Healed cracks in iceberg ice

DOI	Trouver le DOI : https://doi.org/10.3189/172756502781831179
Auteur	Rechercher : Barrette, Paul D.Identifiant ORCID : https://orcid.org/0000-0002-0975-8884; Rechercher : Jordaan, Ian J.
Format	Texte, Article
Résumé	A noticeable trait of iceberg ice is the presence of several sets of planar features cross-cutting each other at various angles. Close-up views of these features show that they consist of an array of individual air inclusions that differ in size, shape and spatial distribution. In none of the cases resolvable at the scale of our obervations were these inclusions physically linked to form a continuous fracture plane, although they may have originated as such. All postdate the formation of ice veins.
Date de publication	2002-12-01
Dans	Journal of Glaciology 48, nº 163 (1 décembre 2002) : 587–591.
Langue	anglais
Numéro NPARC	12338035
Exporter la notice	Exporter en format RIS
Signaler une correction	Signaler une correction (s'ouvre dans un nouvel onglet)
Identificateur de l’enregistrement	9ef84915-d63f-42b2-9a8c-9c6daa2fa9cf
Enregistrement créé	2009-09-10
Enregistrement modifié	2021-03-26