Search results for "limestone"

showing 5 items of 45 documents

Comparison between NMR and MIP in characterizing porosity of limestone used in Cultural Heritage,

2015

Limestone with different porosity are used extensively as a sculptural and architectural stone in artistic-architectural field. As it is known, this kind of material is subjected to physico-chemical decay that involves the loss of surface and in-depth cohesion [1]. Consolidation interventions are performed in order to preserve building and decorative surfaces of architectural monuments, to reduce their degradation rate and to improve cohesion and adhesion in the stone [2]. Porosity of stone and pore size distribution are important factors to evaluate the effectiveness of a consolidation treatment and they are normally performed using a single technique such as mercury intrusion porosimetry,…

noneNMR MIP LimestoneSettore FIS/07 - Fisica Applicata(Beni Culturali Ambientali Biol.e Medicin)
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Guano-related phosphate-rich minerals in European caves

2019

International audience; Guano is a typical deposit found in caves derived from the excretions of bats and in minor cases of birds. These organic deposits decompose and form a series of acid fluids and gases that can interact with the minerals, sediments, and rocks present in the cave. Over sixty phosphates are known and described from caves, but guano decay also often leads to the formation of nitrates and sulfates. In this study twenty-two European caves were investigated for their guano-related secondary minerals. Using various analytical techniques, seventeen phosphates, along with one sulfate (gypsum), were recognized as secondary products of guano decay. Among those minerals, some are …

phosphatesGypsum010504 meteorology & atmospheric sciencesQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaGeochemistrybat guanocave minerals phosphate bat guanoengineering.material010502 geochemistry & geophysics01 natural sciencessecondary cave mineralsApatitechemistry.chemical_compoundCavesecondary cave minerals phosphates minerogenesis limestone caves bat guanominerogenesisBiology (General)Sulfatelimestone cavephosphate0105 earth and related environmental sciencesEarth-Surface Processescave mineralsQE1-996.5geographygeography.geographical_feature_categoryMineralSettore GEO/07 - Petrologia E PetrografiaGeology15. Life on landPhosphatehumanitiessecondary cave mineralchemistryminerogenesivisual_artlimestone cavesGuanoengineeringvisual_art.visual_art_mediumPyrite[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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THE MOSAIC OF THE FRIGIDARIUM OF “VILLA BONANNO” IN PALERMO: MINERALOGICAL AND PETROGRAPHIC ANALYSES FOR IN SITU CONSERVATION AND RESTORATION INTERVE…

2018

The topic of this study was the mineralogical and petrographic characterization of bedding mortars (made of different layers) and tesserae of Roman age (3rd century A.D.), taken from the mosaic of the Frigidarium of “Villa Bonanno”, brought to light by archaeological excavations conducted in the historical centre of Palermo. The collected samples have been analysed by thin-section optical microscopy (PLM), and scanning electron microscopy coupled with energy dispersive spectrometry (SEM-EDS). The study was aimed to define the “recipe” (composition of aggregate and binder, aggregate size distribution, aggregate/binder ratio), in order to assess the provenance of raw m…

restorationlimestone tesseraeRoman mosaicsSicilySicily Roman mosaics bedding mortars limestone tesserae restorationbedding mortarsSettore GEO/09 -Georis. Miner.e Appl.Mineral.-Petrogr. per l'Ambi.ed i B.Cult.
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A well-preserved crinoid stem in a building stone (Early Carboniferous, Mississippian) at Maastricht, the Netherlands

2017

An exceptionally well-preserved and long crinoid stem is exposed on a slab of decorative Lower Carboniferous (Mississippian) limestone in front of an opticianʼs in Maastricht-Wyck, the Netherlands. The pluricolumnal is incomplete, but is c. 176.5 mm long by at least 7.0 mm wide and with a broad axial canal. The column is heteromorphic, N3231323. The specimen most likely represents a cladid or monobathrid that was preserved parallel to bedding.

taphonomyurban geologylimestonePalaeozoicBulletin of the Mizunami Fossil Museum
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An Upper Mississippian echinoderm microfauna from the Genicera Formation of northern León (Carboniferous, Cantabrian Mountains, N Spain)

2020

For the first time an echinoderm microfauna is recorded from the cephalopod limestone facies (‘griotte facies’) of the lower Carboniferous (Mississippian) Genicera Fm. (Alba Fm.). The formation is widespread in the Cantabrian Mountains in NW Spain, but the ossicles are from some sections in the surroundings of the Bernesga valley in northern León. They have been derived from insoluble acetic acid residues from samples of the upper and especially of the uppermost part of the formation (Canalón Mb. and Millaró Beds). The microfauna include taxonomically treated wheel-shaped ossicles, sieve-plates and rods of holothurians, goniodonts of ophiocistioids, and ophiuroid and stenuroid skeletal elem…

viséan serpukhovian cephalopod limestone carbonate microfacies echinoderm ossicles taxonomy.PaleozoicbiologyApodidaPaleontologybiology.organism_classificationQE701-760SerpukhovianPaleontologyEchinodermViséanCarboniferousMicrofaunaOphiocistioideaGeologySpanish Journal of Palaeontology
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