CHICAGO, ILLINOIS
October 45, 2001
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Hosted by
The Field Museum
FIRST ANNOUNCEMENT JANUARY 2001 ____________________________________________________________________________________ MEETING ORGANIZERS
Mark Robinson, Northwestern University
G. Jeffrey Taylor, University of Hawai'iSPONSORED BY
Lunar and Planetary Institute
The Field Museum
National Aeronautics and Space AdministrationSCIENTIFIC ORGANIZING COMMITTEE
Mark Robinson, Northwestern University
Paul Spudis, Lunar and Planetary Institute
Jim Slavin, NASA Goddard Space Flight Center
Sean Solomon, Carnegie Institution
Marty Slade, Jet Propulsion Laboratory
Ann Sprague, University of Arizona
G. Jeffrey Taylor, University of Hawai'i
Faith Vilas, NASA Johnson Space Center
Meenakshi Wadhwa, The Field Museum
Thomas Watters, National Air and Space Museum
____________________________________________________________________________________PURPOSE AND SCOPE
Mariner 10 gave the first close-up look of Mercury over 25 years ago by imaging one hemisphere of the planet and measuring its space environment. Initial results from this mission showed Mercury to have a heavily cratered surface with younger superposed plains, a complex history of tectonic deformation, and a magnetic field. Since then, many new discoveries about Mercury have appeared, utilizing not only the Mariner 10 data, but also exciting results obtained from Earth-based remote sensing: Ionic species have been identified in the mercurian exosphere, unusual radar reflective deposits in the polar regions have been found, and large-scale radar morphologic features are seen in the unimaged hemisphere. It is the intent of this meeting to bring together representatives from diverse scientific disciplines to foster a broader understanding of Mercury as planet its space environment, surface, and interior. Such a meeting should be of interest not only to Mercury enthusiasts, but also to scientists interested in the broader topics of solar system formation and comparative planetology. Mercury is an endmember terrestrial planet in terms of proximity to the Sun, density, and size and therefore holds important information regarding planetary formation in the early solar system. Thus a broad synthesis of Mercury science is anticipated to serve a wide scientific community.There has not been a meeting dedicated to Mercury in nearly 15 years, despite the large strides made in mercurian science over the past decade. No spacecraft has visited Mercury since Mariner 10; however, both NASA (MESSENGER) and ESA (Bepi-Columbo) intend to send orbiters by the end of this decade. The time is right to bring together current Mercury science in context of these upcoming missions to Mercury.
MEETING FORMAT
The intent of the meeting is to bring new results concerning Mercury to a single forum through both oral and poster presentations. There will be a few invited talks, but the bulk of the conference will consist of contributed talks. Poster presentations will be given high visibility through short summary talks in appropriate sessions, as well as ample viewing times on Thursday evening. Abstracts may cover (but are not limited to) the following topics relating to Mercury:For planning purposes, if you think you may want to attend the workshop, please complete and return the downloadable Indication of Interest form or simply fill in the electronic Indication of Interest form. Future announcements will only be available electronically on the schedule shown below. No additional announcements will be mailed in hard copy, but if there are important notices other than the scheduled announcements on the Web listed below, we will send e-mail notices only to those who have returned the Indication of Interest form.
- Surface geology including tectonic, volcanic, and impact processes
- Earth-based surface spectral measurements and space weathering
- Migration, deposition, and preservation of volatiles at the poles
- Identification and sources of exospheric ions
- Constraints on size and composition of the core
- Bulk composition of the crust and mantle
- Magnetic field and near-space environment
- Modeling of Mercury's formation
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