Matches in SemOpenAlex for { <https://semopenalex.org/work/W3203045791> ?p ?o ?g. }
- W3203045791 endingPage "1932" @default.
- W3203045791 startingPage "1905" @default.
- W3203045791 abstract "Abstract Data returned by NASA’s Mars Science Laboratory Curiosity rover showed evidence for abundant secondary materials, including Fe‐oxides, phyllosilicates, and an amorphous component on and below Vera Rubin ridge in the Murray formation. We used equilibrium thermochemical modeling to test the hypothesis that altered sediments were deposited as detrital igneous grains and subsequently underwent diagenesis. Chemical compositions of the Murray formations’ altered components were calculated using data returned by the chemistry and mineralogy X‐ray diffraction instrument and the alpha particle X‐ray spectrometer on board Curiosity. Reaction of these alteration compositions with a CO 2 ‐poor and oxidizing dilute aqueous solution was modeled at 25–100 °C, with 10–50% Fe 3+ /Fe tot of the host rock. The modeled alteration assemblages included abundant phyllosilicates and Fe‐oxides at water‐to‐rock ratios >100. Modeled alteration abundances were directly comparable to observed abundances of hematite and clay minerals at a water‐to‐rock ratio of 10,000, for system temperatures of 50–100 °C with fluid pH ranging from 7.9 to 9.3. Modeling results suggest that the hematite–clay mineral assemblage is primarily the result of enhanced groundwater flow compared to the Sheepbed mudstone observed at Yellowknife Bay, and underwent further, localized alteration to produce the mineralogy observed by Curiosity." @default.
- W3203045791 created "2021-10-11" @default.
- W3203045791 creator A5012873516 @default.
- W3203045791 creator A5023965891 @default.
- W3203045791 creator A5025997294 @default.
- W3203045791 creator A5026106238 @default.
- W3203045791 creator A5031368661 @default.
- W3203045791 creator A5035578260 @default.
- W3203045791 creator A5044839502 @default.
- W3203045791 creator A5051403886 @default.
- W3203045791 creator A5058320863 @default.
- W3203045791 creator A5060508061 @default.
- W3203045791 creator A5070693444 @default.
- W3203045791 creator A5079092537 @default.
- W3203045791 creator A5087046444 @default.
- W3203045791 date "2021-09-26" @default.
- W3203045791 modified "2023-10-18" @default.
- W3203045791 title "Early diagenesis at and below Vera Rubin ridge, Gale crater, Mars" @default.
- W3203045791 cites W1484635710 @default.
- W3203045791 cites W1576917120 @default.
- W3203045791 cites W1596847809 @default.
- W3203045791 cites W1657971927 @default.
- W3203045791 cites W1830358639 @default.
- W3203045791 cites W1895144666 @default.
- W3203045791 cites W1966251031 @default.
- W3203045791 cites W1968326025 @default.
- W3203045791 cites W1981028812 @default.
- W3203045791 cites W1983614512 @default.
- W3203045791 cites W1983647645 @default.
- W3203045791 cites W1986859129 @default.
- W3203045791 cites W1988912694 @default.
- W3203045791 cites W1989241955 @default.
- W3203045791 cites W1994505906 @default.
- W3203045791 cites W1996653003 @default.
- W3203045791 cites W2011543988 @default.
- W3203045791 cites W2012554282 @default.
- W3203045791 cites W2013915611 @default.
- W3203045791 cites W2015649958 @default.
- W3203045791 cites W2017207473 @default.
- W3203045791 cites W2018287068 @default.
- W3203045791 cites W2025257083 @default.
- W3203045791 cites W2026006742 @default.
- W3203045791 cites W2028932647 @default.
- W3203045791 cites W2031077189 @default.
- W3203045791 cites W2040136115 @default.
- W3203045791 cites W2047283655 @default.
- W3203045791 cites W2049753999 @default.
- W3203045791 cites W2056139484 @default.
- W3203045791 cites W2057163772 @default.
- W3203045791 cites W2067551570 @default.
- W3203045791 cites W2072280901 @default.
- W3203045791 cites W2074253436 @default.
- W3203045791 cites W2083184196 @default.
- W3203045791 cites W2091321670 @default.
- W3203045791 cites W2093662773 @default.
- W3203045791 cites W2100420146 @default.
- W3203045791 cites W2100451067 @default.
- W3203045791 cites W2102090896 @default.
- W3203045791 cites W2111125339 @default.
- W3203045791 cites W2125610349 @default.
- W3203045791 cites W2126018044 @default.
- W3203045791 cites W2129892603 @default.
- W3203045791 cites W2137246201 @default.
- W3203045791 cites W2141153767 @default.
- W3203045791 cites W2142328350 @default.
- W3203045791 cites W2146376665 @default.
- W3203045791 cites W2146547148 @default.
- W3203045791 cites W2148965904 @default.
- W3203045791 cites W2152819168 @default.
- W3203045791 cites W2159049505 @default.
- W3203045791 cites W2159767575 @default.
- W3203045791 cites W2170411650 @default.
- W3203045791 cites W2314555703 @default.
- W3203045791 cites W2321341409 @default.
- W3203045791 cites W2336362230 @default.
- W3203045791 cites W2417054513 @default.
- W3203045791 cites W2503570975 @default.
- W3203045791 cites W2508133401 @default.
- W3203045791 cites W2509504714 @default.
- W3203045791 cites W2512700343 @default.
- W3203045791 cites W2549668206 @default.
- W3203045791 cites W2608846545 @default.
- W3203045791 cites W2612591151 @default.
- W3203045791 cites W2618300027 @default.
- W3203045791 cites W2620979631 @default.
- W3203045791 cites W2735137573 @default.
- W3203045791 cites W2748472866 @default.
- W3203045791 cites W2757065511 @default.
- W3203045791 cites W2771183068 @default.
- W3203045791 cites W2789655633 @default.
- W3203045791 cites W2793233300 @default.
- W3203045791 cites W2799301691 @default.
- W3203045791 cites W2805196455 @default.
- W3203045791 cites W2805284632 @default.
- W3203045791 cites W2891630101 @default.
- W3203045791 cites W2899995281 @default.
- W3203045791 cites W2901653527 @default.
- W3203045791 cites W2902484202 @default.