Evidence of slumping/sliding in Krishna–Godavari offshore basin due to gas/fluid movements |
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| Institution: | 1. U.S. Geological Survey, Santa Cruz, CA, 95060, United States;2. U.S. Geological Survey, Denver, CO, 80203, United States;1. CSIR-National Institute of Oceanography, Goa 403004, India;2. Directorate General of Hydrocarbons, Noida, U.P 201301, India;1. Department of Petroleum and Mining Engineering, Jashore University of Science and Technology, Jashore, 7408, Bangladesh;2. Atmosphere and Ocean Research Institute (AORI), the University of Tokyo, Kashiwanoha 5-1-5, Chiba, 277-8564, Japan;3. Department of Geoscience, Shimane University, 1060 Nishikawatsu, Matsue, 690-8504, Japan;4. Estuary Research Center, Shimane University, Nishikawatsu-cho 1060, Matsue, 690-8504, Japan;5. Department of Earth Sciences, University of Southern California, 3651 Trousdale Pkwy, Los Angeles, CA, 90089, USA;6. Faculty of Applied Sciences, Uva Wellassa University, Passara Road, Badulla, 90000, Sri Lanka |
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| Abstract: | The Krishna–Godavari (KG) offshore basin is one of the promising petroliferous basins of the eastern continental margin of India. Drilling in this basin proved the presence of gas hydrate deposits in the shallow marine sediments beyond 750 m water depths, and provided lithologic and stratigraphic information. We obtained multibeam swath bathymetry covering an area of about 4500 km2 in water depths of 280–1800 m and about 1260 line km of high resolution seismic (HRS) records. The general lithology of midslope deposits is comprised of nannofossil-rich clay, nannofossil-bearing clay and foraminifera-bearing clay. The HRS records and bathymetry reveal evidence of slumping and sliding of the upper and midslope sediments, which result in mass transport deposits (MTD) in the northwestern part of the study area. These deposits exhibit 3–9.5 km widths and extend 10–13 km offshore. The boundaries of the MTDs are often demarcated by sharp truncation of finely layered sediments (FLS) and the MTDs are characterized by acoustically transparent zones in the HRS data. Average thickness of recent MTDs varies with depth, i.e., in the upper slope, the thickness is about 45 m, while in the lower slope it is about 60 m, and in deeper offshore locations they attain a maximum thickness of about 90 m. A direct indication for slumping and mass transportation of deposits is provided by the age reversal in 14C AMS dates observed in a sediment core located in the midslope region. Seismic profiling signatures provide indications of fluid/gas movement. We propose that the presence of steep topographic gradients, high sedimentation rates, a regional fault system, diapirism, fluid/gas movement, and neotectonic activity may have facilitated the slumping/sliding of the upper slope sediments in the KG offshore basin. |
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