Abstract Details
(2020) Petrochronological and Structural Constraints on Intra-Oceanic Subduction Initiation from the Metamorphic Sole of the New Caledonia Ophiolite
Guerer D, Cenki-Tok B, Chatzaras V, Corfu F, Collot J & Maurizot P
https://doi.org/10.46427/gold2020.899
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04h: Room 5, Thursday 25th June 22:15 - 22:18
Derya Guerer
BÉNÉDICTE Cenki-Tok View all 3 abstracts at Goldschmidt2020
Vasileios Chatzaras View abstracts at 2 conferences in series
Fernando Corfu View abstracts at 18 conferences in series
Julien Collot View abstracts at 2 conferences in series
Pierre Maurizot View abstracts at 2 conferences in series
BÉNÉDICTE Cenki-Tok View all 3 abstracts at Goldschmidt2020
Vasileios Chatzaras View abstracts at 2 conferences in series
Fernando Corfu View abstracts at 18 conferences in series
Julien Collot View abstracts at 2 conferences in series
Pierre Maurizot View abstracts at 2 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 Simon Cuthbert on Wednesday 24th June 17:05
Thanks very much for your poster - it looks like it will be a very interesting study. I see that you propose to determine the P-T evolution of the metamorphic sole, so my question is - what differences would you expect to see in P-T evolution between the two scenarios you set out (forced vs. passive initiation)?
Thanks very much for your poster - it looks like it will be a very interesting study. I see that you propose to determine the P-T evolution of the metamorphic sole, so my question is - what differences would you expect to see in P-T evolution between the two scenarios you set out (forced vs. passive initiation)?
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