The available geological and thermodynamic data, essential for the formatio
n and accumulation of gas hydrates, have been integrated and broadly interp
reted for the deeper waters of India. The preliminary studies indicate that
, in all probability, vast gas hydrate resources exist in the shallow sedim
ents under deep waters.
The area of the Bay of Bengal and Arabian Sea, off the coast of India and A
ndaman Islands, have accumulated thick sediments, over 22 and 10 km, respec
tively, during collision of the Indian Plate with the Tibetan Plate.
Bottom Simulating Reflectors (BSRs), indicating the likely presence of gas
hydrates, have been observed from multichannel and single-channel seismic r
eflection data west of the Andaman Islands and Kerala-Konkan offshore. The
Indian continental shelf, slope, and rise areas have, at places, shown the
presence of gas-charged sediments and gas seeps through faults. There are c
ommercial oil and gas fields in the shallow water of both the east and west
coasts of India. These are indicative of generation of both biogenic as we
ll as thermogenic gases in the offshore areas of India.
For the first time, an attempt has been made to estimate in- place gas hydr
ate resources under deep water of India beyond 600 m water depth to the leg
al continental shelf boundary, and the the Andaman Islands. The gas hydrate
resources appear to be vast, and require extensive exploratory efforts for
their precise mapping and quantitative assessment.