5 results on '"Brilli, M."'
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2. Black limestone used in antiquity: recognizing the limestone of Teos.
- Author
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Brilli, M., Giustini, F., and Kadıoğlu, M.
- Subjects
- *
LIMESTONE , *STONE , *BLACK - Abstract
This paper documents the petrographic and isotopic characteristics of some black limestones that were exploited in antiquity near the ancient site of Teos in Ionia (south‐western Anatolia, Turkey). The best‐quality black limestone of Teos is represented by a series of step‐cut‐shaped blocks situated north of the Seferihisar–Sığacık road, destined to be exported and used for architectural elements. The techniques used to study these blocks allow possible identification of the origin of Teos in ancient black stone artefacts. Nevertheless, petrographic and geochemical investigation on some black limestones that outcrop in the area near Teos has not firmly identified the quarry fronts from which these blocks were quarried away, but it supports the known hypothesis that Teian black limestones were found and quarried in conjunction with the Africano marble. [ABSTRACT FROM AUTHOR]
- Published
- 2019
- Full Text
- View/download PDF
3. Growth of fi ssure ridge travertines from geothermal springs of Denizli Basin, western Turkey
- Author
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De Filippis, L., Faccenna, C., Billi, A., Anzalone, E., Brilli, M., Özkul, Mehmet, Soligo, M., Tuccimei, P., and Villa, I.M.
- Subjects
Structural observations ,uranium series dating ,carbon isotope ,Turkey ,Temporal relationships ,Stratigraphy ,Geochronology ,Central axis ,Quaternary ,Denizli Basin ,Isotopes ,travertine ,U-series ,stable isotope ,hydrothermal deposit ,sill ,Sloping surfaces ,oxygen isotope ,Paleoclimates ,Rare earth elements ,Stable isotopes ,lithostratigraphy ,Tectonics ,Limestone ,thermal spring ,geothermal system ,Seismic event ,Deposits ,fissure ,Feeding circuit - Abstract
Fissure ridge travertines grown from geothermal springs of Denizli Basin, southwestern Turkey, are investigated through stratigraphic, structural, geochemical, and geochronological methods, with the aim of understanding the growth of these elongate mound-shaped structures. Two main types of travertine deposits are recognized: (1) bedded travertines, which grew as fl owstone on sloping surfaces and form the bulk of fi ssure ridges, and (2) banded travertines, which grew as veins within the bedded travertine chiefly along its central feeding conduit. Stratigraphic and structural observations shed light on the bedded-banded travertine relationships, where the banded features grew through successive accretion phases, crosscutting the bedded travertine or forming sill-like structures. The bedded and banded travertines alternated their growth, as demonstrated by complicated crosscutting relationships and by the upward suture, in places, of banded travertine by bedded travertine that was, in turn, crosscut by younger banded travertine. The bedded travertine is often tilted away from the central axis of the fi ssure ridge, thus leaving more room for the central banded travertine to form. U-series ages confi rm the bedded-banded travertine temporal relationships and show that the growth of the studied fi ssure ridges lasted up to several tens of thousands of years during Quaternary time. The banded travertine was deposited mainly during cold events, possibly in coincidence with seismic events that might have triggered the outfl ow of deep geothermal fl uids. C and O stable isotope and rare earth element data indicate a shallow feeding circuit for the studied structures with a fl uid component deriving from a deeper geothermal circuit. A crack-and-seal mechanism of fi ssure ridge growth is proposed, modulated by the interplay of local and regional infl uencing factors and mechanisms such as geothermal fl uid discharge, paleoclimate, tectonics, and the progressive tilting of bedded travertine limbs over a soft substratum creating the necessary space for the central veins to grow. © 2012 Geological Society of America.
- Published
- 2012
4. Determining the provenance of black limestone artifacts using petrography, isotopes and EPR techniques: the case of the monument of Bocco
- Author
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Brilli, M., Conti, L., Giustini, F., Occhiuzzi, M., Pensabene, P., and De Nuccio, M.
- Subjects
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ANTIQUITIES provenance , *LIMESTONE , *PETROLOGY , *STABLE isotopes , *ELECTRON paramagnetic resonance , *MONUMENTS , *OXYGEN isotopes - Abstract
Abstract: This paper investigates the provenance of the black limestone of the monument known as Bocco, named after the king of Mauretania who presented Silla with this work as a sign of his submission to the power of Rome. A multi-method approach, comprising petrographic observations, carbon and oxygen isotope composition and electron paramagnetic resonance (EPR) spectra characteristics, was used for this purpose. The monument is part of a reconstruction of a rectangular base (approx. 8 × 2 m) which is likely to have served as the base for a bronze statuary group and is currently composed of six blocks of limestone whose exterior is engraved with a fine frieze. The results of the different analyses were compared with the data of a published database of the most important black limestone quarries exploited during Roman times in the Mediterranean area. The petrographic and physico-chemical parameters did not prove to be very effective in determining the provenance of the black limestone of Bocco; the isotopes result even raised some uncertainty as to whether all six blocks came from the same quarry, though this doubt was dispelled by the EPR data and, above all, by the evident petrographic similarity between them. Differences in the isotopic composition of the various blocks may be due to an in situ rock alteration process caused by interaction with an aqueous fluid. It was, however, impossible to determine with certainty the origin of the material of the stone artifact using the database available; it is possible that the black limestone of Bocco came from an ancient quarry that is likely to be located in north western Africa but has not yet been uncovered. An alternative hypothesis, according to which the limestone used for the monument of Bocco came from the ancient quarry of Ain el Ksir, one of the Tunisian quarries present in the database, is also discussed. [Copyright &y& Elsevier]
- Published
- 2011
- Full Text
- View/download PDF
5. Black limestones used in antiquity: the petrographic, isotopic and EPR database for provenance determination
- Author
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Brilli, M., Antonelli, F., Giustini, F., Lazzarini, L., and Pensabene, P.
- Subjects
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LIMESTONE , *ANTIQUITIES , *PETROLOGY , *ISOTOPES , *ELECTRON paramagnetic resonance , *STATISTICAL correlation - Abstract
Abstract: We compiled a database of some of the most important black limestone quarries used in Roman times to be able to determine the provenance of ancient artifacts. For this purpose, we adopted a multimethod approach using the techniques commonly applied to study the provenance of white marbles: petrographic observations, carbon and oxygen isotope composition, electron paramagnetic resonance (EPR) spectra characteristics. Few black limestones were quarried and traded in ancient times; indeed, the importance of most of these quarries was restricted to the areas in which they were located. In this work, we selected a limited number of quarries that produced material believed to have been exported and used throughout the Mediterranean area; most of the quarries selected are found in northern Tunisia, i.e. the Roman proconsular Africa: Djebel Oust, Djebel Azeiz, Ain al Ksir and (presumably) Thala. The “Nero Chiota” limestone quarried on the Aegean island of Chios (Greece) was also included in the database. The petrographic and physicochemical parameters used to distinguish between the different provenances of the black limestones we selected proved to be very effective. The isotope and EPR numerical data processed by means of discriminant analysis proved to be almost decisive in determining the provenance of unknown artifacts. However, the combination of these parameters with the petrographic data definitely provides a more organic characterization. [Copyright &y& Elsevier]
- Published
- 2010
- Full Text
- View/download PDF
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