February 2015 – Isotope preparation

In order to understand the source of magma under Ascension, and how much interaction the magma has with surrounding rock as it ascends to the surface can be understood by measuring the isotopic composition of the rocks erupted. In this first round of isotope work, Katy has powdered up whole samples of both lava flows and pyroclastic material, and then dissolved them to liquids, in order to isolate the two elements on interest for us: lead (Pb) and strontium (Sr). While a lot of whole rock (WR) isotope work has been carried out on Ascension previously, we have new samples which haven’t been examined in detail before, so we are aiming to fill in a few gaps in our understanding of the source of volcanism on Ascension Island.

Once Katy has cuts of Pb and Sr from each sample, the cuts are taken up into a dilute acid solution, and analysed using a multi-collector (MC) inductively coupled plasma mass spectrometer (ICPMS) at Durham University. Data to come soon!

2015_5 MC-ICP_MS dur

MC-ICP-MS at Durham University.

Leave a Reply

Fill in your details below or click an icon to log in:

WordPress.com Logo

You are commenting using your WordPress.com account. Log Out / Change )

Twitter picture

You are commenting using your Twitter account. Log Out / Change )

Facebook photo

You are commenting using your Facebook account. Log Out / Change )

Google+ photo

You are commenting using your Google+ account. Log Out / Change )

Connecting to %s