Delineation of Outer Limits of Continental Shelf

According to the provisions of UNCLOS, the coastal State that intends to delineate the outer limits of the continental shelf beyond 200 nautical miles, is required to submit particulars of such limits along with the supporting scientific and technical data. The claims are required to be submitted by May 2009 and would be examined by the Commission on the Limits of Continental Shelf (CLCS). If the claims are accepted by CLCS India would be in a position to claim substantial area beyond the EEZ.


The States submitting claims are required to determine the (a) baselines (b) foot of the continental slope and 2500 metre isobath, and  (c) thickness of sedimentary rocks to establish the outer limits of the continental shelf. Accordingly, a comprehensive desktop study was undertaken considering the data sources available to determine the scope of the project, the type of data to be collected, the scientific and technical issues involved and the development of a data acquisition programme in concert with the objectives of other programmes viz. Gas Hydrates Programme.  Upon identification of the requirement, a data acquisition programme was taken up and various sub-components of the programme viz. parameters of data acquisition, data quality protocol, cruise schedules, area of operation etc., were finalised.  The data acquisition of various geophysical parameters commenced during the year and is progressing with simultaneous data processing.  


National Centre for Antarctic and Ocean Research (NCAOR) at Goa, an autonomous body under the DOD, is coordinating this national endeavour with active co-operation and participation of all national institutions.

Objectives of the program are:

n    Determination of the total sediment thickness below the seabed along a series of transects normal to the foot of the slope and spaced less than 60 nautical miles apart, through seismic reflection, refraction, gravity and magnetic methods


n    Determination of the nature and type of the basement above which the sediments have been deposited through modeling of the MCS and refraction data