FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2094222242> ?p ?o ?g. }

• W2094222242 endingPage "199" @default.
• W2094222242 startingPage "199" @default.
• W2094222242 abstract "Research Article| March 01, 2003 Antarctic permafrost: An analogue for water and diagenetic minerals on Mars Warren W. Dickinson; Warren W. Dickinson 1Antarctic Research Centre, Victoria University, P.O. Box 600, Wellington, New Zealand Search for other works by this author on: GSW Google Scholar Michael R. Rosen Michael R. Rosen 2Institute of Geological and Nuclear Sciences, Private Bag 2000, Taupo, New Zealand Search for other works by this author on: GSW Google Scholar Geology (2003) 31 (3): 199–202. https://doi.org/10.1130/0091-7613(2003)031<0199:APAAFW>2.0.CO;2 Article history received: 19 Aug 2002 rev-recd: 06 Nov 2002 accepted: 08 Nov 2002 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 Warren W. Dickinson, Michael R. Rosen; Antarctic permafrost: An analogue for water and diagenetic minerals on Mars. Geology 2003;; 31 (3): 199–202. doi: https://doi.org/10.1130/0091-7613(2003)031<0199:APAAFW>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 At high altitudes (>1000 m) throughout the Dry Valleys, Antarctica, liquid water is rare, yet ground ice, which may be millions of years old, is pervasive in glacial sediments and bedrock. The origin of this ice is different from its arctic and alpine counterparts and may be similar to water on Mars. We present chemical and isotopic analyses of Antarctic ground ice from cores of Sirius Group sediments at Table Mountain in the Dry Valleys. These data, together with the presence of diagenetic calcite and chabazite in the frozen sediments, indicate that the ice and minerals accumulated over long periods of time from atmospheric water vapor and brine films formed on the surface of the ground. This analogy indicates that ferric-bearing minerals could precipitate under present conditions in the Martian soil. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2094222242 created "2016-06-24" @default.
• W2094222242 creator A5019453857 @default.
• W2094222242 creator A5026615721 @default.
• W2094222242 date "2003-01-01" @default.
• W2094222242 modified "2023-10-14" @default.
• W2094222242 title "Antarctic permafrost: An analogue for water and diagenetic minerals on Mars" @default.
• W2094222242 cites W1533667087 @default.
• W2094222242 cites W1975801642 @default.
• W2094222242 cites W1981295645 @default.
• W2094222242 cites W1997821159 @default.
• W2094222242 cites W2017289858 @default.
• W2094222242 cites W2021490749 @default.
• W2094222242 cites W2031005465 @default.
• W2094222242 cites W2036051649 @default.
• W2094222242 cites W2048437887 @default.
• W2094222242 cites W2056411484 @default.
• W2094222242 cites W2061325259 @default.
• W2094222242 cites W2066606864 @default.
• W2094222242 cites W2067434913 @default.
• W2094222242 cites W2078571499 @default.
• W2094222242 cites W2081890296 @default.
• W2094222242 cites W2083317216 @default.
• W2094222242 cites W2109113863 @default.
• W2094222242 cites W2123486627 @default.
• W2094222242 cites W2123514375 @default.
• W2094222242 cites W2132118841 @default.
• W2094222242 cites W2150494204 @default.
• W2094222242 cites W2162311525 @default.
• W2094222242 cites W2602606476 @default.
• W2094222242 cites W4256468369 @default.
• W2094222242 doi "https://doi.org/10.1130/0091-7613(2003)031<0199:apaafw>2.0.co;2" @default.
• W2094222242 hasPublicationYear "2003" @default.
• W2094222242 type Work @default.
• W2094222242 sameAs 2094222242 @default.
• W2094222242 citedByCount "84" @default.
• W2094222242 countsByYear W20942222422012 @default.
• W2094222242 countsByYear W20942222422013 @default.
• W2094222242 countsByYear W20942222422014 @default.
• W2094222242 countsByYear W20942222422015 @default.
• W2094222242 countsByYear W20942222422016 @default.
• W2094222242 countsByYear W20942222422017 @default.
• W2094222242 countsByYear W20942222422018 @default.
• W2094222242 countsByYear W20942222422019 @default.
• W2094222242 countsByYear W20942222422020 @default.
• W2094222242 countsByYear W20942222422021 @default.
• W2094222242 countsByYear W20942222422022 @default.
• W2094222242 countsByYear W20942222422023 @default.
• W2094222242 crossrefType "journal-article" @default.
• W2094222242 hasAuthorship W2094222242A5019453857 @default.
• W2094222242 hasAuthorship W2094222242A5026615721 @default.
• W2094222242 hasConcept C111368507 @default.
• W2094222242 hasConcept C121332964 @default.
• W2094222242 hasConcept C127313418 @default.
• W2094222242 hasConcept C130452526 @default.
• W2094222242 hasConcept C15098985 @default.
• W2094222242 hasConcept C151730666 @default.
• W2094222242 hasConcept C161191863 @default.
• W2094222242 hasConcept C166957645 @default.
• W2094222242 hasConcept C199360897 @default.
• W2094222242 hasConcept C2778447006 @default.
• W2094222242 hasConcept C2778805511 @default.
• W2094222242 hasConcept C41008148 @default.
• W2094222242 hasConcept C518008717 @default.
• W2094222242 hasConcept C83260615 @default.
• W2094222242 hasConcept C87355193 @default.
• W2094222242 hasConcept C95457728 @default.
• W2094222242 hasConceptScore W2094222242C111368507 @default.
• W2094222242 hasConceptScore W2094222242C121332964 @default.
• W2094222242 hasConceptScore W2094222242C127313418 @default.
• W2094222242 hasConceptScore W2094222242C130452526 @default.
• W2094222242 hasConceptScore W2094222242C15098985 @default.
• W2094222242 hasConceptScore W2094222242C151730666 @default.
• W2094222242 hasConceptScore W2094222242C161191863 @default.
• W2094222242 hasConceptScore W2094222242C166957645 @default.
• W2094222242 hasConceptScore W2094222242C199360897 @default.
• W2094222242 hasConceptScore W2094222242C2778447006 @default.
• W2094222242 hasConceptScore W2094222242C2778805511 @default.
• W2094222242 hasConceptScore W2094222242C41008148 @default.
• W2094222242 hasConceptScore W2094222242C518008717 @default.
• W2094222242 hasConceptScore W2094222242C83260615 @default.
• W2094222242 hasConceptScore W2094222242C87355193 @default.
• W2094222242 hasConceptScore W2094222242C95457728 @default.
• W2094222242 hasIssue "3" @default.
• W2094222242 hasLocation W20942222421 @default.
• W2094222242 hasOpenAccess W2094222242 @default.
• W2094222242 hasPrimaryLocation W20942222421 @default.
• W2094222242 hasRelatedWork W1824336683 @default.
• W2094222242 hasRelatedWork W1975043628 @default.
• W2094222242 hasRelatedWork W1982366144 @default.
• W2094222242 hasRelatedWork W1998906033 @default.
• W2094222242 hasRelatedWork W2349454828 @default.
• W2094222242 hasRelatedWork W2900526884 @default.
• W2094222242 hasRelatedWork W2941001766 @default.
• W2094222242 hasRelatedWork W3157142868 @default.
• W2094222242 hasRelatedWork W4252886933 @default.
• W2094222242 hasRelatedWork W4297535931 @default.
• W2094222242 hasVolume "31" @default.

• next