Journal article
Tridymite in a lacustrine mudstone in Gale Crater, Mars: Evidence for an explosive silicic eruption during the Hesperian
Earth and planetary science letters, Vol.594, 117694
09/15/2022
DOI: 10.1016/j.epsl.2022.117694
Abstract
The unexpected detection of ∼16 wt.% monoclinic tridymite, a high-temperature silica polymorph, within an otherwise lacustrine mudstone in Gale crater, Mars raises significant questions about its formation and the extent of magmatic evolution on that planet. The rock sample, analyzed by the X-ray diffractometer onboard the Curiosity rover, also contained feldspar, cristobalite, and opaline silica (±Si-glass). Monoclinic tridymite is extremely rare on Earth, and has only been discovered in silicic volcanic environments, high-temperature impact settings, and extraterrestrial rocks. We review the most common formation pathways of natural tridymite and run thermodynamical models to investigate possible formation mechanisms. We consider the broader context of the sample to propose a formation and transport mechanism based on: (1) the mineralogical assemblage of the mudstone and rocks in the vicinity, (2) the composition of the mudstone layer, and (3) the overall geological context. Based on the large amount of tridymite, the high SiO2 and low Al2O3 concentration of the mudstone, and the low temperature context within distal lacustrine mudstone, we propose that an explosive eruption released Si-rich ashes, which were deposited into Gale crater's watershed as a tridymite-rich ashfall along with cristobalite, feldspar, Ti-oxide, and Si-rich glass, when Gale was still a lake (Hesperian). The dissolution of Si-rich glass and mineral sorting during transport would have concentrated tridymite, caused opaline silica precipitation, and relatively lowered the Al2O3 concentration. This scenario implies that explosive volcanism on Mars occurred during the Hesperian and might not be restricted to basaltic eruptions, revealing the complexity of Mars magmatism.
•One layer of lacustrine mudstone in Gale contains high temperature silicic minerals.•Tridymite and plagioclase could have co-crystallized from a rhyolitic magma.•The rhyolitic magma is consistent with evolution of observed igneous rock sources.•The Buckskin sample is detrital from tridymite-bearing ash in Gale lake's watershed.•At least one silicic explosive eruption occurred on Mars in the Hesperian.
Details
- Title: Subtitle
- Tridymite in a lacustrine mudstone in Gale Crater, Mars: Evidence for an explosive silicic eruption during the Hesperian
- Creators
- V. Payré - Rice UniversityK.L. Siebach - Rice UniversityM.T. Thorpe - Rice UniversityP. Antoshechkina - Division of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, United States of AmericaE.B. Rampe - Johnson Space Center
- Resource Type
- Journal article
- Publication Details
- Earth and planetary science letters, Vol.594, 117694
- Publisher
- Elsevier B.V
- DOI
- 10.1016/j.epsl.2022.117694
- ISSN
- 0012-821X
- eISSN
- 1385-013X
- Language
- English
- Date published
- 09/15/2022
- Academic Unit
- Earth and Environmental Sciences
- Record Identifier
- 9984294926902771
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