[Eoas-seminar] Tuesday Jan 28 Faculty Candidate for Solid Earth Processes in the Lithosphere (Chenguang Sun)

eoas-seminar at lists.fsu.edu eoas-seminar at lists.fsu.edu
Tue Jan 21 16:44:11 EST 2020

Dear all,

The first faculty candidate for the Lithospheric Processes (Metamorphic Petrology) search, Dr. Chenguang Sun will be arriving next Monday (27th) afternoon and will be leaving on Wednesday (29th).

I am attaching the title and abstract of his talk. The talk is scheduled at 3:30 PM; 28th January 2020 (Tuesday)
Venue: EOA 1044.

I am also attaching his CV+ application materials for your reference. If you would like additional information please feel free to contact me, I will be happy to update. Also if you would like to meet the candidate, please let me know of your availability and I will try and schedule a meeting.

I hope you are able to attend the presentation.

Title: Cratonic lithosphere thinning through time: Evidence from kimberlite thermobarometry

Abstract: As the keels of continents, cratons are believed to have been stable since their formation at billions of years ago. This conventional view was established from petrological, geochemical, and geophysical studies on cratonic lithosphere. Yet, evidence for the absence of cratonic roots at some Archean terrains casts doubt on the craton stability. This poses a fundamental question on the destabilization of cratons globally through time, which was often overlooked due to the lack of geological observations. To address this question, I develop a new liquid thermobarometer for kimberlite and other silica-poor, CO2-rich melts using high-temperature and high-pressure experimental data. As unique mantle-derived melts at ancient continents, kimberlite magmas are ideal tools to constrain the temporal variation of lithosphere thickness and the processes affecting the lithosphere root. Applying this new thermobarometer to global kimberlite rock records, I will show that the thickness of cratonic lithosphere has decreased globally by up to ~150 km during the past ~2 Gyr, indicating that the conventional view of stable, long-lived cratons needs to be revised. This has significant consequences on Earth’s dynamic and chemical evolution that demand a series of future studies. Taking the temporal evolution of kimberlite volcanism and subduction flux into account, I will also discuss the possible mechanism of craton destabilization through time and its implications for Earth’s deep carbon cycle.

Best wishes

Mainak Mookherjee
Associate Professor
Earth, Ocean and Atmospheric Sciences
Florida State University
Tallahassee, FL, 32310, USA

Phone: (850) 644 1536 (Office)
Email: mmookherjee at fsu.edu<mailto:mmookherjee at fsu.edu>
Email: mainak.mookherjee at gmail.com

-------------- next part --------------
An HTML attachment was scrubbed...
URL: <http://lists.fsu.edu/pipermail/eoas-seminar/attachments/20200121/ac6bbbe1/attachment.html>
-------------- next part --------------
A non-text attachment was scrubbed...
Name: Chenguang_Sun_Application_Report.pdf
Type: application/pdf
Size: 668625 bytes
Desc: Chenguang_Sun_Application_Report.pdf
URL: <http://lists.fsu.edu/pipermail/eoas-seminar/attachments/20200121/ac6bbbe1/attachment.pdf>

More information about the Eoas-seminar mailing list