Roman Amphorae: a digital resource

University of Southampton, 2005. (updated 2014) https://doi.org/10.5284/1028192. How to cite using this DOI

Digital Object Identifiers

Digital Object Identifiers (DOIs) are persistent identifiers which can be used to consistently and accurately reference digital objects and/or content. The DOIs provide a way for the ADS resources to be cited in a similar fashion to traditional scholarly materials. More information on DOIs at the ADS can be found on our help page.

Citing this DOI

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https://doi.org/10.5284/1028192
Sample Citation for this DOI

University of Southampton (2014) Roman Amphorae: a digital resource [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1028192

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Resource identifiers

Digital Object Identifiers

Digital Object Identifiers (DOIs) are persistent identifiers which can be used to consistently and accurately reference digital objects and/or content. The DOIs provide a way for the ADS resources to be cited in a similar fashion to traditional scholarly materials. More information on DOIs at the ADS can be found on our help page.

Citing this DOI

The updated Crossref DOI Display guidelines recommend that DOIs should be displayed in the following format:

https://doi.org/10.5284/1028192
Sample Citation for this DOI

University of Southampton (2014) Roman Amphorae: a digital resource [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1028192

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Hammamet 2



Click on the image to see larger versions of each image.

Hammamet 2 Hammamet 2
Hammamet fabric

Visual characteristics

Relatively coarse-grained sandy fabric with visible quartz and limestone inclusions.

Petrology

All the fabrics are characterised by inclusions which are relatively coarse-grained, more or less abundant, and mainly composed of quartz, with microfossils and limestone fragments in subordinate quantities. The coarser quartz grains (up to more than 1 mm across) exhibit a rounded shape and opaque surfaces that are typical aeolian characteristics. There is some variability in textural and technical features. Two groups of fabrics (A and E) are more common than the rest. Group A shows an inclusion-poor matrix and a well-sorted (possibly added) temper, while in Group E the matrix is rich in quartz and foraminifera and the temper is moderately or poorly-sorted (Capelli, 2004). Claudio Capelli

 


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