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10B - Geochronology

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Ages of geological formations or secondary events (i.e. alteration or metamorphism) can be determined through using K-Ar, (Ar-Ar), U-Pb, Rb-Sr or the Sm-Nd dating methods. These analytical procedures include several steps:

1.       Dating method selection

2.       Sample collection

3.       Sample preparation, mineral separation and treatment

4.       Irradiation of the samples in a nuclear reactor for the Ar-Ar technique

5.       High precision determination of the concentration of the moter and daughter isotopes by TIMS (Thermal Ionization Mass Spectrometry)

6.       Apparent age calculation and interpretation of the results


The dating strategy depends on the type of formation (magnmatic, metamorphic or sedimentary), the sampe composition and the age of formation. The concentration of the mother and daughter isotopes, as well as the apparent age can be determined with high preision. In many cases, however, the determined age may not be the real age of the geological event. The apparent age may be affected by the post-depositional or post-formation history of the rocks. Natural contamination of chemical sediments with detrital material can also affect the results of dating of diagenesis.


There are some techniques and calculations which can “look through” the post formation event. These include isochron dating, such as K-Ar, U-Pb, Rb-Sr and Sm-Nd, or the step heating Ar-Ar technique of the K-Ar method. In the Ar-Ar technique, the K and Ar are measured on the same sample aliqupt. First the sample is irradiated in a nuclear reactor, where fast neutrons convert some of the 39K to 39Ar. After irradiation, the Ar is released fractionally by incremental heating. The result is a series of apparent ages from which useful information about the geologic history and the age of the sample can be inferred. Specific techniques for dating clay fractions have also been developed.


Our geochronological services provide dating methods for all types of geological samples through use of modern analytical facilities. We can advise on selecting the method of dating, sampling and interpretation of the data so that meaningful geological results are obtained.


For the dating of a monomineralic sample only tens of milligrams of sample are required. For rocks, a few hundred milligrams are typically used for analysis. Size of the rock sample required will vary considerably for mineral separation depending on which minerals must bbe separated and the amount and type of the accessory mineral present.


Advice concerning dating strategies and interpretation of data is provided as erquired. Disounts may be applicable for large dating programs. For more information, please contact geochronology@actlabs.com




Carbon and Oxygen Isotopes



K-Ar dating

Rock fractions, clay fractions and separated minerals (e.g. biotite, hornblende, sericite, K-feldspar, illite, glauconite, etc.)

K-Ar dating in duplicate

Two independent measurements on one sample

40 Ar-39Ar step heating dating

Rock fractions, clay fractions or separated minerals (e.g. biotite, hornblende, sericite, K-feldspar, illite, glauconite, etc.)

U-Pb dating by TIMS

Single grain analysis (e.g. zircon, monazite, titanite, apatite)

U-Pb isochron dating by SHRIMP

Single grain analysis

Rb-Sr dating by TIMS

Isochron dating whole rock and minerals

Sm-Nd dating by TIMS

Isochron dating whole rock and minerals

Re-Os dating

Re-Os dating

Petrographic description

Includes thin section preparation

Mineral Separation

Specific mineral phases are separated to provide best data for age dating


Activation Laboratories Ltd. | 41 Bittern Street, Ancaster, Ontario, L9G 4V5, Canada | TF: +1.888.228.5227
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