In my post about new evidence for the supercontinent Rodinia, I mentioned that there’s an interesting process that’s performed for dating rocks and that it’s actually the kind of work that I assist with. I thought it would be interesting to make a post that goes into more detail about how this is done.
I’ve made a presentation that outlines the science and process behind dating rocks which should help introduce the subject matter in a way that’s quick and easy to digest. Here’s the link: https://prezi.com/3k4tv3lligxw/geochonology-and-mineral-separation/
To summarize the material in the presentation, zircon is a mineral that is in virtually every kind of rock and contains uranium impurities. Uranium decays radioactively at a very slow rate. This means we can calculate the amount of radioactive decay that has occurred within the zircon and use that to come up with a formation age for the rock.
There are four main processes that we must go through in order to separate the zircons from the rock: crushing, panning, demagnetizing, and heavy liquids. I decided to make a video showing my favorite, heavy liquids. This process involves putting the sample in a super dense liquid (methylene iodide/MEI) and extracting the densest minerals, which should all be zircon. This is the most rewarding stage of the process because I get to finally see all the zircons I’ve been working to isolate. The video shows off the process and the logistics of how it’s performed in detail. Check it out below:
The sample used in the video was representative of a really high zircon yield. This was great because it was easy to see the large quantity of them sinking during the time lapse and collected in the filter paper at the end. In samples that have a lower yield, the zircons may be harder to see sinking in the MEI and collected in the filter paper. Ultimately the zircon yield in a sample simply depends on the type of rock the sample is and where it came from, I just got lucky by picking one that had a high yield for the video.
Geochronology is really helpful for solidifying geologists’ understanding of specific sets of rocks. Without this method we wouldn’t be able to come up with an exact age for any given set of rocks. These qualitative ages allow geologists to improve their understanding of a region, how it formed, and what it has experienced in the time since it formed. USGS is currently working on dating a large number of samples from various sandstones near the Mississippi River delta. They send out field geologists to collect samples that they want dates for. These samples are then sent to UC Santa Barbara where I take them through the processes of mineral separation. Finally I send the zircons off to our laser lab where they can be dated. While this project is obviously still in its earlier stages, when it is complete it should provide significant data that improves our understanding of that region.







