Zobrazeno 1 - 6
of 6
pro vyhledávání: '"P. T. Staudigel"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 5, Pp n/a-n/a (2021)
Abstract Biogenic and inorganic calcium carbonates contain considerable amounts of internal water, both as free and organically associated water. The oxygen isotopic compositions (δ18O) of internal water and hosting carbonate are analyzed for variou
Externí odkaz:
https://doaj.org/article/004da7d10ad94650887135d8eef94877
Autor:
Peter Müller, Philip T. Staudigel, Sean T. Murray, Robert Vernet, Jean-Paul Barusseau, Hildegard Westphal, Peter K. Swart
Publikováno v:
Scientific Reports, Vol 7, Iss 1, Pp 1-11 (2017)
Abstract The reconstruction of pre-depositional cooking treatments used by prehistoric coastal populations for processing aquatic faunal resources is often difficult in archaeological shell midden assemblages. Besides limiting our knowledge of variou
Externí odkaz:
https://doaj.org/article/84479557d40445b0bb3dec165d26430a
Autor:
F. W. H. Smit, L. Stemmerik, M. E. Smith, P. T. Staudigel, M. Lüthje, A. Mathiesen, F. S. P. van Buchem, P. K. Swart
Publikováno v:
Smit, F W H, Stemmerik, L, Smith, M E, Staudigel, P T, Lüthje, M, Mathiesen, A, van Buchem, F S P & Swart, P K 2022, ' The occurrence of a palaeo-lithification front in an overpressured basin (Chalk Group)—Timing from clumped isotopes and seismic stratigraphic analysis ', Basin Research, vol. 34, no. 4, pp. 1341-1373 . https://doi.org/10.1111/bre.12662
This study proposes a unique workflow to unravel complex burial diagenetic histories of overpressured basins based on the integration of seismic and well log data, biostratigraphy, petrography, clumped isotope analyses and basin modelling. This appro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f2ff2e93c2dcfe15f0d166fb771bbcb7
https://orbit.dtu.dk/en/publications/87a10c7c-6d64-4a08-992d-dadee10d688c
https://orbit.dtu.dk/en/publications/87a10c7c-6d64-4a08-992d-dadee10d688c
Autor:
Philip T. Staudigel, Peter K. Swart
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 19, Iss 8, Pp 2371-2383 (2018)
Abstract Accurate determination of paleotemperatures using carbonate δ18O and Δ47 values rely upon the assumption that the minerals in question formed close to expected isotopic equilibrium with their environment. If there is insufficient time for
Externí odkaz:
https://doaj.org/article/8d9120b48d684489b6275ce1d7cd7eda