Die geschichtlichen Fresken in den Arkaden des Hofgartens zu München /

Mode of access: Internet.

Appendice aux Lettres d'un antiquare à un artiste sur l'emploi della peinture historique murale dans la décoration des temples et des autres édifices publics ou particulière chez les Grecs et les Romains.

Mode of access: Internet.

Art and common sense /

Art and common sense.--Ingres: a pilgrimage to Montauban.--The magic of mere paint.--Contemporary European painting.--A note of French military painting.--The post-impressionist illusion.--A memorable exhibition.--Whistler.--Sargent.--Spanish art in Spain and elsewhere.--Secular types in Italian mural decoration.--Rodin.--Four leaders in American architecture.--J. Pierpont Morgan as a collector.

Kievo-Sofiĭskiĭ sobor : izsli͡e︡dovanie drevneĭ mozaicheskoĭ i freskovoĭ zhivopisi /

Includes bibliographical footnotes.

Romance literature pamphlets.

A collection of miscellaneous pamphlets.

La cappella degli Scrovegni e gli affreschi di Giotto in essa dipinti /

Includes bibliographical references.

L'oeuvre de P.-V. Galland,

At head of title: Le peinture décorative au XIXe siècle.

Ecclesiae anglicanae trophæa, siue, Sanctor̄ martyrum, qui pro Christo catholicæq̀ fidei veritate asserenda : antiquo recentioriq̀ persecutionum tempore, mortem in Anglia subierunt, passiones, Romæ in Collegio Anglico /

Cavalieri has engraved reproductions of Circignano's frecoes in the church of St. Thomas of Canterbury of the English College in Rome.

Ecclesiae militantis trivmphi, sive, Deo amabilium martyrvm gloriosa pro Christi fide certamina : prout opera RR Patrum Societatis Iesv Collegij Germanici et Hungarici moderator impensa S.D.N. Gregorii PP XIII in ecclesia S. Stephani Rotundi Romae Nicolai Circiniani pictoris manu uisuntur depicta, ad exictandam pior deuotionem /

Cavalieri has engraved reproductions of Circignano's frescoes in S. Stefano Rotondo in Rome.

Pietro da Cortona e gli affreschi nel Palazzo Pitti : notizie documentate /

Includes bibliographical references.

Giovanni Sanzio and his fresco at Cagli.

Cover-title.

Über die Maltechnik der Alten : mit besonderer Berücksichtigung der römisch-pompejanischen Wandmalerei, nebst einer Anleitung zur mikroskopischen Untersuchung der Kunstwerke /

Includes bibliographical references.

Chambre sépulcrale avec fresques découverte en 1872 près de Kertch ...

Extract from Report for 1872 of Russia. I. Arkheologicheskaia kommissïia.

A trace element study of siderite-jasper banded iron formation in the 3.45 Ga Warrawoona Group, Pilbara Craton - Formation from hydrothermal fluids and shallow seawater

Shale-normalised rare earth element and yttrium (REE + Y) patterns for siderite-jasper couples in a banded iron formation of the 3.45 Ga Panorama Formation, Warrawoona Group, eastern Pilbara Craton, display distinct positive Y and Eu anomalies and weak positive La and Gd anomalies, combined with depleted light REE relative to middle and heavy REE. Ambient seawater and hydrothermal fluids are identified as major sources of REE + Y for the BIF. In the case of siderites, strong correlations between incompatible trace elements and trace element ratios diagnostic of seawater indicate variable input from a terrigenous source (e.g. volcanic ash). We propose a volcanic caldera setting as a likely depositional environment where jasper and siderite precipitated as alternating bands in response to episodic changes in ambient water chemistry. The episodicity was either driven by fluctuations in the intensity of hydrothermal activity or changes in magma chamber activity, which in turn controlled relative sea level. In this context, precipitation of jasper probably reflects background conditions during which seawater was saturated in silica due to evaporative conditions, while siderites were deposited most likely during intermittent periods of enhanced volcanic activity when seawater was more acidic due to the release of exhalative phases (e.g. CO2). © 2005 Elsevier B.V. All rights reserved.

Volcanogenic mineralisation in the limestone lake area, Saskatchewan, Canada

This thesis describes the geology, geochemistry and mineralogy of a Lower Proterozoic, metamorphosed volcanogenic Cu-Zn deposit, situated at the western end of the Flin Flon greenstone belt. Stratabound copper mineralisation occurs in silicified and chloritoid-bearing alteration assemblages within felsic tuffs and is mantled by thin (< 3m) high-grade sphalerite layers. Mineralisation is underlain by garnet-hornblende bearing Lower Iron Formation (LIF), and overlain by garnet-grunerite bearing Upper Iron Formation (UIF). Distinctive trace element trends, involving Ti and Zr, in mineralised and footwall felsic tuffs are interpreted to have formed by fractionation associated with a high-level magma chamber in a caldera-type environment. Discrimination diagrams for basaltic rocks are interpreted to indicate their formation in an environment similar to that of recent, primitive, tholeiitic island arcs. Microprobe studies of key mineral phases demonstrate large and small scale chemical variations in silicate phases related to primary lithological, rather than metamorphic, controls. LIF is characterised by alumino-ferro-tschermakite and relatively Mn-poor, Ca-rich garnets, whereas UIF contains manganoan grunerite and Mn-rich garnets. Metamorphic mineral reactions are considered and possible precursor assemblages identified for garnet-, and chloritoid-bearing rocks. Chloritoid-bearing rocks are interpreted as the metamorphosed equivalents of iron-rich feeder zones formed near the surface. The iron-formations are thought to represent iron-rich sediments formed on the sea floor formed from the venting of the ore fluids. Consideration of various mineral assemblages leads to an estimate for peak metamorphic conditions of 450-500oC and > 4Kb total pressure. Comparisons with other volcanogenic deposits indicate affinities with deposits of `Mattabi-type' from the Archean of Ontario. An extrapolation of the main conclusions of the thesis to adjacent areas points to the presence of a number of geologically similar localities with potential for mineralisation.