Water and volatile element accretion to the inner planets
Water and volatile element accretion to the inner planets
Date
2018-02
Authors
Sarafian, Adam
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DOI
10.1575/1912/9490
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Keywords
Solar system
Water
Meteorites
Water
Meteorites
Abstract
This thesis investigates the timing and source(s) of water and volatile elements to the inner solar
system by studying the basaltic meteorites angrites and eucrites. In chapters 2 and 3, I present the
results from angrite meteorites. Chapter 2 examines the water and volatile element content of the
angrite parent body and I suggest that some water and other volatile elements accreted to inner
solar system bodies by ~2 Myr after the start of the solar system. Chapter 3 examines the D/H of
this water and I suggest it is derived from carbonaceous chondrites. Chapter 4, 5, 6, and 7
addresses eucrite meteorites. Chapter 4 expands on existing models to explain geochemical
trends observed in eucrites. In Chapter 5, I examine the water and F content of the eucrite parent
body, 4 Vesta. In chapter 6, I determine the source of water for 4 Vesta and determine that
carbonaceous chondrites delivered water to this body. Chapter 7 discusses degassing on 4 Vesta
while it was forming.
Description
Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the
Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution February 2018
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Citation
Sarafian, A. (2018). Water and volatile element accretion to the inner planets [Doctoral thesis, Massachusetts Institute of Technology and Woods Hole Oceanographic Institution]. Woods Hole Open Access Server. https://doi.org/10.1575/1912/9490