Low-Temperature Aqueous Alteration of Chondrites.
Martin R Lee1, Conel M O'D Alexander2, Addi Bischoff3
1School of Geographical & Earth Sciences, University of Glasgow, Glasgow, G12 8QQ UK.
Summary
Early Solar System small bodies experienced liquid water alteration, as evidenced by chondritic meteorites. This review examines the processes, products, and timing of these low-temperature aqueous alteration reactions.
Area of Science:
- Cosmochemistry
- Planetary Science
- Geology
Background:
- Chondritic meteorites provide crucial evidence for early liquid water interactions on small bodies.
- Understanding aqueous alteration is key to deciphering the conditions of the early Solar System.
Purpose of the Study:
- To review the processes, products, and timings of low-temperature aqueous alteration in various chondrites and asteroids.
- To synthesize insights into alteration conditions, fluid properties, and reaction chronologies.
Main Methods:
- Analysis of chondritic lithologies, mineralogy, and petrology.
- Physicochemical modeling and hydrothermal experiments.
- Fluid inclusion analysis and isotope geochemistry (Mn-Cr, I-Xe).
Main Results:
- Detailed characterization of mineralogy and petrology in hydrated chondrites and dark clasts.
- Insights into the nature of aqueous fluids and their reactions with parent body materials.
- Chronological constraints on aqueous alteration events using radiometric dating.
Conclusions:
- Aqueous alteration was a significant process in the early Solar System, shaping the composition of small bodies.
- This review consolidates current knowledge on the conditions, evolution, and timing of these critical early processes.
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