The Natural History Museum uses Linkam temperature- controlled microscopy to study inclusions in mineral deposits

This is a multiphase brine inclusion image (approximately 30 microns in length) from the Boyongan copper-gold porphyry deposit in the Philippines. In addition to a high salinity aqueous solution it contains a round vapour bubble, a large halite (NaCl) cube, a smaller sylvite (KCl) cube and several other “daughter” crystals that have crystallised during cooling of the fluid after high temperature entrapment. For a high-resolution copy of the image, either right click to download or contact Jezz Leckenby at Talking Science Limited.

Dr Jamie Wilkinson is a Research Leader in Mineral Deposits in the Department of Earth Sciences at the Natural History Museum, London. He is a member of the London Centre for Ore Deposits and Exploration (LODE) Research Group, a joint initiative between the Natural History Museum in London and the Department of Earth Science and Engineering at Imperial College London. The Group carries out research on the mineralogy and geochemistry of ore deposits in order to improve the success rates of mineral resource discovery and provide solutions to reduce both the environmental impact and energy use of resource extraction. Their work combines both seeking practical solutions to exploration challenges and improving the understanding of the processes by which ore deposits form in the Earth’s crust.

Dr Wilkinson has worked with various Linkam stages for more than 20 years starting with his PhD research work at the University of Southampton. The Linkam temperature stages are used to study fluid inclusions – microscopic droplets of liquid that can be trapped inside growing crystals when they form in the Earth. These are typically just a few tens of microns in size, thus requiring microscopic methods for their investigation, and may have formed millions or even billions of years ago. By freezing and heating these inclusions, it is possible to obtain information on the composition, density, temperature and pressure of entrapment of the fluid – information that provides critical constraints on the conditions of crystal growth. In ore deposits, this information can tell a researcher about the temperature at which the ore minerals formed, their depth of formation beneath the Earth’s surface and something about the fluid composition, in particular how salty it is, and also whether it contains dissolved gases like methane or carbon dioxide. Data like this can be critical in distinguishing between different mechanisms for ore formation.

Dr Wilkinson discusses the benefits of working with Linkam and their temperature stages. “I have become more and more impressed with the Linkam family of temperature-controlled stages. They provide precise and accurate measurement capability, are designed with a small thermal mass so respond quickly and require small temperature calibration corrections. Not least is their ease of use (particularly where inexperienced undergraduate students are concerned). All are equally important to us.”

An example of Dr Wilkinson’s research is presented in a paper that documents data gathered over a number of years to demonstrate a new method for the estimation of salinity in aqueous fluid inclusions.¹ In discussing the design of Linkam’s stages, Dr Wilkinson said “the thermal masses of the stages (heating block and sample holders) are small and hence thermal equilibration rates are clearly very fast. This is evidenced by the virtually immediate response of an inclusion to a small step in temperature when close to a phase change such as final ice melting or CO₂ phase homogenisation. Linkam’s stages were ideal for this work.”

For information on Linkam’s range of temperature-controlled stages along with other temperature and environmental materials characterisation solutions, click here to visit the click here to visit the website.

Reference

¹ METASTABLE FREEZING: A NEW METHOD FOR THE ESTIMATION OF SALINITY IN AQUEOUS FLUID INCLUSIONS, J J Wilkinson, Economic Geology, v. 112, pp. 185–193, https://doi.org/10.2113/econgeo.112.1.185