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Manuscript Details Manuscript numberQUAGEO_2019_55TitleLUMINESCENCE DATING OF QUARTZ AND FELDSPARS AT MWULUS CAVE (LIMPOPO, SOUTH AFRICA)Article typeResearch paperAbstract Luminescence dating is applied
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01
To fill out extended-range luminescence dating, follow these steps:
02
Gather the necessary materials, including a sample for dating and a luminescence reader.
03
Prepare the sample by carefully cleaning it to remove any contaminants.
04
Take multiple measurements of the radiation dose rate at the sample location using the luminescence reader.
05
Record the data obtained from the measurements, including the radiation dose rate and the age of the sediment.
06
Calculate the dose rate of the sample by considering various factors such as water content, cosmic ray contribution, and radioactive isotopes present.
07
Use mathematical models or software to determine the age of the sample based on the luminescence signals.
08
Validate the results by comparing them with other dating methods or by conducting additional tests on different samples.
09
Interpret the dating results in the context of the geological or archaeological research being conducted.
10
Document the entire process, including the methods used, equipment used, and any deviations from standard procedures.
11
Share the findings with the scientific community through publications or presentations.

Who needs extended-range luminescence dating of?

01
Extended-range luminescence dating is needed by researchers and scientists in fields such as archaeology, geology, and paleoclimatology.
02
Archaeologists can use extended-range luminescence dating to determine the age of artifacts, sediments, or archaeological sites beyond the limitations of traditional dating methods.
03
Geologists can utilize this dating method to establish the ages of geological formations, sedimentary deposits, or mineral samples.
04
Paleoclimatologists often rely on extended-range luminescence dating to study past climate changes by dating sediment cores or glacial deposits.
05
In summary, anyone involved in studying the history, geology, or climate of the Earth can benefit from extended-range luminescence dating.
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Extended-range luminescence dating is a method used to determine the age of sedimentary deposits by measuring the amount of trapped energy in mineral grains, primarily quartz and feldspar, which have been exposed to light or heat.
Researchers and professionals in fields like geology, archaeology, and environmental science who wish to date sediment layers or artifacts may be required to file for extended-range luminescence dating.
To fill out extended-range luminescence dating, one should provide detailed information about the sample location, the type of sediment, methodology used for dating, and any relevant context or prior studies related to the samples.
The purpose of extended-range luminescence dating is to provide accurate age estimations for geological and archaeological samples, helping to construct timelines of human activity and environmental changes.
Information that must be reported includes the sample identification, geographic coordinates, the depth of the sample, the method of luminescence dating applied, and the results including age estimates and associated uncertainties.
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