
Categorization Of Sedimentary Basins

| Category |
Basin |
Basinal Area (Sq. Km.)
|
Total |
UPTO 200M |
ISOBATH |
On land |
Offshore |
|
I |
Cambay |
51,000
|
2,500 |
53,500
|
|
Assam Shelf |
56,000 |
- - - - |
56,000 |
|
Bombay offshore |
- - - - |
116,000 |
116,000 |
|
Krishna Godavari |
28,000 |
24,000 |
52,000 |
|
Cauvery |
25,000 |
30,000 |
55,000 |
|
Assam-Arakan Fold Belt
|
60,000 |
- - - - |
60,000 |
|
Rajasthan |
126,000 |
- - - - |
126,000 |
|
SUB. TOTAL |
346,000
|
172,500
|
518,500
|
II |
Kutch |
35,000 |
13,000 |
48,000 |
| |
Mahanadi-NEC |
55,000 |
14,000 |
69,000 |
|
Andaman-Nicobar |
6,000 |
41,000 |
47,000 |
|
SUB. TOTAL |
96,000
|
68,000
|
164,000
|
III |
Himalayan Foreland |
30,000 |
- - - - |
30,000 |
|
Ganga |
186,000 |
- - - - |
186,000 |
|
Vindhyan |
162,000 |
- - - - |
162,000 |
| |
Saurashtra |
52,000 |
20,000 |
80,000 |
|
Kerala-Konkan-Lakshadweep
|
- - - - |
94,000 |
94,000 |
|
Bengal |
57,000 |
32,000 |
89,000 |
|
SUB. TOTAL |
542,000
|
168,000
|
710,000
|
IV |
Karewa |
3,700 |
- - - - |
3,700 |
|
Spiti-Zanskar |
22,000 |
- - - - |
22,000 |
|
Satpura-South Rewa-Damodar
|
46,000 |
- - - - |
46,000 |
|
Narmada |
17,000 |
- - - - |
17,000 |
|
Decan Syneclise |
273,000 |
- - - - |
273,000 |
|
Bhima-Kaladgi |
8,500 |
- - - - |
8,500 |
|
Cuddapah |
39,000 |
- - - - |
39,000 |
|
Pranhita-Godavari |
15,000 |
- - - - |
15,000 |
|
Bastar |
5,000 |
- - - - |
5,000 |
|
Chhattisgarh |
32,000 |
- - - - |
32,000 |
|
SUB. TOTAL |
461,200
|
- - - -
|
461,200
|
|
TOTAL |
1,390,200
|
394,500
|
1,784,
700 |
DEEP WATERS
|
|
Kori-Comorin J |
|
|
|
|
85° E |
- - - - |
- - - - |
1,350,000
|
|
Narcodam |
|
|
|
|
GRAND TOTAL |
- - - - |
- - - - |
3,134, 700 |
* Categorization based on the prospectivity
of the basin as presently known. The four recognized
categorie are basins which have:
- Established commercial production
- Known accumulation of hydrocarbons but no
commercial production as yet
- Indicated hydrocarbon shows that are considered
geologically prospective
- Uncertain potential which may be prospective
by analogy with similar basins in the world.
This categorization will necessarily change with the results
of further exploration.
|