DI13B:
Heterogeneity in Earth's Deep Interior: From Natural and Laboratory Observations to Theoretical Models II
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DI13B:
Heterogeneity in Earth's Deep Interior: From Natural and Laboratory Observations to Theoretical Models II
Heterogeneity in Earth's Deep Interior: From Natural and Laboratory Observations to Theoretical Models II
You can still search the program to see your colleague�s abstract submissions as well as the sessions submitted for the 2016 Fall Meeting. The final program will be released in early October.
Session ID#: 16723
Session Description:
Geochemistry plays an important role in our understanding of Earth’s accretion, its differentiation, and the formation of the atmosphere. Combining natural and laboratory measurements with geophysical observations and geodynamic models of mantle convection will position us to make major breakthroughs in our understanding of Earth’s formation and subsequent evolution. This session encourages abstract submissions dealing with e.g., [1] the relationship between the geochemistry of mid-ocean ridge and ocean island basalts and seismically observed features in the mantle, [2] the geochemistry of mantle end-members and how they relate to the origin and distribution of chemical variability in the deep mantle, and [3] whether the formation and preservation of ancient, chemically distinct components in the Earth’s deep interior is compatible with a dynamically convecting mantle. Study of the deep Earth is inherently multidisciplinary, and we encourage abstract submissions from all realms of the geosciences (e.g., petrology and geochemistry, geophysics, mineral physics, geodynamics).
Primary Convener: Curtis D Williams, University of California Davis, Department of Earth and Planetary Sciences, Davis, CA, United States
Conveners: Matthew G Jackson, University of California Santa Barbara, Earth Science, Santa Barbara, CA, United States, Elizabeth Cottrell, Smithsonian, NMNH, Department of Mineral Sciences, Washington, DC, United States and Pilar Madrigal, Virginia Polytechnical Institute and State University, Department of Geosciences, Blacksburg, VA, United States
Chairs: Elizabeth Cottrell, Smithsonian, NMNH, Department of Mineral Sciences, Washington, DC, United States, Curtis D Williams, University of California Davis, Department of Earth and Planetary Sciences, Davis, CA, United States, Matthew G Jackson, University of California Santa Barbara, Earth Science, Santa Barbara, CA, United States and Pilar Madrigal, Virginia Polytechnical Institute and State University, Department of Geosciences, Blacksburg, VA, United States
OSPA Liaison: Curtis D Williams, University of California Davis, Department of Earth and Planetary Sciences, Davis, CA, United States
Index Terms:
1038 Mantle processes [GEOCHEMISTRY]
Abstracts Submitted to this Session:
182W in Modern Ocean Island Basalts (179641)
See more of: Study of Earth's Deep Interior
