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Abstract Details

(2020) Th–U Powered Metamorphism: Thermal Consequences of a Chemical Hot Spot

De Vries Van Leeuwen A, Hand M, Morrissey L & Raimondo T


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04h: Room 1, View in program

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 Christopher Lambert on
Liked your talk Alex!

Submitted by Shah Wali Faryad on
Th–U Powered Metamorphism: Thermal Consequences of a Chemical Hot Spot De Vries Van Leeuwen A, Hand M, Morrissey L & Raimondo T Formation of cordierite or andalusite prophyroblasts in a fine grained matrix, as indicated in slide 3, is typical feature of contact-thermal metamorphism. Are you sure that the formation of cordierite is not related to the granite intrusion in your field?

Submitted by Thomas Zack on
1.) WHY are the sediments in your area so radiogenic in the first place? 2.) Is there still an elevated geothermal gradient in the Arkaroola area? There are geothermal springs, but they may be shallow. I am curious as most of the sedimentary cover is eroded, or not?

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