Dear Colleagues,
Sorry for multiple cross-postings
With this email, we would like to bring your attention to our session about
core–mantle interactions and processes at Goldschmidt 2021 to be held in
Lyon, France. Goldschmidt 2021 will be in a hybrid format, combining an
onsite meeting for delegates who can travel, with an online meeting for
those who cannot.
The deadline for abstract submission to Goldschmidt 2021 is approaching
fast (26th February 2021, 23:59 CET). We look forward to seeing you in Lyon
and also online! Abstracts can be submitted at this link
https://2021.goldschmidt.info/goldschmidt/2021/02/papers/index.cgi?sessionid=1853
.
*Session 2g: **An interdisciplinary view of core-mantle interactions and
processes *(https://2021.goldschmidt.info/goldschmidt/2021/meetingapp.cgi/Session/1853
https://2021.goldschmidt.info/goldschmidt/2021/meetingapp.cgi/Session/1853)
Description: The interior of the Earth is complex, heterogeneous,
and ever-changing. At the surface, material is subducted into the mantle,
and at the core-mantle boundary, interactions take place between the
silicate mantle and the metallic core. While the core is the most
inaccessible part of the Earth and other planetary bodies, signatures of
its interaction with the mantle above can reveal key information about
planetary evolution, from the earliest formation to the present. To
decode such information is extremely valuable but also difficult, and often
requires integrated interdisciplinary research. Advances in both
experimental and theoretical techniques in recent years have greatly pushed
forward studies on core-mantle interaction. Research works probing or
simulating core/lower-mantle conditions by employing seismology, isotope
fractionation, element partitioning, geodynamic modeling,
thermodynamics, and other techniques, have significantly improved
our understanding of these possible interactions, as well as their
subsequent expression on the surface. At the same time, new ideas and
models about the core-mantle boundary are emerging. We seek to organize a
session that highlights the broad-scale study of the core and its
interaction with the mantle in the Earth and other rocky planets. We invite
contributions from a wide range of fields focusing on
this multidisciplinary topic, including but not limited to
geodynamics, seismology, mineral physics, and those presenting new
theoretical/analytical or experimental techniques. Topics could include
accretion, core-mantle differentiation, core crystallization and
exsolution, lowermost mantle melting, geodynamo, plume dynamics, the nature
of seismic anomalies at the core-mantle boundary, and heat and volatile
transport.
Keynote speaker: James Badro (Institut de Physique du Globe de Paris)
Sincerely,
Kind regards form the conveners:
Juliane Dannberg, Rebecca Fischer, Yunguo Li, Anat Shahar
Dear Colleagues,
**Sorry for multiple cross-postings**
With this email, we would like to bring your attention to our session about
core–mantle interactions and processes at Goldschmidt 2021 to be held in
Lyon, France. Goldschmidt 2021 will be in a hybrid format, combining an
onsite meeting for delegates who can travel, with an online meeting for
those who cannot.
The deadline for abstract submission to Goldschmidt 2021 is approaching
fast (26th February 2021, 23:59 CET). We look forward to seeing you in Lyon
and also online! Abstracts can be submitted at this link
<https://2021.goldschmidt.info/goldschmidt/2021/02/papers/index.cgi?sessionid=1853>
.
*Session 2g: **An interdisciplinary view of core-mantle interactions and
processes **(https://2021.goldschmidt.info/goldschmidt/2021/meetingapp.cgi/Session/1853
<https://2021.goldschmidt.info/goldschmidt/2021/meetingapp.cgi/Session/1853>)*
*Description*: The interior of the Earth is complex, heterogeneous,
and ever-changing. At the surface, material is subducted into the mantle,
and at the core-mantle boundary, interactions take place between the
silicate mantle and the metallic core. While the core is the most
inaccessible part of the Earth and other planetary bodies, signatures of
its interaction with the mantle above can reveal key information about
planetary evolution, from the earliest formation to the present. To
decode such information is extremely valuable but also difficult, and often
requires integrated interdisciplinary research. Advances in both
experimental and theoretical techniques in recent years have greatly pushed
forward studies on core-mantle interaction. Research works probing or
simulating core/lower-mantle conditions by employing seismology, isotope
fractionation, element partitioning, geodynamic modeling,
thermodynamics, and other techniques, have significantly improved
our understanding of these possible interactions, as well as their
subsequent expression on the surface. At the same time, new ideas and
models about the core-mantle boundary are emerging. We seek to organize a
session that highlights the broad-scale study of the core and its
interaction with the mantle in the Earth and other rocky planets. We invite
contributions from a wide range of fields focusing on
this multidisciplinary topic, including but not limited to
geodynamics, seismology, mineral physics, and those presenting new
theoretical/analytical or experimental techniques. Topics could include
accretion, core-mantle differentiation, core crystallization and
exsolution, lowermost mantle melting, geodynamo, plume dynamics, the nature
of seismic anomalies at the core-mantle boundary, and heat and volatile
transport.
*Keynote speaker*: James Badro (Institut de Physique du Globe de Paris)
Sincerely,
Kind regards form the conveners:
Juliane Dannberg, Rebecca Fischer, Yunguo Li, Anat Shahar
----------------------------------------------------------------------
Rebecca A. Fischer
Clare Boothe Luce Assistant Professor
Department of Earth and Planetary Sciences
Harvard University
rebeccafischer@g.harvard.edu <rebeccafischer@fas.harvard.edu>
https://scholar.harvard.edu/raf
----------------------------------------------------------------------