Hungaria Asteroid Family as the Source of Aubrite Meteorites
Matija \'Cuk, Brett Gladman, David Nesvorn\'y

TL;DR
This study investigates the hypothesis that aubrite meteorites originate from the Hungaria asteroid family, using orbital models and cosmic ray exposure ages to establish a connection between them.
Contribution
It provides evidence supporting Hungaria asteroids as the primary source of aubrite meteorites through orbital integration and cosmic ray exposure analysis.
Findings
Aubrites have long cosmic ray exposure ages indicating a delivery route from Hungarias.
Meteoroids from Hungarias reach Earth mainly via Yarkovsky drift without orbital resonance assistance.
Hungaria asteroid (434) is a strong candidate as the source of aubrites.
Abstract
The Hungaria asteroids are interior to the main asteroid belt, with semimajor axes between 1.8 and 2 AU, low eccentricities and inclinations of 16-35 degrees. Small asteroids in the Hungaria region are dominated by a collisional family associated with (434) Hungaria. The dominant spectral type of the Hungaria group is the E or X-type (Warner et al, 2009), mostly due to the E-type composition of Hungaria and its genetic family. It is widely believed the E-type asteroids are related to the aubrite meteorites, also known as enstatite achondrites (Gaffey et al, 1992). Here we explore the hypothesis that aubrites originate in the Hungaria family. In order to test this connection, we compare model Cosmic Ray Exposure ages from orbital integrations of model meteoroids with those of aubrites. We show that long CRE ages of aubrites (longest among stony meteorite groups) reflect the delivery…
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