Researchers studied fluid inclusions in quartz samples from an epithermal bonanza-type ore deposit in Mexico using Linkam’s THMSG600.
Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province using Linkam’s THMS600.
Using Linkam’s FTIR600 stage for microthermometric studies in dark and opaque minerals associated to uranium mineralisation
A New Experimental Procedure for Simulation of H2s + CO2 Geological Storage. Application to Well Cement Aging
Application of the Linkam TS1400XY heating stage to melt inclusion studies
Melt inclusions offer a direct method to study magmatic processes and the evolution of magmatic systems, including the determination of volatile content in a magma body before an eruption. Various techniques, such as heating in one-atmosphere furnaces, high-pressure vessels, and microscope-mounted high-temperature stages, are used to homogenize MI for analysis. Discover how the Linkam TS1400XY heating stage revolutionises the study of melt inclusions with its exceptional ability to homogenize melt inclusions and swiftly quench the homogeneous melt into a glass, it opens up new possibilities for research and exploration.
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TS1400XY
Late Eocene to early Oligocene quantitative paleotemperature record: Evidence from continental halite fluid inclusions
THMSG600 shown above
Scientists in China used a Linkam THMSG600 to enable their research into climate change.
Contactless probing of polycrystalline methane hydrate at pore scale suggests weaker tensile properties than thought using Linkam’s CAP500
Tensile properties of polycrystalline methane hydrate are analysed using Linkam’s CAP500 under microscopy.
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Wan, Ye, et al. "An Experimental Study of the Formation of Talc through CaMg (CO3) 2–SiO2–H2O Interaction at 100–200 C and Vapor-Saturation Pressures." Geofluids 2017 (2017).
An Experimental Study of the Formation of Talc through CaMg(CO3)2–SiO2–H2O Interaction at 100–200∘C and Vapor-Saturation Pressures using Linkam’s CAP500
Researchers used Linkam’s CAP500 (shown above) with fused silica capillaries to study the formation of talc, observing the process using techniques including Raman spectroscopy and X-ray diffraction.
Access the research here.
Wan, Ye, et al. "An Experimental Study of the Formation of Talc through CaMg (CO3) 2–SiO2–H2O Interaction at 100–200 C and Vapor-Saturation Pressures." Geofluids 2017 (2017).