Item talk:Q267646
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Dome formation on Ceres by sold-state flow analogous to terrestrial salt tectonics", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70212304", "url": "https://pubs.usgs.gov/publication/70212304" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70212304 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1038/s41561-019-0453-0", "url": "https://doi.org/10.1038/s41561-019-0453-0" } ], "journal": { "@type": "Periodical", "name": "Nature Geoscience", "volumeNumber": "12", "issueNumber": null }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Nature Geoscience" } ], "datePublished": "2019", "dateModified": "2020-08-14", "abstract": "The dwarf planet Ceres\u2019s outer crust is a complex, heterogeneous mixture of ice, clathrates, salts and silicates. Numerous large domes on Ceres\u2019s surface indicate a degree of geological activity. These domes have been attributed to cryovolcanism, but that is difficult to reconcile with Ceres\u2019s small size and lack of long-lived heat sources. Here we alternatively propose that Ceres\u2019s domes form by solid-state flow within the compositionally heterogeneous crust, a mechanism directly analogous to salt tectonics on Earth. We use numerical simulations to illustrate that differential loading of a crust with compositional heterogeneity on a scale of tens of kilometres can produce dome-like features of scale similar to those observed. The mechanism requires the presence of low-viscosity and low-density, possibly ice-rich, material in the upper 1\u201310\u2009km of the subsurface. Such substantial regional heterogeneity in Ceres\u2019s crustal composition is consistent with observations from the National Aeronautics and Space Administration\u2019s Dawn mission. We conclude that deformation analogous to that in terrestrial salt tectonics is a viable alternative explanation for the observed surface morphologies, and is consistent with Ceres being both cold and geologically active.", "description": "5 p.", "publisher": { "@type": "Organization", "name": "Springer Nature" }, "author": [ { "@type": "Person", "name": "Bland, Michael T. mbland@usgs.gov", "givenName": "Michael T.", "familyName": "Bland", "email": "mbland@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-5543-1519", "url": "https://orcid.org/0000-0001-5543-1519" }, "affiliation": [ { "@type": "Organization", "name": "Astrogeology Science Center", "url": "https://www.usgs.gov/centers/astrogeology-science-center" } ] }, { "@type": "Person", "name": "Buczkowski, D. L", "givenName": "D. L", "familyName": "Buczkowski", "affiliation": [ { "@type": "Organization", "name": "Johns Hopkins Applied Physics Lab" } ] }, { "@type": "Person", "name": "Sizemore, H. G.", "givenName": "H. G.", "familyName": "Sizemore", "affiliation": [ { "@type": "Organization", "name": "Planetary Science Inst." } ] }, { "@type": "Person", "name": "Ermakov, A. I.", "givenName": "A. I.", "familyName": "Ermakov", "affiliation": [ { "@type": "Organization", "name": "Jet Propulsion Lab" } ] }, { "@type": "Person", "name": "King, S. D", "givenName": "S. D", "familyName": "King", "affiliation": [ { "@type": "Organization", "name": "Virginia Tech" } ] }, { "@type": "Person", "name": "Sori, M. M.", "givenName": "M. M.", "familyName": "Sori", "affiliation": [ { "@type": "Organization", "name": "University of Arizona" } ] }, { "@type": "Person", "name": "Raymond, C. A.", "givenName": "C. 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