic response and the structural configuration of the salt flank.
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We define three structural domains based on their distinctive salt structures and associated deformation: 1) a region in the northeastern study area consists of relatively undeformed, late Jurassic-Cretaceous section underlain by 0–300 m-thick salt; 2) areas in the central and southwestern study area contain late Mesozoic gravity slides defined by 300–600 m-thick salt rollers and normal faults rooted onto a 1–4° basinward-dipping salt detachment; and 3) the distal margin of the western and central study area exhibits large salt diapirs up to 6 km tall that deform Quaternary stratigraphic units.
We define three structural domains based on their distinctive salt structures and associated deformation: 1) a region in the northeastern study area consists of relatively undeformed, late Jurassic-Cretaceous section underlain by 0–300 m-thick salt; 2) areas in the central and southwestern study area contain late Mesozoic gravity slides defined by 300–600 m-thick salt rollers and normal faults rooted onto a 1–4° basinward-dipping salt detachment; and 3) the distal margin of the western and central study area exhibits large salt diapirs up to 6 km tall that deform Quaternary stratigraphic units.
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Salt Diapir sentence examples within Active Salt Diapir
Existing definitions for passive and active salt diapirism are somewhat overlapping and ambiguous.
Existing definitions for passive and active salt diapirism are somewhat overlapping and ambiguous.
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Kuh-e-Namak (Dashti) namakier is one of the most active salt diapirs along the Zagros fold–thrust belt in Iran.
Kuh-e-Namak (Dashti) namakier is one of the most active salt diapirs along the Zagros fold–thrust belt in Iran.
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Salt Diapir sentence examples within Caume Salt Diapir
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
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Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
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Salt Diapir sentence examples within salt diapir sourced
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
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Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
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10.1016/J.JSG.2021.104422
Two iconic salt diapirs in the Zagros Mountains in Iran – Karmostaj (Gach) and Siah Taq – are regarded as world-class examples of salt extrusions and are frequently called "salt glaciers".
Two iconic salt diapirs in the Zagros Mountains in Iran – Karmostaj (Gach) and Siah Taq – are regarded as world-class examples of salt extrusions and are frequently called "salt glaciers".
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10.1306/05212020001
Existing definitions for passive and active salt diapirism are somewhat overlapping and ambiguous.
Existing definitions for passive and active salt diapirism are somewhat overlapping and ambiguous.
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10.1007/s10064-021-02387-z
The Tangab Dam was constructed at a unique geological structure, within a karst valley at the deepest point of a saddle-shaped feature which was formed by tectonic compression of a post-folding shear zone and later uplifting by two salt diapirs.
The Tangab Dam was constructed at a unique geological structure, within a karst valley at the deepest point of a saddle-shaped feature which was formed by tectonic compression of a post-folding shear zone and later uplifting by two salt diapirs.
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10.3389/feart.2021.556329
Spatial analysis revealed that flares were not randomly distributed but show a relation to locations of subsurface salt diapirs.
Spatial analysis revealed that flares were not randomly distributed but show a relation to locations of subsurface salt diapirs.
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10.1007/s12517-021-06627-0
Analyzing the movement and segmentation of these elastic and viscous stringers provides a comprehensive understanding of the intricate internal deformation mechanisms in the associated salt diapirs.
Analyzing the movement and segmentation of these elastic and viscous stringers provides a comprehensive understanding of the intricate internal deformation mechanisms in the associated salt diapirs.
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10.1016/J.TECTO.2021.228887
More than ~10-km-long salt sheets were efficiently evacuated back towards the Hormuz-Salt diapir, and consequently, maintained the Fars-Salt evacuation and flow to the same direction, accompanied by welding of both salt layers.
More than ~10-km-long salt sheets were efficiently evacuated back towards the Hormuz-Salt diapir, and consequently, maintained the Fars-Salt evacuation and flow to the same direction, accompanied by welding of both salt layers.
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10.5194/EGUSPHERE-EGU21-11685
extended salt walls, salt diapirs, and salt pillows in the depth range up to 8 km.
extended salt walls, salt diapirs, and salt pillows in the depth range up to 8 km.
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10.2110/JSR.2020.047
The salt diapirs grew reactively, then passively, during the Aptian–Albian, and are flanked by deep-water carbonate (Aptian–earliest Albian Urgonian Group) and siliciclastic (middle Albian–Cenomanian Black Flysch Group) successions.
The salt diapirs grew reactively, then passively, during the Aptian–Albian, and are flanked by deep-water carbonate (Aptian–earliest Albian Urgonian Group) and siliciclastic (middle Albian–Cenomanian Black Flysch Group) successions.
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10.1016/J.GEOMORPH.2021.107824
Banded terrain is a planetary enigma that may be associated with salt diapirs.
Banded terrain is a planetary enigma that may be associated with salt diapirs.
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10.1144/JGS2020-136
Emergent salt diapirs are highly mobile geological objects, the kinematics of which pose essential pure and applied problems for geologists and engineers.
Emergent salt diapirs are highly mobile geological objects, the kinematics of which pose essential pure and applied problems for geologists and engineers.
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10.5194/EGUSPHERE-EGU21-13593
During this period, the salt diapirism was accompanied by the development of salt withdrawal minibasins, characterized important growth strata due the differential subsidence.
During this period, the salt diapirism was accompanied by the development of salt withdrawal minibasins, characterized important growth strata due the differential subsidence.
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10.1007/s11600-021-00634-1
Northern Punjab is relatively stable part of the Indian shield with Precambrian basement rock overlaid by varying thickness of salt diapirs and thick sedimentary cover.
Northern Punjab is relatively stable part of the Indian shield with Precambrian basement rock overlaid by varying thickness of salt diapirs and thick sedimentary cover.
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10.5194/EGUSPHERE-EGU21-7220
(1) The western zone is dominated by tectonics with salt diapirism and faults which interact with bottom currents to form erosional pools and ridge systems.
(1) The western zone is dominated by tectonics with salt diapirism and faults which interact with bottom currents to form erosional pools and ridge systems.
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10.1007/s10712-020-09623-3
Using integrated Interferometric Synthetic Aperture Radar (InSAR) datasets (Envisat: 2003–2009; Sentinel-1: 2014–2018), local gravity surveys, and passive seismic data, we investigated the environmental hazards associated with the rise of the Miocene Jazan salt diapir (JZD; ~ 2 km 2 ) within Jazan city, Saudi Arabia, and identified areas at risk in its immediate surroundings.
Using integrated Interferometric Synthetic Aperture Radar (InSAR) datasets (Envisat: 2003–2009; Sentinel-1: 2014–2018), local gravity surveys, and passive seismic data, we investigated the environmental hazards associated with the rise of the Miocene Jazan salt diapir (JZD; ~ 2 km 2 ) within Jazan city, Saudi Arabia, and identified areas at risk in its immediate surroundings.
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10.3390/MIN11070763
Upper Cretaceous chert nodules were sampled at Araxos, where rocks are highly faulted and uplifted by salt diapirism, and on Kastos Island, on the flanks of a regional anticline.
Upper Cretaceous chert nodules were sampled at Araxos, where rocks are highly faulted and uplifted by salt diapirism, and on Kastos Island, on the flanks of a regional anticline.
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10.2113/rgg20214352
The results of numerical modeling of the salt diapir formation processes are presented, and the types of anticlinal structures, potential oil- and gas-promising objects, are considered.
The results of numerical modeling of the salt diapir formation processes are presented, and the types of anticlinal structures, potential oil- and gas-promising objects, are considered.
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10.1038/s41598-021-91517-4
Salt diapirism is often associated with potential hydrocarbon energy resources, and detecting active diapirs can strongly affect the prospect to discover new gas and oilfields.
Salt diapirism is often associated with potential hydrocarbon energy resources, and detecting active diapirs can strongly affect the prospect to discover new gas and oilfields.
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10.1016/J.TECTO.2021.228860
In recent years, salt diapirs have been widely used for gas storing, hazardous waste disposal, mining, and petroleum production.
In recent years, salt diapirs have been widely used for gas storing, hazardous waste disposal, mining, and petroleum production.
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10.5194/EGUSPHERE-EGU21-5680
</p><p>We present 3 areas of application for our method, covering salt diapirs, magmatic systems and subduction zones, using both synthetic and real data.
</p><p>We present 3 areas of application for our method, covering salt diapirs, magmatic systems and subduction zones, using both synthetic and real data.
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10.1144/jgs2020-085
Squeezing of salt diapirs and thrust welding occurred as salt ridges were unroofed.
Squeezing of salt diapirs and thrust welding occurred as salt ridges were unroofed.
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10.1007/s12517-021-06663-w
Iso-resistivity 3D surfaces at 30 m and 60 m depths have been generated using the interpreted data which exhibits salt diapiric structure and dissolution of salt at depth by the action of infiltrating water from nearby ephemeral stream.
Iso-resistivity 3D surfaces at 30 m and 60 m depths have been generated using the interpreted data which exhibits salt diapiric structure and dissolution of salt at depth by the action of infiltrating water from nearby ephemeral stream.
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10.1016/j.quascirev.2020.106719
In addition, the similarity of the elevations of the different sea-level indicators at the two locations in As-Salif Peninsula and Kamran Island suggest relative tectonic stability, with limited influence of salt diapirism.
In addition, the similarity of the elevations of the different sea-level indicators at the two locations in As-Salif Peninsula and Kamran Island suggest relative tectonic stability, with limited influence of salt diapirism.
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10.1016/J.JAFREARSCI.2021.104330
During the deposition of the Jurassic–Cretaceous “red beds”, the Central High Atlas Basin was subjected to important tectonics and salt diapirism events.
During the deposition of the Jurassic–Cretaceous “red beds”, the Central High Atlas Basin was subjected to important tectonics and salt diapirism events.
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10.22059/GEOPE.2021.313048.648581
Syn- and post sedimentation activities of the salt diapirs have dramatically affected the surrounding sedimentary successions in the SE Zagros.
Syn- and post sedimentation activities of the salt diapirs have dramatically affected the surrounding sedimentary successions in the SE Zagros.
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10.3390/JMSE9040396
The mud diapir and salt diapir are diapir structures driven by gravity slides, gravity spread and differential compaction.
The mud diapir and salt diapir are diapir structures driven by gravity slides, gravity spread and differential compaction.
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10.1007/s11069-021-04791-w
The main objective of this study is to detect the subsurface extension of salt diapirs and structural deformations in the city of Jazan and its suburbs using gravity data.
The main objective of this study is to detect the subsurface extension of salt diapirs and structural deformations in the city of Jazan and its suburbs using gravity data.
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10.1007/s12549-021-00496-x
Eight of these sections encircle the Caldas da Rainha Diapir, which was a prominent, emergent, passive salt diapir during the time of deposition.
Eight of these sections encircle the Caldas da Rainha Diapir, which was a prominent, emergent, passive salt diapir during the time of deposition.
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10.3390/geosciences11080341
Additionally, the host rocks were probably also deformed and fractured during the rise of salt diapirs that characterise this part of the Adriatic foreland.
Additionally, the host rocks were probably also deformed and fractured during the rise of salt diapirs that characterise this part of the Adriatic foreland.
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10.5194/EGUSPHERE-EGU21-14873
The Zagros fold-and-thrust belt in Southern Iran is famous for its spectacular outcrops of salt diapirs.
The Zagros fold-and-thrust belt in Southern Iran is famous for its spectacular outcrops of salt diapirs.
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10.1088/1755-1315/817/1/012085
Excess of the total square of all forms of nature management under an area of the landscape geosystem formed by salt diapir, represented as the coefficient of nature management (CNM), acts as trigger risk.
Excess of the total square of all forms of nature management under an area of the landscape geosystem formed by salt diapir, represented as the coefficient of nature management (CNM), acts as trigger risk.
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10.3390/rs13040785
Kuh-e-Namak (Dashti) namakier is one of the most active salt diapirs along the Zagros fold–thrust belt in Iran.
Kuh-e-Namak (Dashti) namakier is one of the most active salt diapirs along the Zagros fold–thrust belt in Iran.
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10.1051/bsgf/2021033
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
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10.1130/2021.2550(05)
While the structure was first considered to be a salt diapir, its impact origin was confirmed in 1989 based on the findings of rare shocked quartz grains and a few poorly developed “shatter cones.
While the structure was first considered to be a salt diapir, its impact origin was confirmed in 1989 based on the findings of rare shocked quartz grains and a few poorly developed “shatter cones.
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10.1007/s11356-021-16135-z
A natural source of pollution in the vicinity of Svetly Yar may be hidden geologically active structures: faults in the Earth’s crust, a salt diapir, an underground ancient semiactive volcanic zone on a steppe, etc.
A natural source of pollution in the vicinity of Svetly Yar may be hidden geologically active structures: faults in the Earth’s crust, a salt diapir, an underground ancient semiactive volcanic zone on a steppe, etc.
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10.1007/s12517-021-07525-1
Unconformity-bound growth strata associated with passively rising salt diapirs defined as halokinetic sequences have been recognized within the Debadib-Ben Gasser Triassic salt body (El Kef–Tajerouine area), at the Triassic contact at Guern Halfaya, at J.
Unconformity-bound growth strata associated with passively rising salt diapirs defined as halokinetic sequences have been recognized within the Debadib-Ben Gasser Triassic salt body (El Kef–Tajerouine area), at the Triassic contact at Guern Halfaya, at J.
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10.1007/s00531-021-02026-8
Three of these regions are located over deep-rooted tectonic faults or salt diapirs and one is in an area without any tectonic or halokinetic activity, but with steep topography.
Three of these regions are located over deep-rooted tectonic faults or salt diapirs and one is in an area without any tectonic or halokinetic activity, but with steep topography.
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10.1190/int-2020-0102.1
We then use the resulting facies probability volumes to construct the 3D distribution of the salt diapir geobodies embedded in a stratigraphic matrix.
We then use the resulting facies probability volumes to construct the 3D distribution of the salt diapir geobodies embedded in a stratigraphic matrix.
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10.5194/EGUSPHERE-EGU21-3233
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit.
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10.1016/S1876-3804(21)60010-1
The experimental results show that the subsalt slopes in the middle West Africa basins are steeper, so the salt rock is likely to rapidly flow towards the ocean to form larger and fewer salt diapirs.
The experimental results show that the subsalt slopes in the middle West Africa basins are steeper, so the salt rock is likely to rapidly flow towards the ocean to form larger and fewer salt diapirs.
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10.1016/J.MARPETGEO.2021.105194
The minibasins adjacent to the Bakio salt diapir, in northern Spain, provide a unique opportunity to study up to seven outcropping MTDs comparable in size to subsurface examples.
The minibasins adjacent to the Bakio salt diapir, in northern Spain, provide a unique opportunity to study up to seven outcropping MTDs comparable in size to subsurface examples.
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10.1016/J.JOG.2019.05.006
This study employs Interferometric Synthetic Aperture Radar (InSAR) data sets to monitor the surface deformation of the Nasr-Abad buried salt diapir in the Central Basin of Iran.
This study employs Interferometric Synthetic Aperture Radar (InSAR) data sets to monitor the surface deformation of the Nasr-Abad buried salt diapir in the Central Basin of Iran.
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10.3997/2214-4609.201901254
The development is located on the flank of a large salt diapir and the wells calibrated the seismic response and the structural configuration of the salt flank.
The development is located on the flank of a large salt diapir and the wells calibrated the seismic response and the structural configuration of the salt flank.
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10.1016/J.MARPETGEO.2019.04.002
Geometric and stratigraphic characteristics of halokinetic sequences adjacent to the salt diapirs highlight the sedimentation response to variation in the rate of salt rise.
Geometric and stratigraphic characteristics of halokinetic sequences adjacent to the salt diapirs highlight the sedimentation response to variation in the rate of salt rise.
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10.1144/petgeo2018-113
We show that a permeable bed tilted by rise of a salt diapir substantially increases pore pressure in sediments near the diapir through hydraulically connecting these sediments to deep, high-overpressure sediments far from the diapir.
We show that a permeable bed tilted by rise of a salt diapir substantially increases pore pressure in sediments near the diapir through hydraulically connecting these sediments to deep, high-overpressure sediments far from the diapir.
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10.1155/2019/5647857
The stratigraphic position of the dolomite reservoirs embedded at the base of a salt diapir had a strong impact on its diagenetic development.
The stratigraphic position of the dolomite reservoirs embedded at the base of a salt diapir had a strong impact on its diagenetic development.
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10.1016/B978-0-12-815048-1.00009-3
The structure of the Fars geological province is a result of the interaction of the Zagros orogeny and Hormuz salt diapirism.
The structure of the Fars geological province is a result of the interaction of the Zagros orogeny and Hormuz salt diapirism.
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10.1007/s10040-018-1912-1
The presented study explores the salt dissolution potential of fluids around a salt diapir in the Transylvanian town of Ocna Mures, Romania, which is facing land-collapse hazards related to salt mining activities.
The presented study explores the salt dissolution potential of fluids around a salt diapir in the Transylvanian town of Ocna Mures, Romania, which is facing land-collapse hazards related to salt mining activities.
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10.1144/petgeo2018-119
To address this, we have developed 2D geomechanical models using the finite-element method to simulate salt diapir and pillow development in two extensional tectonic settings.
To address this, we have developed 2D geomechanical models using the finite-element method to simulate salt diapir and pillow development in two extensional tectonic settings.
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10.1134/S0024490219020032
The paper addresses regularities in the location and conditions of the formation of salt diapirs.
The paper addresses regularities in the location and conditions of the formation of salt diapirs.
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10.3389/fmicb.2019.00024
, elemental) sulfur deposits can be part of caprock assemblages found on top of or in lateral position to salt diapirs and as stratabound mineralization in gypsum and anhydrite lithologies.
, elemental) sulfur deposits can be part of caprock assemblages found on top of or in lateral position to salt diapirs and as stratabound mineralization in gypsum and anhydrite lithologies.
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10.31857/S0024-497X20192130-148
The paper addresses regularities in the location and conditions of the formation of salt diapirs.
The paper addresses regularities in the location and conditions of the formation of salt diapirs.
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10.1016/J.MARPETGEO.2019.02.002
It is characterised by strong compression/shortening due to the sliding of the post-salt super-sequence, resulting in numerous salt diapirs that control the location of seafloor oil seep sites.
It is characterised by strong compression/shortening due to the sliding of the post-salt super-sequence, resulting in numerous salt diapirs that control the location of seafloor oil seep sites.
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10.1007/s12517-019-4611-x
Some of these features correspond to lithological contacts; others reflect tectonic trough zones, Triassic salt diapirs, sedimentary basins, anticlines, and faults.
Some of these features correspond to lithological contacts; others reflect tectonic trough zones, Triassic salt diapirs, sedimentary basins, anticlines, and faults.
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10.1038/s41598-019-55226-3
We contend that the ACCR was formed by upward fluid flow along active sub-surface faults and fractures that formed by lateral extension generated by the ascending movement of salt diapirs at depth.
We contend that the ACCR was formed by upward fluid flow along active sub-surface faults and fractures that formed by lateral extension generated by the ascending movement of salt diapirs at depth.
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10.1016/J.JSEAES.2018.08.024
Three types of iron ore, including banded ore, hydrothermal-metasomatic ore and earthy hematite ochre occur in Hormuz and Pohl salt diapirs.
Three types of iron ore, including banded ore, hydrothermal-metasomatic ore and earthy hematite ochre occur in Hormuz and Pohl salt diapirs.
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10.1144/petgeo2018-095
We focus on a salt diapir, where an exploratory well has been drilled crossing a major fault.
We focus on a salt diapir, where an exploratory well has been drilled crossing a major fault.
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10.18280/EESRJ.060102
The deformed fault-block movement is related to the impacts of strike-slip movements, growing salt diapirs.
The deformed fault-block movement is related to the impacts of strike-slip movements, growing salt diapirs.
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10.1080/07038992.2019.1610656
Axel Heiberg Island has the second highest concentration of salt diapirs globally.
Axel Heiberg Island has the second highest concentration of salt diapirs globally.
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10.1016/J.OREGEOREV.2019.04.006
Based on ore textures, fluid inclusions, isotope data, and geochemical compositions of sulfide minerals, the Kuh-e-Surmeh sulfide mineralization is believed to have precipitated from low-temperature sedimentary basin brines and should be classified as a Mississippi Valley-type deposit in a salt diapir environment.
Based on ore textures, fluid inclusions, isotope data, and geochemical compositions of sulfide minerals, the Kuh-e-Surmeh sulfide mineralization is believed to have precipitated from low-temperature sedimentary basin brines and should be classified as a Mississippi Valley-type deposit in a salt diapir environment.
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10.1016/B978-0-12-815048-1.00005-6
High activity of Na in the salt diapirs provided a suitable mechanism to form blue amphiboles before the theoretical values of pressure and temperature.
High activity of Na in the salt diapirs provided a suitable mechanism to form blue amphiboles before the theoretical values of pressure and temperature.
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10.1088/1742-6596/1279/1/012042
Accurate interpretation and analysis of good quality 2D-seismic data has contributed to understanding evolution of salt diapirism in the Syrian Offshore located in the easternmost Mediterranean.
Accurate interpretation and analysis of good quality 2D-seismic data has contributed to understanding evolution of salt diapirism in the Syrian Offshore located in the easternmost Mediterranean.
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10.1016/J.JSG.2019.02.002
The variations in the rate of salt rise is reflected in the sedimentary sequences adjacent to salt diapirs and provides insights into the style of salt movement-sedimentation interaction and the timing of halokinetic phases.
The variations in the rate of salt rise is reflected in the sedimentary sequences adjacent to salt diapirs and provides insights into the style of salt movement-sedimentation interaction and the timing of halokinetic phases.
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10.1007/978-3-319-93127-2_22
Results show the average estimated rates of salt movement to be 1–2 cm per thousand years, over the top of salt diapirs in the Abyssal Plain, as opposed to 3–5 cm per thousand years near the active convergent plate boundary in the south and near the Sardinian slope to the north where increased stress on salt may be due to the confinement of Sardinian bedrock.
Results show the average estimated rates of salt movement to be 1–2 cm per thousand years, over the top of salt diapirs in the Abyssal Plain, as opposed to 3–5 cm per thousand years near the active convergent plate boundary in the south and near the Sardinian slope to the north where increased stress on salt may be due to the confinement of Sardinian bedrock.
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10.1016/J.JAFREARSCI.2019.03.018
Hormuz Island is a salt diapir in southern Iran, which also comprises transported blocks of rhyolitic and rhyodacitic rocks, which were brought to the surface during the island's diapiric emergence from the Persian Gulf.
Hormuz Island is a salt diapir in southern Iran, which also comprises transported blocks of rhyolitic and rhyodacitic rocks, which were brought to the surface during the island's diapiric emergence from the Persian Gulf.
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10.1080/22020586.2019.12073180
In the central and eastern part of the basin, salt diapirs and associated salt withdrawal and expulsion structures were active during rifting and breakup.
In the central and eastern part of the basin, salt diapirs and associated salt withdrawal and expulsion structures were active during rifting and breakup.
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10.3997/2214-4609.201950075
It is concluded that in the Anabar-Khatanga and Lena-Anabar oil-and-gas areas Permian anticlinal traps complexly related to the salt diapirs have the best prospects of petroleum production.
It is concluded that in the Anabar-Khatanga and Lena-Anabar oil-and-gas areas Permian anticlinal traps complexly related to the salt diapirs have the best prospects of petroleum production.
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10.3997/2214-4609.201901556
The multiple rift phases and salt diapirism have led to multiple structural, stratigraphic and combination play types.
The multiple rift phases and salt diapirism have led to multiple structural, stratigraphic and combination play types.
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10.1016/J.JSG.2019.103870
The telescopic behavior of the salt wall represents a mode of internal deformation that might be applicable to other salt diapirs worldwide.
The telescopic behavior of the salt wall represents a mode of internal deformation that might be applicable to other salt diapirs worldwide.
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10.1306/12181818038
It also increases with increasing offset from the salt diapirs, which can be associated with a large lateral heat-flow component in the complex tectonic environment of the Nordkapp Basin.
It also increases with increasing offset from the salt diapirs, which can be associated with a large lateral heat-flow component in the complex tectonic environment of the Nordkapp Basin.
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10.1134/S0001437019040192
The oil and gas bearing potential on the margins of basins is associated with Late Cretaceous and Tertiary sediments, alluvial fan deposits, and salt diapirs.
The oil and gas bearing potential on the margins of basins is associated with Late Cretaceous and Tertiary sediments, alluvial fan deposits, and salt diapirs.
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10.1016/J.QUASCIREV.2019.105871
Stable isotopes of pore-fluid sulfate (δ34S and δ18O) are similar to the values found in bulk sulfate minerals from the nearby Mount Sedom salt diapir.
Stable isotopes of pore-fluid sulfate (δ34S and δ18O) are similar to the values found in bulk sulfate minerals from the nearby Mount Sedom salt diapir.
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10.3997/2214-4609.2019X604054
In this new study we analyze a properly sampled VSP recorded offshore Brazil in a well drilled on the opposite side of the salt diapir.
In this new study we analyze a properly sampled VSP recorded offshore Brazil in a well drilled on the opposite side of the salt diapir.
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10.3997/2214-4609.201900030
Shallow gas clouds and shallow channels are resolved with the FWI updates, deeper structures including basement horsts within the Senja Ridge and the flanks of salt diapirs are solved with the tomographic updates.
Shallow gas clouds and shallow channels are resolved with the FWI updates, deeper structures including basement horsts within the Senja Ridge and the flanks of salt diapirs are solved with the tomographic updates.
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10.1007/s41063-019-00068-6
The sedimentary deposits of the central Sverdrup Basin on Ellef Ringnes Island were affected by both salt diapirism and igneous activity of the Cretaceous High Arctic Large Igneous Province (HALIP).
The sedimentary deposits of the central Sverdrup Basin on Ellef Ringnes Island were affected by both salt diapirism and igneous activity of the Cretaceous High Arctic Large Igneous Province (HALIP).
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10.1190/SEGAM2019-3216007.1
The first step is to choose candidate attributes that may be able to differentiate chaotic mass-transport deposits and salt diapirs from the more conformal, coherent background reflectors.
The first step is to choose candidate attributes that may be able to differentiate chaotic mass-transport deposits and salt diapirs from the more conformal, coherent background reflectors.
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10.4138/ATLGEOL.2019.004
Examples are provided detailing characteristics of springs associated with faults, karst, salt diapirs, rockfall/alluvial systems and debris avalanche sites.
Examples are provided detailing characteristics of springs associated with faults, karst, salt diapirs, rockfall/alluvial systems and debris avalanche sites.
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10.3997/2214-4609.201903154
The base and top of the Miocene basin in WPG are expressed by two regional erosional unconformities, whereas a salt diapiric wall/nappe has been attributed to Triassic salt exhumation.
The base and top of the Miocene basin in WPG are expressed by two regional erosional unconformities, whereas a salt diapiric wall/nappe has been attributed to Triassic salt exhumation.
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10.5194/SE-10-1283-2019
In contrast, early differential sedimentary loading in the mid-slope area
creates minibasins separated by salt diapirs overprinting the translational
domain.
In contrast, early differential sedimentary loading in the mid-slope area
creates minibasins separated by salt diapirs overprinting the translational
domain.
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10.5194/SE-2019-2
In contrast, early differential sedimentary loading in the mid-slope area creates minibasins intervened by salt diapirs overprinting the translational domain.
In contrast, early differential sedimentary loading in the mid-slope area creates minibasins intervened by salt diapirs overprinting the translational domain.
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10.5194/SE-11-1187-2020
Suprasalt deformation
geometries and orientations are strongly controlled by the salt diapir and ridge network produced during extension and subsequent
downbuilding.
Suprasalt deformation
geometries and orientations are strongly controlled by the salt diapir and ridge network produced during extension and subsequent
downbuilding.
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10.12911/22998993/99743
Furthermore, the evidence from chloride and 14 C contents was found to indicate the presence of more saline groundwater, which are influenced by the groundwater flows near salt diapirs.
Furthermore, the evidence from chloride and 14 C contents was found to indicate the presence of more saline groundwater, which are influenced by the groundwater flows near salt diapirs.
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10.1017/S0016756818000018
Although the structural features and formation mechanism of salt diapirs have been extensively investigated, mud diapirs are still not fully understood, largely due to the difficulty of identifying them from seismic data.
Although the structural features and formation mechanism of salt diapirs have been extensively investigated, mud diapirs are still not fully understood, largely due to the difficulty of identifying them from seismic data.
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10.3997/2214-4609.201900510
This abstract presents a workflow for quantifying the overpressure due to both the lateral strain exerted by a salt diapir and the clay diagenesis (smectite to illite transformation).
This abstract presents a workflow for quantifying the overpressure due to both the lateral strain exerted by a salt diapir and the clay diagenesis (smectite to illite transformation).
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10.1080/01431161.2019.1608386
ABSTRACT This study employs interferometric synthetic aperture radar (InSAR) data sets to monitor the surface deformation of the Nasr Abad buried salt diapir in the Central Basin of Iran.
ABSTRACT This study employs interferometric synthetic aperture radar (InSAR) data sets to monitor the surface deformation of the Nasr Abad buried salt diapir in the Central Basin of Iran.
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10.1016/J.GEOMORPH.2019.06.018
This paper explores the use of trenching and paleoseismological techniques to determine salt flow rates into a salt diapir for the first time in the literature.
This paper explores the use of trenching and paleoseismological techniques to determine salt flow rates into a salt diapir for the first time in the literature.
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10.3997/2214-4609.201900887
Summary The Mungo field in the North Sea is both structurally and stratigraphically complex - salt diapirism has resulted in large dips on the Palaeocene and Cretaceous reservoirs that drape the flanks of the salt intrusion.
Summary The Mungo field in the North Sea is both structurally and stratigraphically complex - salt diapirism has resulted in large dips on the Palaeocene and Cretaceous reservoirs that drape the flanks of the salt intrusion.
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10.1016/J.MARPETGEO.2019.03.001
We define three structural domains based on their distinctive salt structures and associated deformation: 1) a region in the northeastern study area consists of relatively undeformed, late Jurassic-Cretaceous section underlain by 0–300 m-thick salt; 2) areas in the central and southwestern study area contain late Mesozoic gravity slides defined by 300–600 m-thick salt rollers and normal faults rooted onto a 1–4° basinward-dipping salt detachment; and 3) the distal margin of the western and central study area exhibits large salt diapirs up to 6 km tall that deform Quaternary stratigraphic units.
We define three structural domains based on their distinctive salt structures and associated deformation: 1) a region in the northeastern study area consists of relatively undeformed, late Jurassic-Cretaceous section underlain by 0–300 m-thick salt; 2) areas in the central and southwestern study area contain late Mesozoic gravity slides defined by 300–600 m-thick salt rollers and normal faults rooted onto a 1–4° basinward-dipping salt detachment; and 3) the distal margin of the western and central study area exhibits large salt diapirs up to 6 km tall that deform Quaternary stratigraphic units.
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10.3390/GEOSCIENCES9070316
Although the thermal effect of large salt tongues and allochthonous salt sheets in passive margins is described in the literature, little is known about the thermal effect of salt structures in confined rift basins where sub-vertical, closely spaced salt diapirs may affect the thermal evolution and petroleum system of the basin.
Although the thermal effect of large salt tongues and allochthonous salt sheets in passive margins is described in the literature, little is known about the thermal effect of salt structures in confined rift basins where sub-vertical, closely spaced salt diapirs may affect the thermal evolution and petroleum system of the basin.
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10.1016/j.epsl.2019.115843
Seismic data from Perdido Canyon show two clustered BSRs associated with turbidite sequences within two dome folds formed from tectonic folding and salt diapir rise.
Seismic data from Perdido Canyon show two clustered BSRs associated with turbidite sequences within two dome folds formed from tectonic folding and salt diapir rise.
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10.1190/INT-2018-0246.1
Multiple attributes are tested to classify salt diapirs, mass transport deposits (MTDs), and the conformal reflector “background” for a 3D seismic marine survey acquired on the northern Gulf of Mexico shelf.
Multiple attributes are tested to classify salt diapirs, mass transport deposits (MTDs), and the conformal reflector “background” for a 3D seismic marine survey acquired on the northern Gulf of Mexico shelf.
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