Isotopic MethodsUranium series dating of Quaternary deposits
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Cited by (68)
An integrated study of constraining the initial <sup>230</sup>Th of a stalagmite and its implications
2024, Quaternary GeochronologyMulti dating approach of long marine core sediments from the south-eastern continental shelf of Korea: Comparison of SAR OSL, TT-OSL and pIRIR dates
2022, Quaternary GeochronologyCitation Excerpt :Notwithstanding the shortcomings of each method, the two dating methods were determined to be suitable as complementary methods for analysing aged long- and old-core sediments. The commonly used 230Th/234U technique can be applied to a variety of materials and time ranges, from a few hundred years to more than 500 kyr (Schwarcz, 1989; Walker, 2005). Previous studies used corals containing large amounts of uranium (Cheng et al., 2000; Cobb et al., 2003; Schellmann et al., 2004; Shen et al., 2008).
Speleothem record from Pentadactylos cave (Cyprus): new insights into climatic variations during MIS 6 and MIS 5 in the Eastern Mediterranean
2020, Quaternary Science ReviewsCitation Excerpt :Petrographical observation shows that section B (base of Penta 1) is the most porous part of the whole record and where most of the age inversions occurs (Fig. 2). Porous calcite structures are known to be subject of U–Th open-system behavior (Richards and Dorale, 2003; Borsato et al., 2005) via dissolution and recrystallization processes of the primary carbonate (Frisia, 2015), remobilization, or post-depositional filling of pores (Schwarcz, 1989), resulting in out-of-sequence ages. Dating points Pentad-2, -5, -14 and Pentad-18 were therefore excluded from the age model.
Climate and structure of the 8.2 ka event reconstructed from three speleothems from Germany
2020, Global and Planetary Change