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• W2076222719 abstract "Research Article| May 01, 2001 Modeling the influence of sinking anhydrite blocks on salt diapirs targeted for hazardous waste disposal Hemin A. Koyi Hemin A. Koyi 1Hans Ramberg Tectonic Laboratory, Department of Earth Sciences, Uppsala University, SE-752 36 Uppsala, Sweden Search for other works by this author on: GSW Google Scholar Author and Article Information Hemin A. Koyi 1Hans Ramberg Tectonic Laboratory, Department of Earth Sciences, Uppsala University, SE-752 36 Uppsala, Sweden Publisher: Geological Society of America Received: 11 Sep 2000 Revision Received: 22 Jan 2001 Accepted: 26 Jan 2001 First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2001) 29 (5): 387–390. https://doi.org/10.1130/0091-7613(2001)029<0387:MTIOSA>2.0.CO;2 Article history Received: 11 Sep 2000 Revision Received: 22 Jan 2001 Accepted: 26 Jan 2001 First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Hemin A. Koyi; Modeling the influence of sinking anhydrite blocks on salt diapirs targeted for hazardous waste disposal. Geology 2001;; 29 (5): 387–390. doi: https://doi.org/10.1130/0091-7613(2001)029<0387:MTIOSA>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Due to the low permeability and high ductility of rock salt, many salt diapirs, such as those in Germany and the Netherlands, are targeted as long-term repositories for disposal of high-level radioactive and chemical wastes. Geophysical and subsurface data show that the Gorleben salt diapir, which is one of the most extensively investigated diapirs in the world, and other salt diapirs of the Zechstein Formation in Germany contain large blocks (∼80 m thick) of high-density anhydrite inclusions. These blocks, which were carried upward by the rising salt, are considered to be detached segments of intercalated layers that initially were deposited with the salt. Results of physical and numerical models, presented here, show that such detached, high-density blocks, which were entrained and carried upward by the diapir at an earlier stage, tend to sink in the late stages of diapiric evolution when the rate of diapiric rise slows down. During their descent, these high- density competent blocks deform by folding and create shear zones at the immediate contact with the less competent salt. The descending blocks initiate a secondary internal flow within the salt diapirs they descend, and they may deform any repository built within such diapirs, which would otherwise be considered as tectonically inactive. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2076222719 title "Modeling the influence of sinking anhydrite blocks on salt diapirs targeted for hazardous waste disposal" @default.
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• W2076222719 doi "https://doi.org/10.1130/0091-7613(2001)029<0387:mtiosa>2.0.co;2" @default.
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