ROCKMAN wrote:Interesting map...thanks. As I don't know much about other global basins it does make me wonder how many other Deep Water depo centers with hydrocarbon potential are out there which haven’t been tested at all. It was easy for the industry to jump into the DW GOM or move eastward from the shallower Brazil waters. Without the associated shallow water plays I wonder how many Deep Water basins haven't been given even basic evaluations. I think some folks have done some poking around Deep Water India but consider the sediment source of the Himalayas vs. the Miss River. Food for thought.
ROCKMAN wrote:I think some folks have done some poking around Deep Water India but consider the sediment source of the Himalayas vs. the Miss River. Food for thought.
ONGC had earlier discovered gas from the same block which is adjacent to Reliance Industries’ KG-DWN-98/3 where RIL had made the country’s biggest gas discovery. The ONGC discovery reaffirms the abundance of oil in the country’s east coast. RIL has also started producing oil from KG-DWN-98/3, popularly called D-6.
KG basin is turning out to be India’s Gulf of Mexico, with major oil and gas discoveries made by RIL, ONGC and Gujarat State Petroleum Corporation (GSPC), said an oil expert.
ROCKMAN wrote:OF2 -- Plenty of time. I'm not an oil generation expert but it doesn't take but a few million years and relatively shallow burial to generate considerable amounts of oil. Decades ago I read a report that detailed most of the GOM oil was generated within 3000' of burial. The Middle East oil is much older but but the Ganges delta systems would be a direct anaology to the Miss. River deltas. I see no reason not to expect similar source rocks over there also. I don't have the details but the Miss. River has been dumping into the GOM for at least 100 million years which I suspect is a similar time frame to the Ganges. I don't have any info on the subsea topography but I suspect you get into fairly Deep Water not too far offshore. More like W Africa then the GOM. Thus water depth may have been the barrier to development all this time.
dorlomin wrote:But why is so much of that oil and gas what is now offshore? The sea level was a good 70 meters higher for most of the past 100 million years.
ROCKMAN wrote: I don't have the details but the Miss. River has been dumping into the GOM for at least 100 million years which I suspect is a similar time frame to the Ganges.
ROCKMAN wrote:Dorlomin
If I understand your question I’ll use the Gulf of Mexico as an example. There are vast regions around the globe called geosynclines. Think of them as giant bowls (1 million sq miles) which have been slowly sinking over 10’s of millions of years. The area of the US coast along the Gulf of Mexico is one such geosyncline. One can drill a well today a mile off of the Louisiana coast in 5’ of water and go 20,000’ feet down. There you would find a sandstone that was deposited in 5’ of water. Thus since the time that sandstone was deposited the region had sunk 20,000’. I’m not sure what the current estimate is for the total thickness of sediments in the GOM geosyncline but I would imagine it’s in excess of 50,000’ (7 miles). The land along the Gulf Coast continues to sink today but only at a fraction of an inch per year. Sea level does rise and fall significantly over geologic time but relative land movement (up like mountain building or down like geosynclines) has a much greater impact of the geologic record.
ROCKMAN wrote:Maybe I didn't get the memo OF2. What exactly do you kids call those massive depo centers these days.
Geosyncline theory is an obsolete concept involving vertical crustal movement that has been replaced by plate tectonics to explain crustal movement and geologic features. Geosyncline is a term still occasionally used for a subsiding linear trough that was caused by the accumulation of sedimentary rock strata deposited in a basin and subsequently compressed, deformed, and uplifted into a mountain range, with attendant volcanism and plutonism.
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