Constraints on Martian Chronology from Meteorites
Keyword(s):
Martian meteorites provide the only direct constraints on the timing of Martian accretion, core formation, magmatic differentiation, and ongoing volcanism. While many radiogenic isotope chronometers have been applied to a wide variety of Martian samples, few, if any, techniques are immune to secondary effects from alteration and terrestrial weathering. This short review focuses on the most robust geochronometers that have been used to date Martian meteorites and geochemically model the differentiation of the planet, including 147Sm/143Nd, 146Sm/142Nd, 176Lu/176Hf, 182Hf/182W, and U-Th-Pb systematics.
2004 ◽
Vol 68
(13)
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pp. 2935-2946
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1999 ◽
Vol 63
(11-12)
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pp. 1865-1875
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2021 ◽
Vol 07
(01)
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pp. 003-007
1974 ◽
Vol 32
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pp. 532-533
1970 ◽
Vol 28
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pp. 494-495
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2019 ◽
Vol 47
(5)
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pp. 1393-1404
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