Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines
MARSIS attenuation and thermal data confirm that liquid brines are the most plausible source for the bright reflections at the base of the South Polar Layered Deposits. Such results also justify why SHARAD does not penetrate to the base of the ice.
Autor*in: |
Sebastian E. Lauro [verfasserIn] Elena Pettinelli [verfasserIn] Graziella Caprarelli [verfasserIn] Jamaledin Baniamerian [verfasserIn] Elisabetta Mattei [verfasserIn] Barbara Cosciotti [verfasserIn] David E. Stillman [verfasserIn] Katherine M. Primm [verfasserIn] Francesco Soldovieri [verfasserIn] Roberto Orosei [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2022 |
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Übergeordnetes Werk: |
In: Nature Communications - Nature Portfolio, 2016, 13(2022), 1, Seite 10 |
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Übergeordnetes Werk: |
volume:13 ; year:2022 ; number:1 ; pages:10 |
Links: |
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DOI / URN: |
10.1038/s41467-022-33389-4 |
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Katalog-ID: |
DOAJ004408489 |
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10.1038/s41467-022-33389-4 doi (DE-627)DOAJ004408489 (DE-599)DOAJb8a9a67e32504fb0a072611d38d0cce3 DE-627 ger DE-627 rakwb eng Sebastian E. Lauro verfasserin aut Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier MARSIS attenuation and thermal data confirm that liquid brines are the most plausible source for the bright reflections at the base of the South Polar Layered Deposits. Such results also justify why SHARAD does not penetrate to the base of the ice. Science Q Elena Pettinelli verfasserin aut Graziella Caprarelli verfasserin aut Jamaledin Baniamerian verfasserin aut Elisabetta Mattei verfasserin aut Barbara Cosciotti verfasserin aut David E. Stillman verfasserin aut Katherine M. Primm verfasserin aut Francesco Soldovieri verfasserin aut Roberto Orosei verfasserin aut In Nature Communications Nature Portfolio, 2016 13(2022), 1, Seite 10 (DE-627)626457688 (DE-600)2553671-0 20411723 nnns volume:13 year:2022 number:1 pages:10 https://doi.org/10.1038/s41467-022-33389-4 kostenfrei https://doaj.org/article/b8a9a67e32504fb0a072611d38d0cce3 kostenfrei https://doi.org/10.1038/s41467-022-33389-4 kostenfrei https://doaj.org/toc/2041-1723 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_211 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2110 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 13 2022 1 10 |
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10.1038/s41467-022-33389-4 doi (DE-627)DOAJ004408489 (DE-599)DOAJb8a9a67e32504fb0a072611d38d0cce3 DE-627 ger DE-627 rakwb eng Sebastian E. Lauro verfasserin aut Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier MARSIS attenuation and thermal data confirm that liquid brines are the most plausible source for the bright reflections at the base of the South Polar Layered Deposits. Such results also justify why SHARAD does not penetrate to the base of the ice. Science Q Elena Pettinelli verfasserin aut Graziella Caprarelli verfasserin aut Jamaledin Baniamerian verfasserin aut Elisabetta Mattei verfasserin aut Barbara Cosciotti verfasserin aut David E. Stillman verfasserin aut Katherine M. Primm verfasserin aut Francesco Soldovieri verfasserin aut Roberto Orosei verfasserin aut In Nature Communications Nature Portfolio, 2016 13(2022), 1, Seite 10 (DE-627)626457688 (DE-600)2553671-0 20411723 nnns volume:13 year:2022 number:1 pages:10 https://doi.org/10.1038/s41467-022-33389-4 kostenfrei https://doaj.org/article/b8a9a67e32504fb0a072611d38d0cce3 kostenfrei https://doi.org/10.1038/s41467-022-33389-4 kostenfrei https://doaj.org/toc/2041-1723 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_211 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2110 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 13 2022 1 10 |
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10.1038/s41467-022-33389-4 doi (DE-627)DOAJ004408489 (DE-599)DOAJb8a9a67e32504fb0a072611d38d0cce3 DE-627 ger DE-627 rakwb eng Sebastian E. Lauro verfasserin aut Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier MARSIS attenuation and thermal data confirm that liquid brines are the most plausible source for the bright reflections at the base of the South Polar Layered Deposits. Such results also justify why SHARAD does not penetrate to the base of the ice. Science Q Elena Pettinelli verfasserin aut Graziella Caprarelli verfasserin aut Jamaledin Baniamerian verfasserin aut Elisabetta Mattei verfasserin aut Barbara Cosciotti verfasserin aut David E. Stillman verfasserin aut Katherine M. Primm verfasserin aut Francesco Soldovieri verfasserin aut Roberto Orosei verfasserin aut In Nature Communications Nature Portfolio, 2016 13(2022), 1, Seite 10 (DE-627)626457688 (DE-600)2553671-0 20411723 nnns volume:13 year:2022 number:1 pages:10 https://doi.org/10.1038/s41467-022-33389-4 kostenfrei https://doaj.org/article/b8a9a67e32504fb0a072611d38d0cce3 kostenfrei https://doi.org/10.1038/s41467-022-33389-4 kostenfrei https://doaj.org/toc/2041-1723 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_211 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2110 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 13 2022 1 10 |
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using marsis signal attenuation to assess the presence of south polar layered deposit subglacial brines |
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Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines |
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MARSIS attenuation and thermal data confirm that liquid brines are the most plausible source for the bright reflections at the base of the South Polar Layered Deposits. Such results also justify why SHARAD does not penetrate to the base of the ice. |
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MARSIS attenuation and thermal data confirm that liquid brines are the most plausible source for the bright reflections at the base of the South Polar Layered Deposits. Such results also justify why SHARAD does not penetrate to the base of the ice. |
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MARSIS attenuation and thermal data confirm that liquid brines are the most plausible source for the bright reflections at the base of the South Polar Layered Deposits. Such results also justify why SHARAD does not penetrate to the base of the ice. |
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Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines |
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score |
7.4003944 |