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Temperature and composition of the mantle sources of martian basalts as constrained by MAGMARS, a new melting model for FeO-rich peridotite

Collinet, Max und Plesa, Ana-Catalina und Ruedas Gomez, Thomas und Schwinger, Sabrina und Breuer, Doris (2021) Temperature and composition of the mantle sources of martian basalts as constrained by MAGMARS, a new melting model for FeO-rich peridotite. AGU Fall Meeting, 2021-12-13 - 2021-12-17, New Orleans USA & Online Everywhere.

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Offizielle URL: https://agu.confex.com/agu/fm21/meetingapp.cgi/Paper/942655

Kurzfassung

The martian surface is predominantly covered by FeO-rich basalts and their alteration products. Several samples, either analyzed in situ by rovers or recovered as meteorites, might represent primitive (i.e. near-primary) basaltic melts that can shed light on the mineralogy, the bulk composition, and the temperature of their mantle sources. We recently developed a new melting model, called MAGMARS, that can predict the melt compositions of FeO-rich mantles and the martian mantle in particular (Collinet et al., submitted to JGR:P). It represents a more accurate alternative to pMELTS (Ghiorso et al., 2002, G3), which systematically overestimates the FeO and MgO content of martian melts and underestimates the SiO2 content (by up to 8 wt.%). MAGMARS can simulate near-fractional and batch melting of various mantle compositions. For example, MAGMARS can produce melts identical to the Adirondack-class basalts by near-fractional melting, between 2.3 and 1.7 GPa, of a depleted mantle with a potential temperature (Tp) of 1390°C (~7 wt.% melt fraction). For this study, MAGMARS is applied to all other martian basalts from which the primary melt compositions can be inferred in order to constrain their mantle sources: the Columbia hills basalts, igneous rocks from Gale crater, shergottites, nakhlites and Northwest Africa (NWA) 7034/7533. We find that a few basaltic clasts in the pre-Noachian polymict regolith breccia NWA 7034/7533 are the only samples with bulk compositions that could represent melts derived from a primitive mantle. The Columbia hills basalts (Gusev crater), alkali-rich rocks from Gale crater, nakhlites and enriched shergottites are most easily reproduced by melting depleted mantle reservoirs that were re-fertilized to different degrees in alkalis by fluids or melts (i.e. metasomatized sources). Most martian basalts, with the exception of depleted shergottites, can be produced from martian mantle reservoirs with Mg# comprised between 75 and 81. From this sample set, the melting conditions of the martian mantle seem to remain relatively stable through time (Tp = 1400 ± 100 ºC and P = 2 ± 0.5 GPa) but the depleted nature of all mantle sources sampled after the pre-Noachian points towards an early crust-mantle differentiation.

elib-URL des Eintrags:https://elib.dlr.de/148224/
Dokumentart:Konferenzbeitrag (Poster)
Titel:Temperature and composition of the mantle sources of martian basalts as constrained by MAGMARS, a new melting model for FeO-rich peridotite
Autoren:
AutorenInstitution oder E-Mail-AdresseAutoren-ORCID-iDORCID Put Code
Collinet, Maxmax.collinet (at) dlr.dehttps://orcid.org/0000-0002-8791-9751NICHT SPEZIFIZIERT
Plesa, Ana-CatalinaAna.Plesa (at) dlr.dehttps://orcid.org/0000-0003-3366-7621NICHT SPEZIFIZIERT
Ruedas Gomez, ThomasThomas.Ruedas (at) dlr.deNICHT SPEZIFIZIERTNICHT SPEZIFIZIERT
Schwinger, SabrinaSabrina.Schwinger (at) dlr.deNICHT SPEZIFIZIERTNICHT SPEZIFIZIERT
Breuer, DorisDoris.Breuer (at) dlr.dehttps://orcid.org/0000-0001-9019-5304NICHT SPEZIFIZIERT
Datum:2021
Referierte Publikation:Nein
Open Access:Nein
Gold Open Access:Nein
In SCOPUS:Nein
In ISI Web of Science:Nein
Seitenbereich:P55B-1926
Status:veröffentlicht
Stichwörter:Martian basalts, Source composition and temperature, Melting model
Veranstaltungstitel:AGU Fall Meeting
Veranstaltungsort:New Orleans USA & Online Everywhere
Veranstaltungsart:internationale Konferenz
Veranstaltungsbeginn:13 Dezember 2021
Veranstaltungsende:17 Dezember 2021
HGF - Forschungsbereich:Luftfahrt, Raumfahrt und Verkehr
HGF - Programm:Raumfahrt
HGF - Programmthema:Erforschung des Weltraums
DLR - Schwerpunkt:Raumfahrt
DLR - Forschungsgebiet:R EW - Erforschung des Weltraums
DLR - Teilgebiet (Projekt, Vorhaben):R - Exploration des Sonnensystems, R - Projekt InSight - HP3
Standort: Berlin-Adlershof
Institute & Einrichtungen:Institut für Planetenforschung > Planetenphysik
Hinterlegt von: Plesa, Dr. Ana-Catalina
Hinterlegt am:12 Jan 2022 07:57
Letzte Änderung:24 Apr 2024 20:46

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