Asthenospheric and Lithospheric Broadband Architecture from the

California Offshore Region Experiment

(ALBACORE)

Objectives
The objective of this project is to understand the tectonic interaction at the Pacific-North America plate boundary by identifying the physical properties and deformation styles of the Pacific plate and nearshore microplates. The results will be used to distinguish among contrasting upper mantle geodynamic scenarios that predict large-scale mantle flow patterns beneath western North America. Seismic studies using broadband ocean bottom seismometer (OBS) data will characterize the driving plate motion consequences of collision between the rift system, a fragmented subducted plate, the lengthening of the San Andreas transform fault system, and block rotations. The boundaries for the seismic array overlap the region of complex breakup and fracture of the Pacific plate near shore where several microplates are observed, and extend far to the west to provide comparison with oceanic lithosphere that is not fractured and has formed at a uniform rate. The results will aid in understanding the boundary forces due to relative plate motions, the driving forces and characteristics of oceanic and continental scale deformation, and how the continental margin accretionary process is influenced by offshore tectonics.

Experiment Design

Analysis Projects


People

Monica Kohler (Center for Embedded Networked Sensing, UCLA)
Dayanthie Weeraratne (Dept. of Geological Sciences, CSU Northridge)
Natsumi Shintaku (Dept. of Geological Sciences, CSU Northridge)


Publications, posters, and abstracts


Related links

U.S. National Ocean Bottom Seismograph Instrument Pool (OBSIP)
University-National Oceanographic Laboratory System (UNOLS)
Scripps Institute of Oceanography Ship Operations (SIO Ship Operations)
National Geophysical Data Center: Marine Geology and Geophysics (NGDC-MGG)
GMT Supplemental Man pages (GMT Supplemental)
MB-System manual (MB-System)
Southern California Earthquake Center (SCEC)

Funded by the National Science Foundation, Division of Ocean Sciences in the Geosciences Directorate