Seismic research cruise provides new data on US Atlantic margin gas hydrates

September 20, 2018, United States Geological Survey
The Mid-Atlantic Resource Imaging Experiment (MATRIX) collected reflection seismic data along more than 2000 km of trackline shown in yellow. Black tracklines show transit lines where no seismic data were acquired, and orange crosses denote sonobuoy deployments. Purple areas were identified by BOEM based on legacy seismic data and show possible gas hydrate accumulations. Red symbols mark seafloor methane seeps, and the black and white circles represent exploratory wells drilled in the 1970s and 1980s. Names at the edge of the shelf refer to the major shelf-break submarine canyons. Credit: Bathymetric base map from B. Andrews.

Data acquired by the U.S. Geological Survey on the U.S. Atlantic margin in August 2018 reveal new information about the distribution of gas hydrates in the sector stretching from the upper continental slope to deep water areas offshore New Jersey to North Carolina. The Mid-Atlantic Resource Imaging Experiment (MATRIX), which was jointly sponsored by the USGS Coastal/Marine Hazards and Resources Program (CMHRP), the Methane Hydrates R&D Program at the Department of Energy, and the Bureau of Ocean Energy Management, acquired more than 2,000 kilometers (about 1,240 statute miles) of marine seismic data that image gas hydrate features and other geologic structures below the seafloor.

Gas forms naturally in seafloor sediments when methane and water combine at moderate pressures and relatively low temperatures. Gas hydrate deposits resemble ice, and they concentrate enormous amounts of methane in the global oceans and in permafrost areas. On the U.S. Atlantic margin, BOEM had previously identified potential deep water gas hydrate accumulations that guided planning for MATRIX. In fact, the sediments of deep marine continental margins host nearly 99 percent of the world's gas hydrate.

The MATRIX data image 1 to 3 km (about 3,300 to 9,800 ft) below the seafloor and provide new information about the distribution of a key seismic indicator linked to the presence of gas hydrate. The data also reveal shallow gas deposits and structural features beneath some of the hundreds of seafloor methane seeps discovered along the Atlantic margin since 2011 and image submarine landslide deposits, shallow faults, and sedimentary markers considered important in interpreting the history of the Atlantic Ocean basin to inform assessment of geologic hazards along the eastern seaboard.

During MATRIX, USGS scientists and operational staff from CMHRP were joined by BOEM scientists, protected species visual observers, and outside technicians aboard the research vessel (R/V) Hugh R. Sharp, which is owned and operated by the University of Delaware as part of the University-National Oceanographic Laboratory System.

USGS scientist Jenny White McKee watches as an expendable sonobuoy leaves the launcher during the 2018 MATRIX cruise on the R/V Hugh R. Sharp. The sonobuoy deploys an antenna used to transmit received seismic signals back to the ship over radio frequencies at distances up to 15 km away. Credit: Carolyn Ruppel, USGS.

Up to four airguns were used to generate the acoustic energy for imaging seafloor sediments. The seismic signals were recorded by 112 to 160 receivers towed behind the ship and arrayed within a streamer up to 1.2 kilometers (0.75 miles) long. The USGS also deployed 60 sonobuoys, which are expendable instruments that receive seismic signals and transmit the information back to the ship at distances up to 15 km (9.3 miles).

Renee Orr, Chief of BOEM's Office of Strategic Resources commented, "MATRIX presented an opportunity to acquire modern seismic data to refine understanding of on the U.S. Atlantic margin in areas that both BOEM and the USGS have previously identified as worthy of study."

Lou Capitanio, program manager for DOE's Methane Hydrates program, added that, "MATRIX also represented an important step in addressing interagency priorities to identify deep water gas hydrate deposits on U.S. marine margins."

MATRIX Chief Scientists Carolyn Ruppel and Nathan Miller, both marine geophysicists with the USGS, credited excellent weather and a favorable Gulf Stream current as key factors in the success of the seismic cruise. Researchers acquired six seismic lines running down the continental slope from the shelf-break to waters as deep as 4,000 meters (about 13,100 ft) offshore New Jersey, Delaware, Maryland, Virginia, and North Carolina. MATRIX also completed three upper continental slope lines and three (more than 2,700 meters water depth) lines oriented parallel to the coastline in this sector.

USGS personnel on the deck of the R/V Hugh R. Sharp during retrieval of seismic airguns. The streamer that receives the seismic signals generated by the airguns is towed behind the ship and is here shown spooled on the winch at right. Credit: Carolyn Ruppel, USGS.

John Haines, Program Coordinator for USGS CMHRP, noted that the MATRIX effort "engaged scientific, technical, and operations staff across our USGS Program and marked the first time since the 1990s that CMHRP has independently conducted a regional-scale seismic project with airgun sources. The multiagency collaboration that contributed to the success of MATRIX is an excellent model for marine seismic programs that support mission-related research objectives."

In addition to the scientific partnership among the USGS Gas Hydrates Project, DOE, and BOEM, MATRIX benefited from logistical support provided by Scripps Institute of Oceanography, Lamont-Doherty Earth Observatory, and the National Science Foundation. The National Marine Fisheries Service of the National Oceanic and Atmospheric Administration supported environmental compliance and permitting under the Marine Mammal Protection Act and the Endangered Species Act.

The USGS Gas Hydrates Project focuses on the energy resource potential of gas hydrates, the interaction between hydrates and the environment, and connections between gas hydrates and geohazards like submarine landslides. MATRIX produced data that will, for years to come, facilitate studies in all of these areas and support broader analyses of the margin's hazards, stratigraphy, and deep structure by the USGS, other agencies, and the academic community.

Explore further: Stable gas hydrates can trigger landslides

Related Stories

Stable gas hydrates can trigger landslides

February 21, 2018

Like avalanches onshore,many processes cause submarine landslides. One very widespread assumption is that they are associated with dissociating gas hydrates in the seafloor. However, scientists at GEOMAR Helmholtz Centre ...

Why did gas hydrates melt at the end of the last ice age?

February 13, 2018

Methane hydrates, also known as "burning ice," occur at all ocean margins. The compound of gas and water occurs in the seafloor and it is only stable under relatively high pressures and low temperatures. If the pressure is ...

Recommended for you

0 comments

Please sign in to add a comment. Registration is free, and takes less than a minute. Read more

Click here to reset your password.
Sign in to get notified via email when new comments are made.