Marine Geophysics

In the summer of 2008, researchers and students at UTIG will be sailing on the R/V Marcus Langseth to acquire marine geophysical data across the Yakutat block. The funded survey includes two reflection-refraction profiles, one down the long-axis of the exposed block and one crossing it and the proximal Pacific plate, and two grids of reflection data over fault zones that may be regionally significant. The seismic source will be received on the Langseth's 8 km digital, solid streamer for the reflection work and on a series of Ocean Bottom Seismometers (OBS) offshore and Texan seismometers onshore for the refraction work. The goals of the experiment are to: 1) Determine the type of crust that makes up the Yakutat block to test competing models of plateau subduction versus continental-oceanic accretion, 2) Examine the connections at depth between well-known surface structures such as the Pamplona Zone, the Kayak Island fault zone, and their onshore extensions and the deeper architecture of the collision, and 3) To investigate the role of glacial erosion and sediment transport in influencing mountain building. In preparation for this work researcher Sean Gulick, student Lindsay Lowe, and their colleagues are analyzing the deformation recorded on previously acquired industry, USGS, and high-resolution academic seismic data sets. The STEEP project and allied investigations are providing the framework for proposed Integrated Ocean Drilling Program (IODP) expeditions to study tectonic-climate interactions in the Gulf of Alaska.


R/V Marcus Langseth