| Naslov: | Mid-Cretaceous calcarenite in stone products from the Roman colony of Emona, Regio X (modern Ljubljana, Slovenia) |
|---|
| Avtorji: | ID Brajkovič, Rok (Avtor)
ID Djurić, Bojan (Avtor)
ID Gerčar, David (Avtor)
ID Cvetko Tešović, Blanka (Avtor)
ID Rožič, Boštjan (Avtor)
ID Gale, Luka (Avtor) |
|---|
| Datoteke: |  PDF - Predstavitvena datoteka, prenos (25,02 MB)
MD5: DE73E6B9E96C54CB30FDA1381EDD00F9
PDF - Priloga, prenos (1,88 MB)
MD5: F6F8D9F7403A7B41529BF2F843A485FD
|
|---|
| Jezik: | Angleški jezik |
|---|
| Tipologija: | 1.01 - Izvirni znanstveni članek |
|---|
| Organizacija: |  GeoZS - Geološki zavod Slovenije
|
|---|
| Povzetek: | Over the course of studying stone products from theRoman colony of Emona (Regio X), stratigraphicallyundefined calcarenite that was used to make simplesepulchral and architectural stone products wasdetected. The calcarenite used is late Aptian to earlyCenomanian in age. The corresponding facies werefound in the Lower Flyschoid Formation outcroppingnear the town of Medvode, within the local radius ofEmona. The Roman quarry was likely located in thisarea near the Sava River. According to the collecteddata, the quarry was in operation mainly in the 1stcentury. |
|---|
| Ključne besede: | Cretaceous, microfacies, quarry production, Regio X, Roman time, stone products |
|---|
| Status publikacije: | Objavljeno |
|---|
| Verzija publikacije: | Objavljena publikacija |
|---|
| Datum objave: | 28.07.2022 |
|---|
| Leto izida: | 2022 |
|---|
| Št. strani: | str. 31-35 |
|---|
| Številčenje: | vol. 65, no. 1 |
|---|
| PID: | 20.500.12556/DiRROS-15384  |
|---|
| UDK: | 55:903/904 |
|---|
| ISSN pri članku: | 1475-4754 |
|---|
| DOI: | 10.1111/arcm.12814 |
|---|
| COBISS.SI-ID: | 118339843 |
|---|
| Datum objave v DiRROS: | 17.08.2022 |
|---|
| Število ogledov: | 1009 |
|---|
| Število prenosov: | 636 |
|---|
| Metapodatki: |    |
|---|
|
:
|
Kopiraj citat |
|---|
| | | | Objavi na: |  |
|---|
Postavite miškin kazalec na naslov za izpis povzetka. Klik na naslov izpiše
podrobnosti ali sproži prenos. |
