The results of NM-PCI method applied on the analysed pebbles (supplementary material). Abbreviations: h = homogeneous; sh = shaded; m = mottled; sp = spotted; l = laminated; b = banded; st = streaked; c = conchoidal; s = subconchoidal; u = uneven; ND = non determined; Rad = radiolarians; Spi = sponge spiculae; For = foraminifers; FeOx = iron oxides; Org = organic matter. This dataset is cited in the text as Table 3.
Contributors:jose delgado rodrigues, Ferreira Pinto Ana Paula
S1: Deterioration patterns in elements of Ançã stone, in the Queluz gardens.
S2: Main portal of Loulé church and details of intense scaling.
S3: Limestone elements with scaling and deep cracking network in the main portal of Loulé church.
S4: Santa Cruz church, Coimbra, Portugal, in 1997, before the intervention.
S5 – Aspects of the intense spalling, scaling and deep fractures in limestone blocks of Porta Especiosa (Old Cathedral of Coimbra).
Data used for the paper entitled: "Rapid tools for assessing Building Heritage’s seismic vulnerability: a preliminary reliability analysis". Vulnerability assessment of structural units according to Lagormasino and Giovinazzi 2006 and Ferreira Vicente Varum 2010 are provided. Aggregate buildings vulnerability according to the Mazzotti 2008 (SISMA) methods are provided. Finally, Lagormasino and Giovinazzi 2006-based aggregate buildings vulnerability assessment methods according to Section 3.4 of the paper are offered, by including correlations with Mazzotti 2008.
DRIFT reference spectra of 10 synthetic organic pigments.
PR1: Para red, pure (Acros Organics)
PR3: Toluidinrot rein T 10004 (Farbwerke Franz Rasquin AG)
PR4: Permanentrot SG3H (Kali-Chemie AG Berlin)
PR6: Permanentrot hell (Kremer)
PO5: Permanentrot 2 G extra (G. Siegle & Co. GmbH)
PR83: Alizarin Krapplack dunkel (Schmincke)
PG1: Fanal Grün D 8330 (BASF)
PV2: Fanalviolett D 5460 (BASF)
PY12: Permanentgelb DHG (Hoechst)
PY3: Echtgelb rein R 10 G (Farbwerke Franz Rasquin AG)
The uploaded file contains single specimen results (declination and inclination) for the three sampled structures (Nulles, Cal Ticó-kiln, Cal Ticó-hearth and Camps de Mas Vidal) that were used to compute the corresponding archaeomagnetic mean directions. I suggest this data to be made available to the reader as supplementary material for online publication only. This has been also uploaded as e-component and it is cited in the manuscript as 'Supplementary Table'.