Abstract Details
(2020) The Temporal Variation of Magma Plumbing System of the Kattadake Pyroclastic Rocks in the Zao Volcano, Northeastern Japan
Takebe M, Nishi Y & Ban M
https://doi.org/10.46427/gold2020.2533
The author has not provided any additional details.
05d: Room 2, Friday 26th June 05:54 - 05:57
MIrai Takebe
Yuki Nishi View abstracts at 2 conferences in series
Masao Ban View all 2 abstracts at Goldschmidt2020 View abstracts at 7 conferences in series
Yuki Nishi View abstracts at 2 conferences in series
Masao Ban View all 2 abstracts at Goldschmidt2020 View abstracts at 7 conferences in series
Listed below are questions that have been submitted by the community that the author will try and cover in their presentation. To submit a question, ensure you are signed in to the website. Authors or session conveners approve questions before they are displayed here.
Submitted by Georg F. Zellmer on Monday 22nd June 04:59
Dear Takebe-san, I am always amazed by the petrological and crystal chemical detail of Ban-san's group. Thank you for your hard work on making this poster! The andesitic mush is of great interest to me. What do you think is its origin? Is it formed by crystallization of previously intruded basaltic melts, or partial melting of the preexisting crust, or both? It would be great to include Sr-isotope crystal stratigraphic work in the future to get to the bottom of this. With kind regards, Georg
Dear Takebe-san, I am always amazed by the petrological and crystal chemical detail of Ban-san's group. Thank you for your hard work on making this poster! The andesitic mush is of great interest to me. What do you think is its origin? Is it formed by crystallization of previously intruded basaltic melts, or partial melting of the preexisting crust, or both? It would be great to include Sr-isotope crystal stratigraphic work in the future to get to the bottom of this. With kind regards, Georg
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