Item talk:Q251632
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Channel morphometry, sediment transport, and implications for tectonic activity and surficial ages of Titan basins", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70036114", "url": "https://pubs.usgs.gov/publication/70036114" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70036114 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1016/j.icarus.2011.03.011", "url": "https://doi.org/10.1016/j.icarus.2011.03.011" }, { "@type": "PropertyValue", "propertyID": "ISSN", "value": "00191035" } ], "journal": { "@type": "Periodical", "name": "Icarus", "volumeNumber": "214", "issueNumber": "2" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Icarus" } ], "datePublished": "2011", "dateModified": "2021-02-02", "abstract": "Fluvial features on Titan and drainage basins on Earth are remarkably similar despite differences in gravity and surface composition. We determined network bifurcation (Rb) ratios for five Titan and three terrestrial analog basins. Tectonically-modified Earth basins have\u00a0Rb\u00a0values greater than the expected range (3.0\u20135.0) for dendritic networks; comparisons with\u00a0Rb\u00a0values determined for Titan basins, in conjunction with similarities in network patterns, suggest that portions of Titan\u2019s north polar region are modified by tectonic forces. Sufficient elevation data existed to calculate bed slope and potential fluvial sediment transport rates in at least one Titan basin, indicating that 75\u00a0mm water ice grains (observed at the Huygens landing site) should be readily entrained given sufficient flow depths of liquid hydrocarbons. Volumetric sediment transport estimates suggest that \u223c6700\u201310,000 Titan years (\u223c2.0\u20133.0\u00a0\u00d7\u00a0105\u00a0Earth years) are required to erode this basin to its minimum relief (assuming constant 1\u00a0m and 1.5\u00a0m flows); these lowering rates increase to \u223c27,000\u201341,000 Titan years (\u223c8.0\u201312.0\u00a0\u00d7\u00a0105\u00a0Earth years) when flows in the north polar region are restricted to summer months.", "description": "10 p.", "publisher": { "@type": "Organization", "name": "Elsevier" }, "author": [ { "@type": "Person", "name": "Cartwright, R.", "givenName": "R.", "familyName": "Cartwright" }, { "@type": "Person", "name": "Clayton, J.A.", "givenName": "J.A.", "familyName": "Clayton" }, { "@type": "Person", "name": "Kirk, Randolph L. rkirk@usgs.gov", "givenName": "Randolph L.", "familyName": "Kirk", "email": "rkirk@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0003-0842-9226", "url": "https://orcid.org/0000-0003-0842-9226" }, "affiliation": [ { "@type": "Organization", "name": "Astrogeology Science Center", "url": "https://www.usgs.gov/centers/astrogeology-science-center" } ] } ], "funder": [ { "@type": "Organization", "name": "Astrogeology Science Center", "url": "https://www.usgs.gov/centers/astrogeology-science-center" } ] }, "OpenAlex": { "abstract_inverted_index": { "Fluvial": [ 0 ], "features": [ 1 ], "on": [ 2, 7 ], "Titan": [ 3, 27, 54, 94, 127, 158 ], "and": [ 4, 16, 28, 84, 148 ], "drainage": [ 5 ], "basins": [ 6, 35 ], "Earth": [ 8, 34, 132, 163 ], "are": [ 9, 71, 134, 172 ], "remarkably": [ 10 ], "similar": [ 11 ], "despite": [ 12 ], "differences": [ 13 ], "in": [ 14, 56, 60, 90, 167 ], "gravity": [ 15 ], "surface": [ 17 ], "composition.": [ 18 ], "We": [ 19 ], "determined": [ 20, 52 ], "network": [ 21, 61 ], "bifurcation": [ 22 ], "(Rb)": [ 23 ], "ratios": [ 24 ], "for": [ 25, 45, 53 ], "five": [ 26 ], "three": [ 29 ], "terrestrial": [ 30 ], "analog": [ 31 ], "basins.": [ 32 ], "Tectonically-modified": [ 33 ], "have": [ 36 ], "Rb": [ 37, 50 ], "values": [ 38, 51 ], "greater": [ 39 ], "than": [ 40 ], "the": [ 41, 105, 168 ], "expected": [ 42 ], "range": [ 43 ], "(3.0\u20135.0)": [ 44 ], "dendritic": [ 46 ], "networks;": [ 47 ], "comparisons": [ 48 ], "with": [ 49, 58 ], "basins,": [ 55 ], "conjunction": [ 57 ], "similarities": [ 59 ], "patterns,": [ 62 ], "suggest": [ 63, 124 ], "that": [ 64, 97, 125 ], "portions": [ 65 ], "of": [ 66, 117 ], "Titan's": [ 67 ], "north": [ 68, 169 ], "polar": [ 69, 170 ], "region": [ 70, 171 ], "modified": [ 72 ], "by": [ 73 ], "tectonic": [ 74 ], "forces.": [ 75 ], "Sufficient": [ 76 ], "elevation": [ 77 ], "data": [ 78 ], "existed": [ 79 ], "to": [ 80, 136, 140, 156, 174 ], "calculate": [ 81 ], "bed": [ 82 ], "slope": [ 83 ], "potential": [ 85 ], "fluvial": [ 86 ], "sediment": [ 87, 121 ], "transport": [ 88, 122 ], "rates": [ 89, 154 ], "at": [ 91, 104 ], "least": [ 92 ], "one": [ 93 ], "basin,": [ 95 ], "indicating": [ 96 ], "75": [ 98 ], "mm": [ 99 ], "water": [ 100 ], "ice": [ 101 ], "grains": [ 102 ], "(observed": [ 103 ], "Huygens": [ 106 ], "landing": [ 107 ], "site)": [ 108 ], "should": [ 109 ], "be": [ 110 ], "readily": [ 111 ], "entrained": [ 112 ], "given": [ 113 ], "sufficient": [ 114 ], "flow": [ 115 ], "depths": [ 116 ], "liquid": [ 118 ], "hydrocarbons.": [ 119 ], "Volumetric": [ 120 ], "estimates": [ 123 ], "\u223c6700\u201310,000": [ 126 ], "years": [ 128, 159 ], "(\u223c2.0\u20133.0": [ 129 ], "\u00d7": [ 130, 161 ], "105": [ 131, 162 ], "years)": [ 133, 164 ], "required": [ 135 ], "erode": [ 137 ], "this": [ 138 ], "basin": [ 139 ], "its": [ 141 ], "minimum": [ 142 ], "relief": [ 143 ], "(assuming": [ 144 ], "constant": [ 145 ], "1": [ 146 ], "m": [ 147, 150 ], "1.5": [ 149 ], "flows);": [ 151 ], "these": [ 152 ], "lowering": [ 153 ], "increase": [ 155 ], "\u223c27,000\u201341,000": [ 157 ], "(\u223c8.0\u201312.0": [ 160 ], "when": [ 165 ], "flows": [ 166 ], 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