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.

Gespeichert in:

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]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Übergeordnetes Werk:	In: Nature Communications - Nature Portfolio, 2016, 13(2022), 1, Seite 10
Übergeordnetes Werk:	volume:13 ; year:2022 ; number:1 ; pages:10

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.1038/s41467-022-33389-4

Katalog-ID:	DOAJ004408489

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author	Sebastian E. Lauro
spellingShingle	Sebastian E. Lauro misc Science misc Q Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines
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topic_title	Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines
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title	Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines
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title_full	Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines
author_sort	Sebastian E. Lauro
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author_browse	Sebastian E. Lauro Elena Pettinelli Graziella Caprarelli Jamaledin Baniamerian Elisabetta Mattei Barbara Cosciotti David E. Stillman Katherine M. Primm Francesco Soldovieri Roberto Orosei
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author-letter	Sebastian E. Lauro
doi_str_mv	10.1038/s41467-022-33389-4
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title_sort	using marsis signal attenuation to assess the presence of south polar layered deposit subglacial brines
title_auth	Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines
abstract	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.
abstractGer	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.
abstract_unstemmed	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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title_short	Using MARSIS signal attenuation to assess the presence of South Polar Layered Deposit subglacial brines
url	https://doi.org/10.1038/s41467-022-33389-4 https://doaj.org/article/b8a9a67e32504fb0a072611d38d0cce3 https://doaj.org/toc/2041-1723
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