DI41D:
G, LAB, and MLDs: What Are They Anyway? Lithospheric Boundary Structures within and beneath the Oceans and Continents I
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DI41D:
G, LAB, and MLDs: What Are They Anyway? Lithospheric Boundary Structures within and beneath the Oceans and Continents I
G, LAB, and MLDs: What Are They Anyway? Lithospheric Boundary Structures within and beneath the Oceans and Continents I
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#: 16720
Session Description:
Recent advances in seismic imaging suggest that that the internal structure of the rigid outer layer of the Earth, the lithosphere, appears to have appears more complex than a single boundary layer. Seismology, numerical modeling, mineral, and rock physics, each provide clues about the origins of these structures.
Just what can we discern from the G, LAB and MLDs? Is it significant that they occur around the same depths within the ocean and continental lithosphere? Or is that just a coincidence?
The session seeks submissions from a variety of disciplines to help define and clarify both global and regional lithospheric boundary structures inferred from observations, models, and experiments. Multidisciplinary approaches that help better understand the structure and evolution of the plates are encouraged.
Primary Convener: Meghan Samanth Miller, University of Southern California, Department of Earth Sciences, Los Angeles, CA, United States
Conveners: Catherine M Cooper, Washington State University, School of the Environment, Pullman, United States, Philip A Skemer, Washington University in St Louis, St. Louis, MO, United States and Caroline Beghein, University of California Los Angeles, Earth, Space, and Planetary Sciences, Los Angeles, CA, United States
Chairs: Meghan Samanth Miller, University of Southern California, Department of Earth Sciences, Los Angeles, CA, United States and Philip A Skemer, Washington University in St Louis, St. Louis, MO, United States
OSPA Liaison: Philip A Skemer, Washington University in St Louis, St. Louis, MO, United States
Cross-Listed:
- S - Seismology
- T - Tectonophysics
Index Terms:
1025 Composition of the mantle [GEOCHEMISTRY]
7218 Lithosphere [SEISMOLOGY]
8103 Continental cratons [TECTONOPHYSICS]
8124 Earth's interior: composition and state [TECTONOPHYSICS]
Abstracts Submitted to this Session:
Constraints on the radially anisotropic component of seismic discontinuities at 60-100 km depth (188568)
Imaging lithospheric seismic discontinuities beneath Cascadia using S-to-P receiver functions (189197)
See more of: Study of Earth's Deep Interior
