K Schumann, D Völker, WR Weinrebe - Quaternary Science Reviews, 2012 - Elsevier
A ship-based acoustic mapping campaign was conducted at the exit of Ilulissat Ice Fjord of West Greenland and in the sedimentary basin of Disko Bay west of the fjord mouth …
A Ismail, HF Ewida, MG Al-Ibiary, S Nazeri… - Exploration …, 2021 - Taylor & Francis
The West Delta Deep Marine (WDDM) concession is one of the abundant natural gas resources in the world characterised by the presence of several active gas chimneys conduit …
L Wang, F Zhao, E Miramontes - Marine and Petroleum Geology, 2024 - Elsevier
Pockmarks are prominent morphological features formed by fluid escape at the seafloor that provide valuable information on past environmental conditions and ongoing sedimentary …
Submarine groundwater discharge into coastal areas is a common global phenomenon and is rapidly gaining scientific interest due to its influence on marine ecology, the coastal …
Pockmarks form by gas/fluid expulsion into the ocean and are preserved under conditions of negligible sedimentation. Ideally, they are circular at the seafloor and symmetrical in profile …
K Zhang, Y Guan, H Song, W Fan, H Li… - Marine Geophysical …, 2020 - Springer
Pockmarks consists of depressions on the seafloor and are often considered to originate from fluid escape activities. In this study, we report 125 pockmarks near the Andu Seamount …
The genesis of submarine channels is often controlled by gravity flows, but channels can also be formed by oceanographic processes. Using multibeam bathymetry and two …
X Li, X Guo, F Tian, X Fang - Journal of Marine Science and Engineering, 2024 - mdpi.com
Submarine pockmarks are typical indicators of submarine gas escape activity. The deep strata of the Xisha Uplift are rich in biogenic and thermogenic gas, accompanied by strong …