Xu, Cuiling, Greinert, Jens , Haeckel, Matthias , Bialas, Jörg , Dimitrov, L. and Zhao, Guangtao (2018) The Character and Formation of Elongated Depressions on the Upper Bulgarian Slope. Journal of Ocean University of China, 17 (3). pp. 555-562. DOI 10.1007/s11802-018-3460-7.

Preview	Text Xu et.al.pdf - Accepted Version Download (1MB) | Preview
	Text Xu.pdf - Published Version Restricted to Registered users only Download (1MB) | Contact

Abstract

Seafloor elongated depressions are indicators of gas seepage or slope instability. Here we report a sequence of slope-parallel elongated depressions that link to headwalls of sediment slides on upper slope. The depressions of about 250 m in width and several kilometers in length are areas of focused gas discharge indicated by bubble-release into the water column and methane enriched pore waters. Sparker seismic profiles running perpendicular and parallel to the coast, show gas migration pathways and trapped gas underneath these depressions with bright spots and seismic blanking. The data indicate that upward gas migration is the initial reason for fracturing sedimentary layers. In the top sediment where two young stages of landslides can be detected, the slope-parallel sediment weakening lengthens and deepens the surficial fractures, creating the elongated depressions in the seafloor supported by sediment erosion due to slope-parallel water currents.

Actions (login required)

View Item