Additional file 1 of Cold-based glaciation of Pavonis Mons, Mars: evidence for moraine deposition during glacial advance
Additional file 1: Figure S1. Obliquity History Five representative scenarios for the obliquity of Mars determined by Laskar et al. 2004 over the past 250 Myrs (a) and 26 Myrs (b). The different colored lines refer to different assumed values for the initial precession rate of the rotation axis of M...
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creator | Parsons, Reid A. Kanzaki, Tomohiro Ryodo Hemmi Miyamoto, Hideaki |
description | Additional file 1: Figure S1. Obliquity History Five representative scenarios for the obliquity of Mars determined by Laskar et al. 2004 over the past 250 Myrs (a) and 26 Myrs (b). The different colored lines refer to different assumed values for the initial precession rate of the rotation axis of Mars which produces chaotically different results over long timescales (b), but nearly identical results in the past 26 Myrs (a). Thick lines give obliquity over a 1 Myr averaging window. Scenario "P000" is used as our model input. |
doi_str_mv | 10.6084/m9.figshare.11978904 |
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Obliquity History Five representative scenarios for the obliquity of Mars determined by Laskar et al. 2004 over the past 250 Myrs (a) and 26 Myrs (b). The different colored lines refer to different assumed values for the initial precession rate of the rotation axis of Mars which produces chaotically different results over long timescales (b), but nearly identical results in the past 26 Myrs (a). Thick lines give obliquity over a 1 Myr averaging window. Scenario "P000" is used as our model input.</description><identifier>DOI: 10.6084/m9.figshare.11978904</identifier><language>eng</language><publisher>figshare</publisher><subject>FOS: Earth and related environmental sciences ; Geology</subject><creationdate>2020</creationdate><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><orcidid>0000-0002-9947-346X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>780,1894</link.rule.ids><linktorsrc>$$Uhttps://commons.datacite.org/doi.org/10.6084/m9.figshare.11978904$$EView_record_in_DataCite.org$$FView_record_in_$$GDataCite.org$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Parsons, Reid A.</creatorcontrib><creatorcontrib>Kanzaki, Tomohiro</creatorcontrib><creatorcontrib>Ryodo Hemmi</creatorcontrib><creatorcontrib>Miyamoto, Hideaki</creatorcontrib><title>Additional file 1 of Cold-based glaciation of Pavonis Mons, Mars: evidence for moraine deposition during glacial advance</title><description>Additional file 1: Figure S1. Obliquity History Five representative scenarios for the obliquity of Mars determined by Laskar et al. 2004 over the past 250 Myrs (a) and 26 Myrs (b). The different colored lines refer to different assumed values for the initial precession rate of the rotation axis of Mars which produces chaotically different results over long timescales (b), but nearly identical results in the past 26 Myrs (a). Thick lines give obliquity over a 1 Myr averaging window. 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Obliquity History Five representative scenarios for the obliquity of Mars determined by Laskar et al. 2004 over the past 250 Myrs (a) and 26 Myrs (b). The different colored lines refer to different assumed values for the initial precession rate of the rotation axis of Mars which produces chaotically different results over long timescales (b), but nearly identical results in the past 26 Myrs (a). Thick lines give obliquity over a 1 Myr averaging window. Scenario "P000" is used as our model input.</abstract><pub>figshare</pub><doi>10.6084/m9.figshare.11978904</doi><orcidid>https://orcid.org/0000-0002-9947-346X</orcidid><oa>free_for_read</oa></addata></record> |
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title | Additional file 1 of Cold-based glaciation of Pavonis Mons, Mars: evidence for moraine deposition during glacial advance |
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