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Basin Configuration in Konkan Deepwaters: Western Indian Offshore


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1 Deepwater Exploration Group, EBG, Mumbai Regional Business Centre, ONGC, Mumbai, India
     

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The sedimentary patch in Konkan deepwaters, located west of the Konkan continental shelf contains over 3 km thick sediments. Based upon the interpretation of over 11,000 line km of seismic data, gross basin configuration model has been worked out. The basin floor at the base of Tertiary is differentiated into a series of rift zones containing synrift sediments. These zones are superimposed by post-rift sediments deposited as a result of flexurally distributed thermal subsidence. Therefore, the sediments in the basin are divisible into three distinct mega-seismic packages denoting three major tectonic habitats of the evolution of the Konkan continental margin. Based upon the basinal configuration of each mega-seismic package in space and time, tectono-sedimentary evolution of the continental margin is brought out with an assessment of hydrocarbon prospects.

Keywords

Marine Geophysics, Seismic Data, Rift Tectonics, Hydrocarbon Prospects, Western Indian Continental Shelf.
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  • Basin Configuration in Konkan Deepwaters: Western Indian Offshore

Abstract Views: 182  |  PDF Views: 2

Authors

Sanjeev S. Thakur
Deepwater Exploration Group, EBG, Mumbai Regional Business Centre, ONGC, Mumbai, India
R. T. Arasu
Deepwater Exploration Group, EBG, Mumbai Regional Business Centre, ONGC, Mumbai, India
V . S. R. Subhramanyam
Deepwater Exploration Group, EBG, Mumbai Regional Business Centre, ONGC, Mumbai, India
A. K. Srivastava
Deepwater Exploration Group, EBG, Mumbai Regional Business Centre, ONGC, Mumbai, India
A .V. S. Murthy
Deepwater Exploration Group, EBG, Mumbai Regional Business Centre, ONGC, Mumbai, India

Abstract


The sedimentary patch in Konkan deepwaters, located west of the Konkan continental shelf contains over 3 km thick sediments. Based upon the interpretation of over 11,000 line km of seismic data, gross basin configuration model has been worked out. The basin floor at the base of Tertiary is differentiated into a series of rift zones containing synrift sediments. These zones are superimposed by post-rift sediments deposited as a result of flexurally distributed thermal subsidence. Therefore, the sediments in the basin are divisible into three distinct mega-seismic packages denoting three major tectonic habitats of the evolution of the Konkan continental margin. Based upon the basinal configuration of each mega-seismic package in space and time, tectono-sedimentary evolution of the continental margin is brought out with an assessment of hydrocarbon prospects.

Keywords


Marine Geophysics, Seismic Data, Rift Tectonics, Hydrocarbon Prospects, Western Indian Continental Shelf.