EAG

Home

  • Program

    The Goldschmidt2020 program

  • Venue

    All about the venue and city

  • Registration

    Details of how to register to attend the conference and/or submit an abstract

  • Exhibition

    Information for and about exhibitors and sponsors

  • My Goldschmidt

    My program, purchases, connections, etc.

Home

Program

Events

  • Sponsor Seminars

  • Training Events

    These are scheduled events to help delegates test out the tools and platform we will be using for the Q&A and other events at the conference.

  • Workshops

    Our workshop program provides training and teaching in topics across geochemistry and related fields. We are currently liaising with the workshop organisers to ascertain if any workshops can become virtual. Any updates will be added to this page.

Locations

  • Conference Locations

    Location of the convention center and social events

  • Hotels

    The hotels are no longer available to book at the special rates agreed by the conference. Should you wish to cancel or change your hotel reservation please see the details below.

Information

Present your work

Attend

Exhibition

Sponsorships

My Goldschmidt

Role functions

Abstract Details

(2020) Extensive Magmatic Heating of the Lithosphere beneath the Hawaiian Islands Inferred from Salt Lake Crater Mantle Xenoliths

Guest I, Ito G, Garcia MO & Hellebrand E

https://doi.org/10.46427/gold2020.900

Sorry, the PDF cannot be displayed on your browser.

Download abstract

The author has not provided any additional details.

05h: Room 2, 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 Keith Putirka on
Hi Imani - The ca. 200-300 deg. C heating is precisely in the range of what we would expect for the excess T of the Hawaiian plume. Is this by accident, or expected? I suppose heating depends upon how much mass is involved for hot and cool end-members, but I'm wondering if the plume can give up close to the entirety of its excess heat (for a case of near-equal masses, which means the plume should be quite cool moving laterally away from the plume core). Or is this a case where large amounts of melt invade a small space, perhaps over an extended period of time, making the excess T match a luckless coincidence? Thanks. -Keith

Sign in to ask a question.

Geochemical Society, an organization registered in USA. Address: 5241 Broad Branch Road, NW Washington, DC 20015-1305.
Tel: +44 1223 852663. Email: helpdesk@goldschmidt.info

Goldschmidt® is a registered trademark of the Geochemical Society and of the European Association of Geochemistry

Conference management and website by White Iron Conferences

Main photograph © Kenneth Rubin