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艾瑞達尼亞湖

维基百科,自由的百科全书
(重定向自埃里达尼亚湖

埃里达尼亚湖(Eridania Lake)是一座理论上曾存在过的火星湖泊,面积约110万平方公里。它位于马丁谷溢出河道的源头,并延伸至埃里达尼亚区法厄同区[1]。随着厄里达尼亚湖在诺亚纪晚期的逐渐干涸,它分裂成一系列较小的湖泊[2][3][4][5]

后来的火星专用小型侦察影像频谱仪(CRISM)发现了厚度超过400米的厚厚沉积物层,所包含的矿物质有皂石(saponite)、滑石皂石(talc-saponite)、富铁云母 (如海绿石-绿脱石)、铁和镁质蛇纹石、碳酸镁-铁-钙及硫化铁。硫化铁可能形成于被火山喷发加热的深水中,这种被归类为热液的过程可能是生命开始的地方[6]

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参考文献

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  1. ^ Rossman, P. Irwin III; Ted A. Maxwell; Alan D. Howard; Robert A. Craddock; David W. Leverington. A Large Paleolake Basin at the Head of Ma'adim Vallis, Mars. Science. 21 June 2002, 296 (5576): 2209–2212. Bibcode:2002Sci...296.2209I. PMID 12077414. S2CID 23390665. doi:10.1126/science.1071143. 
  2. ^ de Pablo, M. A.; Fairén, A. G.; Márquez, A. The Geology of Atlantis Basin, Mars, and Its Astrobiological Interest (PDF). 35th Lunar and Planetary Science Conference, 15–19 March 2004, League City, Texas. 3 March 2004: 1223 [2013-04-23]. Bibcode:2004LPI....35.1223D. abstract no.1223. (原始内容存档 (PDF)于2012-02-17). 
  3. ^ Cabrol, N. and E. Grin (eds.). 2010. Lakes on Mars. Elsevier. NY.
  4. ^ Rossman, R.; et al. A large paleolake basin at the head of Ma'adim Vallis, Mars. Science. 2002, 296 (5576): 2209–2212. Bibcode:2002Sci...296.2209R. PMID 12077414. S2CID 23390665. doi:10.1126/science.1071143. 
  5. ^ HiRISE | Chaos in Eridania Basin (ESP_037142_1430). [2021-09-26]. (原始内容存档于2017-09-16). 
  6. ^ Joseph R. Michalski, Eldar Z. Noe Dobrea, Paul B. Niles & Javier Cuadros. Ancient hydrothermal seafloor deposits in Eridania basin on Mars. Nature Communications. 10 July 2017, 8: 15978. Bibcode:2017NatCo...815978M. PMC 5508135可免费查阅. PMID 28691699. doi:10.1038/ncomms15978. 

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