Start Radiocarbon dating thermoluminescence

Radiocarbon dating thermoluminescence

C ages, suggesting that zeroing of light-sensitive TL in the detrital feldspars has been effective enough in this depositional environment to allow accurate dating of deeper core samples of similar sedimentology.

To obtain a truly absolute chronology, corrections must be made, provided by measurements on samples of know age.

The most suitable types of sample for radiocarbon dating are charcoal and well-preserved wood, although leather, cloth, paper, peat, shell and bone can also be used.

Therefore, luminescence dating results should be regarded with skepticism and the accompanying caveats clearly stated.

While for several samples both dating techniques were at the limits of their detection, results from the upper strata of the northwestern face of the Pantai Mine indicate agreement between the two independent dating techniques.

At this point, the method seems to be a straightforward concept.

However, problems arise from assuming a uniform radiation dose rate over any significant period of time and assuming that the TMRD resulted from the object or artifact being in a strictly constrained environment identical to that in which it was found.

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