FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2071143397> ?p ?o ?g. }

• W2071143397 endingPage "297" @default.
• W2071143397 startingPage "289" @default.
• W2071143397 abstract "Lithology and physical properties of strata exposed at the Earth's surface have direct influence on the erosion and geomorphic expression of landforms. While this is well known on our planet, examples on Mars are just coming to light among the tens of thousands of airphoto-quality images (resolutions 1.5–12 m/pixel) acquired since 1997 by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC). Specific examples occur among martian north polar layered materials, which MOC images reveal are divided into two distinct stratigraphic units: a lower, dark-toned layered unit and a younger, upper, lighter-toned layered unit. The lower unit is less resistant to wind erosion than the upper unit. The upper unit most likely consists of stratified dust and ice, while the lower unit contains abundant, poorly cemented sand. Sand is more easily mobilized by wind than dust; the lower resistance to erosion of the lower unit results from the presence of sand. Where wind erosion in polar troughs has penetrated to the lower unit, geomorphic change has proceeded more rapidly: sand has been liberated from the lower unit, and arcuate scarps have formed as the upper unit has been undermined. Wind erosion of the lower unit thus influences the geomorphology of the north polar region; this result likely explains the genesis of the large polar trough, Chasma Boreale, and the relations between dunes and arcuate scarps that have puzzled investigators for nearly three decades. The properties of the stratigraphic units suggest that the upper limit for the amount of water contained in the north polar layered materials may be 30–50% less than previously estimated." @default.
• W2071143397 created "2016-06-24" @default.
• W2071143397 creator A5011232501 @default.
• W2071143397 creator A5014235466 @default.
• W2071143397 creator A5059312154 @default.
• W2071143397 creator A5059880500 @default.
• W2071143397 creator A5073712139 @default.
• W2071143397 date "2003-06-01" @default.
• W2071143397 modified "2023-10-11" @default.
• W2071143397 title "Mars landscape evolution: influence of stratigraphy on geomorphology in the north polar region" @default.
• W2071143397 cites W1970341234 @default.
• W2071143397 cites W1972641867 @default.
• W2071143397 cites W1978538549 @default.
• W2071143397 cites W1979983657 @default.
• W2071143397 cites W1992643007 @default.
• W2071143397 cites W1995653938 @default.
• W2071143397 cites W2009065106 @default.
• W2071143397 cites W2012249569 @default.
• W2071143397 cites W2020905882 @default.
• W2071143397 cites W2025663379 @default.
• W2071143397 cites W2036789192 @default.
• W2071143397 cites W2043400586 @default.
• W2071143397 cites W2045323482 @default.
• W2071143397 cites W2073051806 @default.
• W2071143397 cites W2074589855 @default.
• W2071143397 cites W2080598070 @default.
• W2071143397 cites W2081421069 @default.
• W2071143397 cites W2083504119 @default.
• W2071143397 cites W2086231674 @default.
• W2071143397 cites W2086697948 @default.
• W2071143397 cites W2101661856 @default.
• W2071143397 cites W2124919065 @default.
• W2071143397 cites W2126449252 @default.
• W2071143397 cites W2167420953 @default.
• W2071143397 cites W2168798314 @default.
• W2071143397 cites W2047344177 @default.
• W2071143397 doi "https://doi.org/10.1016/s0169-555x(02)00262-3" @default.
• W2071143397 hasPublicationYear "2003" @default.
• W2071143397 type Work @default.
• W2071143397 sameAs 2071143397 @default.
• W2071143397 citedByCount "46" @default.
• W2071143397 countsByYear W20711433972012 @default.
• W2071143397 countsByYear W20711433972013 @default.
• W2071143397 countsByYear W20711433972014 @default.
• W2071143397 countsByYear W20711433972015 @default.
• W2071143397 countsByYear W20711433972017 @default.
• W2071143397 countsByYear W20711433972018 @default.
• W2071143397 countsByYear W20711433972019 @default.
• W2071143397 countsByYear W20711433972021 @default.
• W2071143397 countsByYear W20711433972022 @default.
• W2071143397 countsByYear W20711433972023 @default.
• W2071143397 crossrefType "journal-article" @default.
• W2071143397 hasAuthorship W2071143397A5011232501 @default.
• W2071143397 hasAuthorship W2071143397A5014235466 @default.
• W2071143397 hasAuthorship W2071143397A5059312154 @default.
• W2071143397 hasAuthorship W2071143397A5059880500 @default.
• W2071143397 hasAuthorship W2071143397A5073712139 @default.
• W2071143397 hasConcept C108497213 @default.
• W2071143397 hasConcept C109281948 @default.
• W2071143397 hasConcept C114679195 @default.
• W2071143397 hasConcept C114793014 @default.
• W2071143397 hasConcept C121332964 @default.
• W2071143397 hasConcept C122792734 @default.
• W2071143397 hasConcept C123157820 @default.
• W2071143397 hasConcept C127313418 @default.
• W2071143397 hasConcept C151730666 @default.
• W2071143397 hasConcept C180093795 @default.
• W2071143397 hasConcept C2778600265 @default.
• W2071143397 hasConcept C77928131 @default.
• W2071143397 hasConcept C83260615 @default.
• W2071143397 hasConcept C87355193 @default.
• W2071143397 hasConceptScore W2071143397C108497213 @default.
• W2071143397 hasConceptScore W2071143397C109281948 @default.
• W2071143397 hasConceptScore W2071143397C114679195 @default.
• W2071143397 hasConceptScore W2071143397C114793014 @default.
• W2071143397 hasConceptScore W2071143397C121332964 @default.
• W2071143397 hasConceptScore W2071143397C122792734 @default.
• W2071143397 hasConceptScore W2071143397C123157820 @default.
• W2071143397 hasConceptScore W2071143397C127313418 @default.
• W2071143397 hasConceptScore W2071143397C151730666 @default.
• W2071143397 hasConceptScore W2071143397C180093795 @default.
• W2071143397 hasConceptScore W2071143397C2778600265 @default.
• W2071143397 hasConceptScore W2071143397C77928131 @default.
• W2071143397 hasConceptScore W2071143397C83260615 @default.
• W2071143397 hasConceptScore W2071143397C87355193 @default.
• W2071143397 hasIssue "3-4" @default.
• W2071143397 hasLocation W20711433971 @default.
• W2071143397 hasOpenAccess W2071143397 @default.
• W2071143397 hasPrimaryLocation W20711433971 @default.
• W2071143397 hasRelatedWork W2037372977 @default.
• W2071143397 hasRelatedWork W2170616010 @default.
• W2071143397 hasRelatedWork W2171124862 @default.
• W2071143397 hasRelatedWork W2177755041 @default.
• W2071143397 hasRelatedWork W2999839492 @default.
• W2071143397 hasRelatedWork W3048022058 @default.
• W2071143397 hasRelatedWork W3127115430 @default.
• W2071143397 hasRelatedWork W3136062579 @default.
• W2071143397 hasRelatedWork W4213050598 @default.

• next