FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000554912> ?p ?o ?g. }

• W2000554912 endingPage "240" @default.
• W2000554912 startingPage "224" @default.
• W2000554912 abstract "Veins containing carbonates, hydrous silicates, and sulfates that occur within and between grains of augite and olivine in the Nakhla meteorite are good evidence for the former presence of liquid water in the Martian crust. Aqueous solutions gained access to grain interiors via narrow fractures, and those fractures within olivine whose walls were oriented close to (001) were preferentially widened by etching along [001]. This orientation selective dissolution may have been due to the presence within olivine of shock-formed [001](100) and [001]{110} screw dislocations. The duration of etching is likely to have been brief, possibly less than a year, and the solutions responsible were sufficiently cool and reducing that laihunite did not form and Fe liberated from the olivine was not immediately oxidized. The pores within olivine were mineralized in sequence by siderite, nanocrystalline smectite, a Fe-Mg phyllosilicate, and then gypsum, whereas only the smectite occurs within augite. The nanocrystalline smectite was deposited as submicrometer thick layers on etched vein walls, and solution compositions varied substantially between and sometimes during precipitation of each layer. Together with microcrystalline gypsum the Fe-Mg phyllosilicate crystallized as water briefly returned to some of the veins following desiccation fracturing of the smectite. These results show that etching of olivine enhanced the porosity and permeability of the nakhlite parent rock and that dissolution and secondary mineralization took place within the same near-static aqueous system." @default.
• W2000554912 created "2016-06-24" @default.
• W2000554912 creator A5021225531 @default.
• W2000554912 creator A5030664166 @default.
• W2000554912 creator A5069358509 @default.
• W2000554912 creator A5072707395 @default.
• W2000554912 creator A5091780915 @default.
• W2000554912 date "2013-01-28" @default.
• W2000554912 modified "2023-09-25" @default.
• W2000554912 title "Evidence for silicate dissolution on Mars from the Nakhla meteorite" @default.
• W2000554912 cites W1493376842 @default.
• W2000554912 cites W1515758462 @default.
• W2000554912 cites W1521981032 @default.
• W2000554912 cites W1966780453 @default.
• W2000554912 cites W1972077034 @default.
• W2000554912 cites W1972791064 @default.
• W2000554912 cites W1993674353 @default.
• W2000554912 cites W1997360422 @default.
• W2000554912 cites W1998592620 @default.
• W2000554912 cites W2000823471 @default.
• W2000554912 cites W2002746788 @default.
• W2000554912 cites W2003125744 @default.
• W2000554912 cites W2007260609 @default.
• W2000554912 cites W2016528533 @default.
• W2000554912 cites W2030992183 @default.
• W2000554912 cites W2031797934 @default.
• W2000554912 cites W2032748541 @default.
• W2000554912 cites W2038403070 @default.
• W2000554912 cites W2038845141 @default.
• W2000554912 cites W2048235086 @default.
• W2000554912 cites W2057060944 @default.
• W2000554912 cites W2059610826 @default.
• W2000554912 cites W2067218581 @default.
• W2000554912 cites W2069389056 @default.
• W2000554912 cites W2075601040 @default.
• W2000554912 cites W2084590963 @default.
• W2000554912 cites W2087439424 @default.
• W2000554912 cites W2095906449 @default.
• W2000554912 cites W2107535381 @default.
• W2000554912 cites W2109918785 @default.
• W2000554912 cites W2114057247 @default.
• W2000554912 cites W2125291350 @default.
• W2000554912 cites W2141190941 @default.
• W2000554912 cites W2144096366 @default.
• W2000554912 cites W2145092699 @default.
• W2000554912 cites W2158391305 @default.
• W2000554912 cites W2899794452 @default.
• W2000554912 cites W4239725541 @default.
• W2000554912 doi "https://doi.org/10.1111/maps.12053" @default.
• W2000554912 hasPublicationYear "2013" @default.
• W2000554912 type Work @default.
• W2000554912 sameAs 2000554912 @default.
• W2000554912 citedByCount "32" @default.
• W2000554912 countsByYear W20005549122013 @default.
• W2000554912 countsByYear W20005549122014 @default.
• W2000554912 countsByYear W20005549122015 @default.
• W2000554912 countsByYear W20005549122016 @default.
• W2000554912 countsByYear W20005549122017 @default.
• W2000554912 countsByYear W20005549122018 @default.
• W2000554912 countsByYear W20005549122019 @default.
• W2000554912 countsByYear W20005549122020 @default.
• W2000554912 countsByYear W20005549122021 @default.
• W2000554912 countsByYear W20005549122022 @default.
• W2000554912 countsByYear W20005549122023 @default.
• W2000554912 crossrefType "journal-article" @default.
• W2000554912 hasAuthorship W2000554912A5021225531 @default.
• W2000554912 hasAuthorship W2000554912A5030664166 @default.
• W2000554912 hasAuthorship W2000554912A5069358509 @default.
• W2000554912 hasAuthorship W2000554912A5072707395 @default.
• W2000554912 hasAuthorship W2000554912A5091780915 @default.
• W2000554912 hasBestOaLocation W20005549122 @default.
• W2000554912 hasConcept C121332964 @default.
• W2000554912 hasConcept C127313418 @default.
• W2000554912 hasConcept C127413603 @default.
• W2000554912 hasConcept C130635790 @default.
• W2000554912 hasConcept C151730666 @default.
• W2000554912 hasConcept C17409809 @default.
• W2000554912 hasConcept C199289684 @default.
• W2000554912 hasConcept C2776277684 @default.
• W2000554912 hasConcept C2776283581 @default.
• W2000554912 hasConcept C2777335606 @default.
• W2000554912 hasConcept C2779181077 @default.
• W2000554912 hasConcept C2779870107 @default.
• W2000554912 hasConcept C2780364934 @default.
• W2000554912 hasConcept C40212044 @default.
• W2000554912 hasConcept C42360764 @default.
• W2000554912 hasConcept C62074269 @default.
• W2000554912 hasConcept C87355193 @default.
• W2000554912 hasConcept C88380143 @default.
• W2000554912 hasConceptScore W2000554912C121332964 @default.
• W2000554912 hasConceptScore W2000554912C127313418 @default.
• W2000554912 hasConceptScore W2000554912C127413603 @default.
• W2000554912 hasConceptScore W2000554912C130635790 @default.
• W2000554912 hasConceptScore W2000554912C151730666 @default.
• W2000554912 hasConceptScore W2000554912C17409809 @default.
• W2000554912 hasConceptScore W2000554912C199289684 @default.
• W2000554912 hasConceptScore W2000554912C2776277684 @default.
• W2000554912 hasConceptScore W2000554912C2776283581 @default.

• next