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An electron microprobe study of P645/T390: Evidence for an Early Helladic III Lerna–Aegina connection

Identifieur interne : 000191 ( Main/Exploration ); précédent : 000190; suivant : 000192

An electron microprobe study of P645/T390: Evidence for an Early Helladic III Lerna–Aegina connection

Auteurs : Michael J. Dorais [États-Unis] ; Christine M. Shriner [États-Unis]

Source :

Geoarchaeology [ 0883-6353 ] ; 2002-12.

RBID : ISTEX:E4D6D5E99259F1138A57492FF5D736F43B0D3A41

English descriptors

KwdEn :
- Aegina, Aegina connection, Aeginetan, Aeginetan andesites, Aeginetan ware, American school, Amphibole, Amphibole compositions, Andesite, Batch dorais, Biotite, Biotite compositions, Classical studies, Clinopyroxene, Clinopyroxenes, Cultural interaction, Dacite, Dorais, Early helladic, Early phase, Fytikas, General formula, Geoarchaeology, Gray diamonds, Gray triangles, Helladic, International journal, Late helladic, Lerna, Lled, Lled circles, Magma, Methana, Methana biotites, Microprobe, Middle helladic, Middle helladic period, Milo, Na2o, Northern portion, Open circles, Plagioclase, Plagioclase compositions, Pleochroic, Poros, Poros biotites, Preclassical site, Pyroxene, Right batch evidence, Rock fragments, Rutter, Same minerals, Santorini, Saronic gulf, Shriner, Shriner figure, Sio2, Sio2 tio2, Subtle differences, Text base, Text dorais, Volcanic, Volcanic centers, Volcanic rocks, Ware.
Teeft :
- Aegina, Aegina connection, Aeginetan, Aeginetan andesites, Aeginetan ware, American school, Amphibole, Amphibole compositions, Andesite, Batch dorais, Biotite, Biotite compositions, Classical studies, Clinopyroxene, Clinopyroxenes, Cultural interaction, Dacite, Dorais, Early helladic, Early phase, Fytikas, General formula, Geoarchaeology, Gray diamonds, Gray triangles, Helladic, International journal, Late helladic, Lerna, Lled, Lled circles, Magma, Methana, Methana biotites, Microprobe, Middle helladic, Middle helladic period, Milo, Na2o, Northern portion, Open circles, Plagioclase, Plagioclase compositions, Pleochroic, Poros, Poros biotites, Preclassical site, Pyroxene, Right batch evidence, Rock fragments, Rutter, Same minerals, Santorini, Saronic gulf, Shriner, Shriner figure, Sio2, Sio2 tio2, Subtle differences, Text base, Text dorais, Volcanic, Volcanic centers, Volcanic rocks, Ware.

Abstract

Middle Helladic Aeginetan Ware is widely distributed throughout the Aegean. It is characterized by a “gold mica or volcanic ash” fabric and is abundant at Lerna on the Argive plain, Greece, in the Middle Helladic and Late Helladic I periods. A group of Early Helladic III ceramics at Lerna includes P645/T390, which also has a volcanic fabric. We have sampled all the major rock types of the separate volcanic episodes on Aegina, Methana, and Poros and analyzed the constituent minerals with the electron microprobe. These analyses provide a reference standard against which the mineralogy of P645/T390 and other potential Aeginetan wares can be compared. The compositions of amphibole, clinopyroxene, plagioclase, and biotite in P645/T390 are identical to the same minerals in dacites on Aegina, suggesting an origin on that island. Compositional mismatches with the minerals of Methana and Poros indicated the ceramic was not manufactured at these locations. This narrow‐necked jar represents the earliest occurrence of Aeginetan Ware on mainland Greece that has been confirmed by a quantitative method. © 2002 Wiley Periodicals, Inc.

Url:

https://api.istex.fr/document/E4D6D5E99259F1138A57492FF5D736F43B0D3A41/fulltext/pdf

DOI: 10.1002/gea.10041

Affiliations:

États-Unis
Indiana, Utah

Links toward previous steps (curation, corpus...)

to stream Istex, to step Corpus: 000284
to stream Istex, to step Curation: 000284
to stream Istex, to step Checkpoint: 000132
to stream Main, to step Merge: 000194
to stream Main, to step Curation: 000191

Le document en format XML

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<front><div type="abstract" xml:lang="en">Middle Helladic Aeginetan Ware is widely distributed throughout the Aegean. It is characterized by a “gold mica or volcanic ash” fabric and is abundant at Lerna on the Argive plain, Greece, in the Middle Helladic and Late Helladic I periods. A group of Early Helladic III ceramics at Lerna includes P645/T390, which also has a volcanic fabric. We have sampled all the major rock types of the separate volcanic episodes on Aegina, Methana, and Poros and analyzed the constituent minerals with the electron microprobe. These analyses provide a reference standard against which the mineralogy of P645/T390 and other potential Aeginetan wares can be compared. The compositions of amphibole, clinopyroxene, plagioclase, and biotite in P645/T390 are identical to the same minerals in dacites on Aegina, suggesting an origin on that island. Compositional mismatches with the minerals of Methana and Poros indicated the ceramic was not manufactured at these locations. This narrow‐necked jar represents the earliest occurrence of Aeginetan Ware on mainland Greece that has been confirmed by a quantitative method. © 2002 Wiley Periodicals, Inc.</div>
</front>
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An electron microprobe study of P645/T390: Evidence for an Early Helladic III Lerna–Aegina connection

An electron microprobe study of P645/T390: Evidence for an Early Helladic III Lerna–Aegina connection

Source :

English descriptors

Abstract

Links toward previous steps (curation, corpus...)

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri