Joachim Szulc
Dados Biográficos
| ID | 5602089 |
|---|---|
| NOME | Joachim Szulc |
| PRENOMES | Joachim |
| SOBRENOME | Szulc |
| ASSINATURA | SZULC J |
| AFILIAÇÕES | Instytut Nauk Geologicznych |
| VERIFICADO | Não |
| TOTAL DE OBRAS | 2 |
| TOTAL DE CITAÇÕES | 8 |
| TOTAL COMO AUTOR | 2 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1988 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 1988 |
| ÍNDICE H | 1 |
Stable Isotopes of Holocene Calcareous Tufa in Southern Poland as Paleoclimatic Indicators
The isotopic composition of oxygen in freshwater calcareous tufa seems to be a sensitive indicator of past climatic changes. Results of measurements of δ c 18 O and δ c 13 C in tufa samples dated with the 14 C method are used to reconstruct Holocene climatic changes in southern Poland. Values of δ c 18 O obtained on tufa samples from four sites (Raclawka, Rzerzuŝnia, Trzebienice, Sieradowice) representing different hydrodynamic conditions of tufa…
Radiocarbon Dating of Holocene Calcareous Tufa in Southern Poland
Calcareous tufa from five sites in southern Poland, representing several most typical conditions of tufa sedimentation, were chosen for 14 C, 13 C, and 18 O measurements. These tufas were deposited in a high-energy turbulent stream (the Racławka site), in streams with moderate but variable flow (Rzerzuśnia and Trzebienice), and in semilimnic conditions (Sieradowice site). Sediments of the Gliczarów site represent spring travertines. In all but th…
Radiocarbon Dating of Holocene Calcareous Tufa in Southern Poland
Calcareous tufa from five sites in southern Poland, representing several most typical conditions of tufa sedimentation, were chosen for 14 C, 13 C, and 18 O measurements. These tufas were deposited in a high-energy turbulent stream (the Racławka site), in streams with moderate but variable flow (Rzerzuśnia and Trzebienice), and in semilimnic conditions (Sieradowice site). Sediments of the Gliczarów site represent spring travertines. In all but th…
Stable Isotopes of Holocene Calcareous Tufa in Southern Poland as Paleoclimatic Indicators
The isotopic composition of oxygen in freshwater calcareous tufa seems to be a sensitive indicator of past climatic changes. Results of measurements of δ c 18 O and δ c 13 C in tufa samples dated with the 14 C method are used to reconstruct Holocene climatic changes in southern Poland. Values of δ c 18 O obtained on tufa samples from four sites (Raclawka, Rzerzuŝnia, Trzebienice, Sieradowice) representing different hydrodynamic conditions of tufa…
Radiocarbon Dating of Holocene Calcareous Tufa in Southern Poland
Calcareous tufa from five sites in southern Poland, representing several most typical conditions of tufa sedimentation, were chosen for 14 C, 13 C, and 18 O measurements. These tufas were deposited in a high-energy turbulent stream (the Racławka site), in streams with moderate but variable flow (Rzerzuśnia and Trzebienice), and in semilimnic conditions (Sieradowice site). Sediments of the Gliczarów site represent spring travertines. In all but th…
Calcareous (2 obras) · Carbonate (2 obras) · Geology and Paleoclimatology Research (2 obras) · Holocene (2 obras) · Isotope Analysis in Ecology (2 obras) · Quaternary (2 obras) · Sediment (2 obras) · Sedimentation (2 obras) · Tufa (2 obras) · Archaeology and ancient environmental studies (1 obras)