Simulation of Mushroom Caps on Salt in Barents Sea, Norway

Various shapes of moving salt were simulated in response to gravity contrast and tectonic movement, and the deformations and fractures of the surrounding sediments examined. The varying parameters in the model include the burial depth of the salt base, the overhang depth of the salt cap, the salt bo...

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Published in:Energy Exploration & Exploitation
Main Authors: Yu, Z., Lerche, I.
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 1991
Subjects:
Online Access:http://dx.doi.org/10.1177/014459879100900301
https://journals.sagepub.com/doi/pdf/10.1177/014459879100900301
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spelling crsagepubl:10.1177/014459879100900301 2024-09-30T14:32:53+00:00 Simulation of Mushroom Caps on Salt in Barents Sea, Norway Yu, Z. Lerche, I. 1991 http://dx.doi.org/10.1177/014459879100900301 https://journals.sagepub.com/doi/pdf/10.1177/014459879100900301 en eng SAGE Publications https://journals.sagepub.com/page/policies/text-and-data-mining-license Energy Exploration & Exploitation volume 9, issue 3, page 94-106 ISSN 0144-5987 2048-4054 journal-article 1991 crsagepubl https://doi.org/10.1177/014459879100900301 2024-09-10T04:25:25Z Various shapes of moving salt were simulated in response to gravity contrast and tectonic movement, and the deformations and fractures of the surrounding sediments examined. The varying parameters in the model include the burial depth of the salt base, the overhang depth of the salt cap, the salt body's size, the salt speed of motion, and the sediment depositional rate. Variation of the surrounding rock properties with depth, such as Lame constants, shearing strength, internal friction were also considered. Mohr's criterion (Mohr, 1900) for failure was applied, allowing an indication of where fractures occur and their orientations. Including the thermal effects of salt in the models yields features favorable to hydrocarbon accumulation: (1) Fractures generated near the vertical salt body and below the mushroom cap salt provide a continuous pathway for hydrocarbon migration due to the enhancement of permeability; (2) The overhanging cap salt sheet provides a good trapping mechanism by formation of seals; (3) The thermal effect of salt enhances the maturity of the source rocks; (4) The observed faulting behaviour around the salt body is accounted for by primary and secondary fracture development as exhibited through the simulations. Application of modelling to the study of a salt diapir in Barents Sea, Norway, shows that the salt would most likely start to rise during the Early-Mid Triassic and Jurassic when the sediment cover was about 1700–2400 m. Depositional faulting was associated with salt diapir motion. The modelling also indicates that at least 1000 m of the salt cap was eroded, based on the dip angles of sedimentary strata against the salt stock. Article in Journal/Newspaper Barents Sea SAGE Publications Barents Sea Norway Energy Exploration & Exploitation 9 3 94 106
institution Open Polar
collection SAGE Publications
op_collection_id crsagepubl
language English
description Various shapes of moving salt were simulated in response to gravity contrast and tectonic movement, and the deformations and fractures of the surrounding sediments examined. The varying parameters in the model include the burial depth of the salt base, the overhang depth of the salt cap, the salt body's size, the salt speed of motion, and the sediment depositional rate. Variation of the surrounding rock properties with depth, such as Lame constants, shearing strength, internal friction were also considered. Mohr's criterion (Mohr, 1900) for failure was applied, allowing an indication of where fractures occur and their orientations. Including the thermal effects of salt in the models yields features favorable to hydrocarbon accumulation: (1) Fractures generated near the vertical salt body and below the mushroom cap salt provide a continuous pathway for hydrocarbon migration due to the enhancement of permeability; (2) The overhanging cap salt sheet provides a good trapping mechanism by formation of seals; (3) The thermal effect of salt enhances the maturity of the source rocks; (4) The observed faulting behaviour around the salt body is accounted for by primary and secondary fracture development as exhibited through the simulations. Application of modelling to the study of a salt diapir in Barents Sea, Norway, shows that the salt would most likely start to rise during the Early-Mid Triassic and Jurassic when the sediment cover was about 1700–2400 m. Depositional faulting was associated with salt diapir motion. The modelling also indicates that at least 1000 m of the salt cap was eroded, based on the dip angles of sedimentary strata against the salt stock.
format Article in Journal/Newspaper
author Yu, Z.
Lerche, I.
spellingShingle Yu, Z.
Lerche, I.
Simulation of Mushroom Caps on Salt in Barents Sea, Norway
author_facet Yu, Z.
Lerche, I.
author_sort Yu, Z.
title Simulation of Mushroom Caps on Salt in Barents Sea, Norway
title_short Simulation of Mushroom Caps on Salt in Barents Sea, Norway
title_full Simulation of Mushroom Caps on Salt in Barents Sea, Norway
title_fullStr Simulation of Mushroom Caps on Salt in Barents Sea, Norway
title_full_unstemmed Simulation of Mushroom Caps on Salt in Barents Sea, Norway
title_sort simulation of mushroom caps on salt in barents sea, norway
publisher SAGE Publications
publishDate 1991
url http://dx.doi.org/10.1177/014459879100900301
https://journals.sagepub.com/doi/pdf/10.1177/014459879100900301
geographic Barents Sea
Norway
geographic_facet Barents Sea
Norway
genre Barents Sea
genre_facet Barents Sea
op_source Energy Exploration & Exploitation
volume 9, issue 3, page 94-106
ISSN 0144-5987 2048-4054
op_rights https://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/014459879100900301
container_title Energy Exploration & Exploitation
container_volume 9
container_issue 3
container_start_page 94
op_container_end_page 106
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