New Insights into Erg Chech 002 Analogues in the Main Belt from Near-Infrared Spectroscopy
arXiv:2603.24332 · doi:10.1016/j.icarus.2026.117050
Abstract
Erg Chech 002 is an andesitic meteorite that formed early in the Solar System's history, and that is thought to have been formed in the primitive crust of an early accreted and differentiated planetesimal. It shows unique spectral features, and no known asteroid spectral type was initially found to match with its compositional type. In the literature, asteroids (10537) 1991 RY16, (7472) Kumakiri and (14390) 1990 QP10 were found to show peculiar spectra, and were not classified in any known existing spectral class. These objects were hypothesised to be fragments of differentiated planetesimals. In a previous study, the Gaia Data Release 3 dataset of visible reflectance spectra of Solar System Objects was exploited to search for potential analogues of Erg Chech 002 in the main belt. As a result, 142 asteroids were found to potentially match this meteorite. In this work, we present NASA's IRTF near-infrared observations of 20 main belt asteroids found as potential analogues of Erg Chech 002. We classified these asteroids based on their visible-near-infrared spectra, then studied and compared their diagnostic spectral features with those of the laboratory spectra of Erg Chech 002. We classified 16 of the 20 observed asteroids as V-types, one as S-complex and one as A-type, and conclude that none of the observed objects match with Erg Chech 002. In addition, we show that asteroids (10537) 1991 RY16 and (14390) 1990 QP10 are good spectral matches to Erg Chech 002 based on the study of their diagnostic spectral features. Asteroid (7472) Kumakiri could match a more olivine-rich Erg Chech 002-like material, and cannot be completely ruled out as a match of the meteorite. This possible link between the meteorite and these asteroids is consistent with the theories regarding their formation, and these asteroids could be part of a new spectral class of andesitic bodies in the main belt.
References in corpus (26)
- Origin of water in the inner Solar System: Planetesimals scattered inward during Jupiter and Saturn's rapid gas accretion
- The Size Distributions of Asteroid Families in the SDSS Moving Object Catalog 4
- Turbulence sets the length scale for planetesimal formation: Local 2D simulations of streaming instability and planetesimal formation
- The Distribution of Basaltic Asteroids in the Main Belt
- A 4565 Myr old andesite from an extinct chondritic protoplanet
- An ancient and a primordial collisional family as the main sources of X-type asteroids of the inner Main Belt
- Gaia Data Release 3: Reflectance spectra of Solar System small bodies
- The common origin of family and non-family asteroids
- Twenty years of SpeX: Accuracy limits of spectral slope measurements in asteroid spectroscopy
- The Eos family halo
- Near-Earth asteroids spectroscopic survey at Isaac Newton Telescope
- A Spectroscopically Unique Main Belt Asteroid: 10537 (1991 RY16)
- The SPHEREx Satellite Mission
- Reconstructing the size distribution of the primordial Main Belt
- 53Mn-53Cr chronology and ε54Cr-Δ17O genealogy of Erg Chech 002: the oldest andesite in the Solar System
- Spectral properties of the largest asteroids associated with Taurid Complex
- The compositional diversity of non-Vesta basaltic asteroids
- Evolution of the parent body of enstatite (EL) chondrites
- Spectral analysis of basaltic asteroids observed by the Gaia space mission
- Gaia search for early-formed andesitic asteroidal crusts
- Distribution and spectrophotometric classification of basaltic asteroids
- Identification of a 4.3 billion year old asteroid family and planetesimal population in the Inner Main Belt
- Composition and origin of L5 Trojan asteroids of Mars: Insights from spectroscopy
- Spectral characterisation of 14 V-type candidate asteroids from the MOVIS catalogue
- Gaia and IRTF abundance of A-type main belt asteroids
- Primitive asteroids in the main belt, Cybele, and Hilda populations from Gaia DR3