دورية أكاديمية
Aqueously altered igneous rocks sampled on the floor of Jezero crater, Mars.
العنوان: | Aqueously altered igneous rocks sampled on the floor of Jezero crater, Mars. |
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المؤلفون: | Farley, KA, Stack, KM, Shuster, DL, Horgan, BHN, Hurowitz, JA, Tarnas, JD, Simon, JI, Sun, VZ, Scheller, EL, Moore, KR, McLennan, SM, Vasconcelos, PM, Wiens, RC, Treiman, AH, Mayhew, LE, Beyssac, O, Kizovski, TV, Tosca, NJ, Williford, KH, Crumpler, LS, Beegle, LW, Bell, JF, Ehlmann, BL, Liu, Y, Maki, JN, Schmidt, ME, Allwood, AC, Amundsen, HEF, Bhartia, R, Bosak, T, Brown, AJ, Clark, BC, Cousin, A, Forni, O, Gabriel, TSJ, Goreva, Y, Gupta, S, Hamran, S-E, Herd, CDK, Hickman-Lewis, K, Johnson, JR, Kah, LC, Kelemen, PB, Kinch, KB, Mandon, L, Mangold, N, Quantin-Nataf, C, Rice, MS, Russell, PS, Sharma, S, Siljeström, S, Steele, A, Sullivan, R, Wadhwa, M, Weiss, BP, Williams, AJ, Wogsland, BV, Willis, PA, Acosta-Maeda, TA, Beck, P, Benzerara, K, Bernard, S, Burton, AS, Cardarelli, EL, Chide, B, Clavé, E, Cloutis, EA, Cohen, BA, Czaja, AD, Debaille, V, Dehouck, E, Fairén, AG, Flannery, DT, Fleron, SZ, Fouchet, T, Frydenvang, J, Garczynski, BJ, Gibbons, EF, Hausrath, EM, Hayes, AG, Henneke, J, Jørgensen, JL, Kelly, EM, Lasue, J, Le Mouélic, S, Madariaga, JM, Maurice, S, Merusi, M, Meslin, P-Y, Milkovich, SM, Million, CC, Moeller, RC, Núñez, JI, Ollila, AM, Paar, G, Paige, DA, Pedersen, DAK, Pilleri, P, Pilorget, C, Pinet, PC, Rice, JW, Royer, C, Sautter, V, Schulte, M, Sephton, MA, Sharma, SK, Sholes, SF, Spanovich, N, St Clair, M, Tate, CD, Uckert, K, VanBommel, SJ, Yanchilina, AG, Zorzano, M-P |
بيانات النشر: | American Association for the Advancement of Science (AAAS) Department of Earth Sciences //dx.doi.org/10.1126/science.abo2196 Science |
سنة النشر: | 2022 |
المجموعة: | Apollo - University of Cambridge Repository |
مصطلحات موضوعية: | 37 Earth Sciences, 51 Physical Sciences, 5101 Astronomical Sciences, 3703 Geochemistry, 3705 Geology |
الوصف: | The Perseverance rover landed in Jezero crater, Mars, to investigate ancient lake and river deposits. We report observations of the crater floor, below the crater's sedimentary delta, finding that the floor consists of igneous rocks altered by water. The lowest exposed unit, informally named Séítah, is a coarsely crystalline olivine-rich rock, which accumulated at the base of a magma body. Magnesium-iron carbonates along grain boundaries indicate reactions with carbon dioxide-rich water under water-poor conditions. Overlying Séítah is a unit informally named Máaz, which we interpret as lava flows or the chemical complement to Séítah in a layered igneous body. Voids in these rocks contain sulfates and perchlorates, likely introduced by later near-surface brine evaporation. Core samples of these rocks have been stored aboard Perseverance for potential return to Earth. |
نوع الوثيقة: | article in journal/newspaper |
وصف الملف: | Print-Electronic; application/pdf |
اللغة: | English |
العلاقة: | https://www.repository.cam.ac.uk/handle/1810/340800Test |
DOI: | 10.17863/CAM.88236 |
الإتاحة: | https://doi.org/10.17863/CAM.88236Test https://www.repository.cam.ac.uk/handle/1810/340800Test |
حقوق: | All Rights Reserved ; http://www.rioxx.net/licenses/all-rights-reservedTest |
رقم الانضمام: | edsbas.20AA4E11 |
قاعدة البيانات: | BASE |
DOI: | 10.17863/CAM.88236 |
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