Titre :

The fusion crust of the Winchcombe meteorite: A preserved record of atmospheric entry processes

Auteur(s) :

Genge, Matthew J. [Auteur]
Imperial College London
Alesbrook, Luke [Auteur]
Almeida, Natasha V. [Auteur]
Bates, Helena C. [Auteur]
Bland, Phil A. [Auteur]
Boyd, Mark R. [Auteur]
Imperial College London
Burchell, Mark J. [Auteur]
Collins, Gareth S. [Auteur]
Imperial College London
Cornwell, Luke T. [Auteur]
Daly, Luke [Auteur]
Devillepoix, Hadrien A. R. [Auteur]
Van Ginneken, Matthias [Auteur]
Greshake, Ansgar [Auteur]
Hallatt, Daniel [Auteur]
Unité Matériaux et Transformations - UMR 8207 [UMET]
Hamann, Christopher [Auteur]
Hecht, Lutz [Auteur]
Jenkins, Laura E. [Auteur]
Johnson, Diane [Auteur]
Jones, Rosie [Auteur]
King, Ashley J. [Auteur]
Mansour, Haithem [Auteur]
McMullan, Sarah [Auteur]
Mitchell, Jennifer T. [Auteur]
Rollinson, Gavyn [Auteur]
Russell, Sara S. [Auteur]
Schröder, Christian [Auteur]
Stephen, Natasha R. [Auteur]
Suttle, Martin D. [Auteur]
Tandy, Jon D. [Auteur]
Trimby, Patrick [Auteur]
Sansom, Eleanor K. [Auteur]
Spathis, Vassilia [Auteur]
Willcocks, Francesca M. [Auteur]
Wozniakiewicz, Penelope J. [Auteur]

Titre de la revue :

Meteoritics & Planetary Science

Nom court de la revue :

Meteorit & Planet Sci

Éditeur :

Wiley

Date de publication :

2023-01-02

ISSN :

1945-5100

Discipline(s) HAL :

Chimie/Matériaux
Physique [physics]/Matière Condensée [cond-mat]/Science des matériaux [cond-mat.mtrl-sci]
Physique [physics]/Physique [physics]/Géophysique [physics.geo-ph]
Physique [physics]/Astrophysique [astro-ph]
Planète et Univers [physics]/Astrophysique [astro-ph]
Planète et Univers [physics]/Sciences de la Terre

Résumé en anglais : [en]

AbstractFusion crusts form during the atmospheric entry heating of meteorites and preserve a record of the conditions that occurred during deceleration in the atmosphere. The fusion crust of the Winchcombe meteorite closely ...
Lire la suite >AbstractFusion crusts form during the atmospheric entry heating of meteorites and preserve a record of the conditions that occurred during deceleration in the atmosphere. The fusion crust of the Winchcombe meteorite closely resembles that of other stony meteorites, and in particular CM2 chondrites, since it is dominated by olivine phenocrysts set in a glassy mesostasis with magnetite, and is highly vesicular. Dehydration cracks are unusually abundant in Winchcombe. Failure of this weak layer is an additional ablation mechanism to produce large numbers of particles during deceleration, consistent with the observation of pulses of plasma in videos of the Winchcombe fireball. Calving events might provide an observable phenomenon related to meteorites that are particularly susceptible to dehydration. Oscillatory zoning is observed within olivine phenocrysts in the fusion crust, in contrast to other meteorites, perhaps owing to temperature fluctuations resulting from calving events. Magnetite monolayers are found in the crust, and have also not been previously reported, and form discontinuous strata. These features grade into magnetite rims formed on the external surface of the crust and suggest the trapping of surface magnetite by collapse of melt. Magnetite monolayers may be a feature of meteorites that undergo significant degassing. Silicate warts with dendritic textures were observed and are suggested to be droplets ablated from another stone in the shower. They, therefore, represent the first evidence for intershower transfer of ablation materials and are consistent with the other evidence in the Winchcombe meteorite for unusually intense gas loss and ablation, despite its low entry velocity.Lire moins >

Langue :

Anglais

Comité de lecture :

Oui

Audience :

Internationale

Vulgarisation :

Non

Établissement(s) :

Université de Lille
CNRS
INRAE
ENSCL

Collections :

• Unité Matériaux et Transformations (UMET) - UMR 8207

Équipe(s) de recherche :

Matériaux Terrestres et Planétaires

Date de dépôt :

2024-01-06T08:57:17Z
2024-01-26T10:36:15Z