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Speleothems, Travertines, and Paleoclimates
Quaternary Research, 1983AbstractAge data for about 660 speleothems and about 140 spring-deposited travertines were collected, including many unpublished results. These data were plotted as histograms and also as error-weighted frequency curves on a 350,000-yr scale. These plots clearly show periods of increased speleothem/travertine growth as well as times of cessation.
G. J. Hennig, R. Grün, K. Brunnacker
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Proceedings of the Geologists' Association, 1993
A review of British Quaternary travertines is provided, including details of 159 sites presented as a cross-referenced coded list with a full bibliography. Almost all of these travertines were formed by the degassing of calcium bicarbonate waters. The ‘carrier’ CO 2 originated from the soil and epigean atmospheres.
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A review of British Quaternary travertines is provided, including details of 159 sites presented as a cross-referenced coded list with a full bibliography. Almost all of these travertines were formed by the degassing of calcium bicarbonate waters. The ‘carrier’ CO 2 originated from the soil and epigean atmospheres.
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Preface to the volume “Travertine”
Acta Geologica Hungarica, 2003Quaternary thermogene and meteogene travertine occurs globally, both in Hungary and abroad. Size and thickness of the individual deposits are highly variable.
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Travertine/tufa resource conservation and sustainable development call for a world-wide initiative
Applied Geochemistry, 2023Jiang Zhongcheng +1 more
exaly
Travertine on the Zagreb Cathedral
2005Romanesque and Gothic capitals of the St. Stephen's Cathedral in Zagreb were built from lithothamnian limestone, which is the autochthonous stone in the Zagreb area. The stone has with time been damaged to such extent, that it needs to be replaced. Travertine has proved to be the most suitable replacement for lithothamnian limestone.
Dunda, Siniša +2 more
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