Item talk:Q312885
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Widespread loess-like deposit in the Martian northern lowlands identifies Middle Amazonian climate change", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70135621", "url": "https://pubs.usgs.gov/publication/70135621" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70135621 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1130/G33513.1", "url": "https://doi.org/10.1130/G33513.1" } ], "journal": { "@type": "Periodical", "name": "Geology", "volumeNumber": "40", "issueNumber": "12" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Geology" } ], "datePublished": "2014", "dateModified": "2018-12-05", "abstract": "Consistently mappable units critical to distinguishing the style and interplay of geologic processes through time are sparse in the Martian lowlands. This study identifies a previously unmapped Middle Amazonian (ca. 1 Ga) unit (Middle Amazonian lowland unit, mAl) that postdates the Late Hesperian and Early Amazonian lowland plains by >2 b.y. The unit is regionally defined by subtle marginal scarps and slopes, has a mean thickness of 32 m, and extends >3.1 \u00d7 106\u00a0km2\u00a0between lat 35\u00b0N and 80\u00b0N. Pedestal-type craterforms and nested, arcuate ridges (thumbprint terrain) tend to occur adjacent to unit mAl outcrops, suggesting that current outcrops are vestiges of a more extensive deposit that previously covered \u223c16 \u00d7 106\u00a0km2. Exposed layers, surface pits, and the draping of subjacent landforms allude to a sedimentary origin, perhaps as a loess-like deposit emplaced rhythmically through atmospheric fallout. We propose that unit mAl accumulated coevally with, and at the expense of, the erosion of the north polar basal units, identifying a major episode of Middle Amazonian climate-driven sedimentation in the lowlands. This work links ancient sedimentary processes to climate change that occurred well before those implied by current orbital and spin axis models.", "description": "4 p.", "publisher": { "@type": "Organization", "name": "Geological Society of America" }, "author": [ { "@type": "Person", "name": "Skinner, James A. jskinner@usgs.gov", "givenName": "James A.", "familyName": "Skinner", "email": "jskinner@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-3644-7010", "url": "https://orcid.org/0000-0002-3644-7010" }, "affiliation": [ { "@type": "Organization", "name": "Astrogeology Science Center", "url": "https://www.usgs.gov/centers/astrogeology-science-center" } ] }, { "@type": "Person", "name": "Tanaka, Kenneth L. ktanaka@usgs.gov", "givenName": "Kenneth L.", "familyName": "Tanaka", "email": "ktanaka@usgs.gov", "affiliation": [ { "@type": "Organization", "name": "Astrogeology Science Center", "url": "https://www.usgs.gov/centers/astrogeology-science-center" } ] }, { "@type": "Person", "name": "Platz, Thomas", "givenName": "Thomas", "familyName": "Platz", "affiliation": [ { "@type": "Organization", "name": "Institute of Geological Sciences, Planetary Sciences and Remote Sensing, Freie Universitat Berlin" }, { "@type": "Organization", "name": "Max Planck Institute for Solar System Research, G\u00f6ttingen, Germany" } ] } ], "funder": [ { "@type": "Organization", "name": "Astrogeology Science Center", "url": "https://www.usgs.gov/centers/astrogeology-science-center" } ] }
}