Abstract Details
(2020) Using Zoned Melt Inclusions to Quantify Eruptive Cooling Rates on Hawaii
Saper L & Stolper E
https://doi.org/10.46427/gold2020.2281
The author has not provided any additional details.
05h: Room 2, Saturday 27th June 06:00 - 06:03
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Submitted by Aaron Pietruszka on Monday 22nd June 23:21
Hi Lee, thanks for sharing the results of your experiments. Do you have any thoughts on how you would like to apply the method to case studies of eruptions in Hawaii or elsewhere? Best regards, Aaron Pietruszka
Hi Lee, thanks for sharing the results of your experiments. Do you have any thoughts on how you would like to apply the method to case studies of eruptions in Hawaii or elsewhere? Best regards, Aaron Pietruszka
Submitted by Keith Putirka on Wednesday 24th June 20:22
Hi Lee - really interesting experiments - always great when they can mimic nature. I presume that MgO decreases in the MI because the crystal walls that enclose the MI are growing inward, so MgO is consumed by crystal growth. Is that the case? And then Ca and Al would increase in the residual MI? So residual MI might preserve original Ca/Al ratios? Thanks. -Keith
Hi Lee - really interesting experiments - always great when they can mimic nature. I presume that MgO decreases in the MI because the crystal walls that enclose the MI are growing inward, so MgO is consumed by crystal growth. Is that the case? And then Ca and Al would increase in the residual MI? So residual MI might preserve original Ca/Al ratios? Thanks. -Keith
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