• DocumentCode
    2851323
  • Title

    Geologic characteristics in the vicinity of the Deepwater Horizon oil spill

  • Author

    McGee, T.

  • Author_Institution
    Center for Marine Resources & Environ. Technol., Univ. of Mississippi, Oxford, MS, USA
  • fYear
    2010
  • fDate
    24-27 Aug. 2010
  • Firstpage
    1
  • Lastpage
    5
  • Abstract
    On April 20, 2010, the Deepwater Horizon offshore drilling rig experienced a catastrophic explosion and fire. At the time, it was drilling about 70km southeast of the mouth of the Mississippi River. A couple of days later it lay on the sea floor in more than 1500m of water. The drilling riser that extended from the sea floor to the water surface was destroyed and the blow-out preventer malfunctioned, causing a massive leak of crude oil and natural gas. Early attempts by British Petroleum (BP) and its drilling sub-contractors failed to cap the well. It continued to flow, at times intermittently, for more than 100 days. In total, it is estimated that at least five million barrels of oil were released into the Gulf of Mexico, undoubtedly the largest oil spill in U.S. history. Due to the proprietary nature of petroleum exploration and production, few details have been made public concerning the well from which the Deepwater Horizon spill originated. There is information about the geologic characteristics in the general vicinity of that well site, however.
  • Keywords
    bathymetry; hydrocarbon reservoirs; seafloor phenomena; AD 2010 04 20; Deepwater Horizon offshore drilling rig; Deepwater Horizon oil spill; GoMHRC; Gulf of Mexico Hydrate Research Consortium; Mississippi Canyon Block 118; hydrate-carbonate mound; petroleum exploration; petroleum production; well site vicinity geologic characteristics; Earthquakes; Fluids; Petroleum; Reflection; Sea floor; Sediments; Vents;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    Baltic International Symposium (BALTIC), 2010 IEEE/OES US/EU
  • Conference_Location
    Riga
  • ISSN
    2150-6027
  • Print_ISBN
    978-1-4244-9226-8
  • Electronic_ISBN
    2150-6027
  • Type

    conf

  • DOI
    10.1109/BALTIC.2010.5621655
  • Filename
    5621655