FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2896796787> ?p ?o ?g. }

• W2896796787 endingPage "684" @default.
• W2896796787 startingPage "669" @default.
• W2896796787 abstract "Alteration of the uppermost surfaces of geologic materials is a pervasive process on planetary surfaces that is dependent upon factors including parent composition and the environment under which alteration is occurring. While rapid and pervasive in hot and humid climates on Earth, chemical weathering of rock surfaces has also been found to dominate in some of Earth's coldest and driest landscapes as well. Specifically, surfaces dominated by resistant fine-grained igneous rocks in the Antarctic preserve evidence of oxidative weathering processes, which represent the initial immature surface alteration processes that stagnate due to the lack of available water and kinetics necessary for the production of more mature alteration phases. In this study, we test the hypothesis that oxidative weathering also dominates the surfaces of sedimentary rocks throughout the Antarctic. We investigated the chemistry and mineralogy of a suite of sedimentary rocks from the Transantarctic Mountains ranging from fine-grained tuffs to coarse-grained sandstones and conglomerates. Our results show that, like the previously studied fine-grained igneous rocks in the Antarctic, sedimentary rocks generally showed only minor chemical weathering signatures at their surfaces relative to their interiors. However, unlike the igneous rocks in this earlier study, the sedimentary rocks exhibited a wide variety of non-systematic differences between surface and interior compositions. This variability of surface weathering signatures is equally as complex as the physical properties and compositions inherently present within these different sedimentary lithologies. Based on these analyses, it is apparent that oxidative weathering products do not dominate the surfaces of sedimentary rocks throughout the Transantarctic Mountains, which instead exhibit a wide array of weathering signatures that are likely dependent on both lithological and environmental factors. Considering that sedimentary lithologies are widespread across a significant fraction of the martian surface, our results suggest that observed alteration signatures limited to the surfaces of martian sedimentary rocks are most likely to be minor and to vary as a result of the lithological properties of the specific rock unit and not as a result of the widespread influences of the modern cold and dry climatic conditions." @default.
• W2896796787 created "2018-10-26" @default.
• W2896796787 creator A5003252649 @default.
• W2896796787 creator A5007151434 @default.
• W2896796787 creator A5012090680 @default.
• W2896796787 creator A5044839502 @default.
• W2896796787 creator A5048080132 @default.
• W2896796787 creator A5055127941 @default.
• W2896796787 creator A5065714714 @default.
• W2896796787 creator A5081146398 @default.
• W2896796787 creator A5086470303 @default.
• W2896796787 date "2019-02-01" @default.
• W2896796787 modified "2023-10-05" @default.
• W2896796787 title "Investigating the role of anhydrous oxidative weathering on sedimentary rocks in the Transantarctic Mountains and implications for the modern weathering of sedimentary lithologies on Mars" @default.
• W2896796787 cites W1488474916 @default.
• W2896796787 cites W1559613350 @default.
• W2896796787 cites W1852865358 @default.
• W2896796787 cites W1884974770 @default.
• W2896796787 cites W1965701586 @default.
• W2896796787 cites W1967942093 @default.
• W2896796787 cites W1978603365 @default.
• W2896796787 cites W1983571813 @default.
• W2896796787 cites W1990289290 @default.
• W2896796787 cites W1995066271 @default.
• W2896796787 cites W1998801327 @default.
• W2896796787 cites W1998894787 @default.
• W2896796787 cites W2002824385 @default.
• W2896796787 cites W2005760474 @default.
• W2896796787 cites W2009113483 @default.
• W2896796787 cites W2009211883 @default.
• W2896796787 cites W2011543988 @default.
• W2896796787 cites W2014589403 @default.
• W2896796787 cites W2026979800 @default.
• W2896796787 cites W2029401070 @default.
• W2896796787 cites W2032425981 @default.
• W2896796787 cites W2032451778 @default.
• W2896796787 cites W203831911 @default.
• W2896796787 cites W2054750651 @default.
• W2896796787 cites W2054904463 @default.
• W2896796787 cites W2054921843 @default.
• W2896796787 cites W2059288596 @default.
• W2896796787 cites W2064721136 @default.
• W2896796787 cites W2068952585 @default.
• W2896796787 cites W2070529447 @default.
• W2896796787 cites W2074797789 @default.
• W2896796787 cites W2078182311 @default.
• W2896796787 cites W2082289296 @default.
• W2896796787 cites W2083522166 @default.
• W2896796787 cites W2085469026 @default.
• W2896796787 cites W2089809480 @default.
• W2896796787 cites W2095127069 @default.
• W2896796787 cites W2095320760 @default.
• W2896796787 cites W2096961319 @default.
• W2896796787 cites W2104224684 @default.
• W2896796787 cites W2105510784 @default.
• W2896796787 cites W2112439085 @default.
• W2896796787 cites W2114331726 @default.
• W2896796787 cites W2123864149 @default.
• W2896796787 cites W2126889852 @default.
• W2896796787 cites W2128247628 @default.
• W2896796787 cites W2137246201 @default.
• W2896796787 cites W2143014585 @default.
• W2896796787 cites W2143444312 @default.
• W2896796787 cites W2146376665 @default.
• W2896796787 cites W2147312569 @default.
• W2896796787 cites W2156378353 @default.
• W2896796787 cites W2161883428 @default.
• W2896796787 cites W2253881385 @default.
• W2896796787 cites W2462912627 @default.
• W2896796787 cites W2563285874 @default.
• W2896796787 cites W2612591151 @default.
• W2896796787 cites W2620979631 @default.
• W2896796787 cites W2621189146 @default.
• W2896796787 cites W4252835680 @default.
• W2896796787 doi "https://doi.org/10.1016/j.icarus.2018.10.007" @default.
• W2896796787 hasPublicationYear "2019" @default.
• W2896796787 type Work @default.
• W2896796787 sameAs 2896796787 @default.
• W2896796787 citedByCount "8" @default.
• W2896796787 countsByYear W28967967872019 @default.
• W2896796787 countsByYear W28967967872020 @default.
• W2896796787 countsByYear W28967967872021 @default.
• W2896796787 crossrefType "journal-article" @default.
• W2896796787 hasAuthorship W2896796787A5003252649 @default.
• W2896796787 hasAuthorship W2896796787A5007151434 @default.
• W2896796787 hasAuthorship W2896796787A5012090680 @default.
• W2896796787 hasAuthorship W2896796787A5044839502 @default.
• W2896796787 hasAuthorship W2896796787A5048080132 @default.
• W2896796787 hasAuthorship W2896796787A5055127941 @default.
• W2896796787 hasAuthorship W2896796787A5065714714 @default.
• W2896796787 hasAuthorship W2896796787A5081146398 @default.
• W2896796787 hasAuthorship W2896796787A5086470303 @default.
• W2896796787 hasBestOaLocation W28967967871 @default.
• W2896796787 hasConcept C121332964 @default.
• W2896796787 hasConcept C122792734 @default.
• W2896796787 hasConcept C127313418 @default.
• W2896796787 hasConcept C17409809 @default.
• W2896796787 hasConcept C187320778 @default.

• next