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90-day Monitoring Report - National Marine Fisheries Service - NOAA

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Figure 1. Location of the Coakley marine geophysical survey in the Arctic Ocean (LGL EA, 2011).<br />

The purpose of the study is to collect seismic reflection data across the transition from the<br />

Chukchi Shelf to the Chukchi Borderland to image the structures that separate these two large<br />

continental blocks. The data from this study will be used to test existing tectonic models and<br />

develop new constraints on the development of the Amerasian Basin, and will substantially<br />

advance the knowledge about the Mesozoic history of this basin. In addition, the seismic data<br />

collected will enable the formulation of new tectonic models for the history of this region, which<br />

will be used to improve our understanding of the surrounding continents.<br />

2.1.1. Energy Source<br />

The acoustic source used during the Coakley 2D marine geophysical survey in the Arctic Ocean<br />

consisted of one towed airgun array and one hydrophone streamer cable. The array was<br />

deployed centrally astern of the vessel. While only one array was firing at a time, two arrays<br />

were interchanged when maintenance was needed so that production could continue. The<br />

airguns arrays were towed at a depth of six meters and were situated either 83.3 meters or<br />

103.3 meters from the Navigational Reference Point (NRP), which was located on the PSO<br />

observation tower. Whenever the arrays were exchanged the PAM operator would notify the<br />

visual PSOs so that they were always aware of the safety radii. The first acoustic source array<br />

that was deployed was being towed at a depth of nine meters, however it was noticed that the<br />

IHA was granted for an array towed at six meters depth and the array was switched out at 20:45<br />

UTC on 15 September 2011 for an array towed at six meters depth.<br />

UME04085<br />

R.V Marcus G. Langseth<br />

L-DEO/NMFS<br />

05 January 2012<br />

3

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