Minerals Report - International Seabed Authority
Minerals Report - International Seabed Authority Minerals Report - International Seabed Authority
The extremely harsh environment brought up the necessity to create extra high tensile steel or concrete floating and fixed producing platforms for the development of deepwater oil and gas fields in the North and Norwegian seas. Therefore the fields discovered as far back as the late 1970s – early 1980s were brought on-stream only in the mid-1990s. Of the 14 known hydrocarbon fields, three are currently producing, Snorre, Troll West, and Heidrun, with total reserves of 285 Mmt oil and 45 Gm 3 gas and a total annual output of 29 Mmt oil. In West Africa, deepwater offshore exploratory drilling began in the mid-1990s in Angola and then extended into the deepwater areas of some other countries. Deepwater offshore hydrocarbon exploration was most successful in Angola where 21 fields, including four large ones, had been discovered by 01.01.2000 (figure 11) 12 . The total reserves in place of these discoveries are estimated as almost 600 Mmtoe. The Kuito discovery was brought onstream first, late in 1999, and the other one, Girassol (in 1350 m of seawater) is due on-stream in 2001. Figure 11: Angola offshore concession blocks and fields (modified from Raposo 12) INTERNATIONAL SEABED AUTHORITY 504
Ten deepwater offshore discoveries have been made in Nigeria, including the Agbami field with a recoverable reserve of 240 Mmt under 1460-1516 m of sea water, which is the largest discovery during the whole hydrocarbon exploration history of the country. It should be noted that offshore exploration blocks under up to 4000 m of seawater have been recently offered here (figure 12). Six more discoveries were made in the deep offshore areas of Congo and Equatorial Guinea. The total number of deepwater offshore discoveries made in West Africa by 01.01.2000 is 37. In terms of deepwater offshore exploration intensity and success, this region is second only to the Gulf of Mexico. INTERNATIONAL SEABED AUTHORITY 505
- Page 462 and 463: 48. J. -P. Lenoble (1996), Les nodu
- Page 464 and 465: 66. J. -J. Prédali and J. -P. Polg
- Page 466 and 467: classification system, Mr. Lenoble
- Page 468 and 469: To recapitulate the sizes and possi
- Page 470 and 471: proposed processing technologies an
- Page 472 and 473: international community is only jus
- Page 474 and 475: Part 2 ISSUES TO BE TAKEN INTO ACCO
- Page 476 and 477: The Secretary-General said that the
- Page 478 and 479: Mr. Nandan pointed out that the nex
- Page 480 and 481: problems would resurface, because i
- Page 482 and 483: prospecting would be more applicabl
- Page 484 and 485: dimensional seafloor massive sulphi
- Page 486 and 487: workshop, in relation to deposit ev
- Page 488 and 489: an economic perspective, including
- Page 490 and 491: sulphides and cobalt-rich ferromang
- Page 492 and 493: CHAPTER 13 PETROLEUM POTENTIAL AND
- Page 494 and 495: structure and filled with sediments
- Page 496 and 497: Basin groups are subdivided into ty
- Page 498 and 499: during the late Mesozoic-Cenozoic s
- Page 500 and 501: Figure 4: Volume density of initial
- Page 502 and 503: ITIPRHC = Vnr φHC γ 103 (Mmtoe),
- Page 504 and 505: Table 1: Offshore (deepwater) initi
- Page 506 and 507: Speaking about particular geographi
- Page 508 and 509: World Ocean, including areas off no
- Page 510 and 511: Table 4: Largest oil and gas discov
- Page 514 and 515: In other regions of the world, enco
- Page 516 and 517: REFERENCES 1. L.G. Weeks (1971), Ma
- Page 518 and 519: SUMMARY OF PRESENTATION AND DISCUSS
- Page 520 and 521: Dr. Vysotsky said that estimates of
- Page 522 and 523: In Southeast Asia, Dr. Vysotsky spo
- Page 524 and 525: Philippines, and possibly Brazil. W
- Page 526 and 527: and we shall encounter severe deple
- Page 528 and 529: In the 1960's scientists discovered
- Page 530 and 531: Figure 2. Worldwide locations of kn
- Page 532 and 533: methane by bacteria in an anoxic en
- Page 534 and 535: It has been assumed that the struct
- Page 536 and 537: identification of gas hydrate in ma
- Page 538 and 539: ottom simulating reflections (BSR)
- Page 540 and 541: Figure 6: Interpretative plot of hy
- Page 542 and 543: floor have indicated the presence o
- Page 544 and 545: of free gas below the BSR is usuall
- Page 546 and 547: sediment and to provide an indicati
- Page 548 and 549: 6. Harvesting methane hydrates -Som
- Page 550 and 551: deposits can be commercial, even in
- Page 552 and 553: at a catastrophic scale. Some of th
- Page 554 and 555: Figure 8. Development of hydrate re
- Page 556 and 557: This is perhaps due to the percepti
- Page 558 and 559: would provide Japan with methane fo
- Page 560 and 561: NOTES AND REFERENCES 1. E.D. Sloan
The extremely harsh environment brought up the necessity to<br />
create extra high tensile steel or concrete floating and fixed producing<br />
platforms for the development of deepwater oil and gas fields in the North<br />
and Norwegian seas. Therefore the fields discovered as far back as the late<br />
1970s – early 1980s were brought on-stream only in the mid-1990s. Of the<br />
14 known hydrocarbon fields, three are currently producing, Snorre, Troll<br />
West, and Heidrun, with total reserves of 285 Mmt oil and 45 Gm 3 gas and<br />
a total annual output of 29 Mmt oil.<br />
In West Africa, deepwater offshore exploratory drilling began in<br />
the mid-1990s in Angola and then extended into the deepwater areas of<br />
some other countries.<br />
Deepwater offshore hydrocarbon exploration was most successful<br />
in Angola where 21 fields, including four large ones, had been discovered<br />
by 01.01.2000 (figure 11) 12 . The total reserves in place of these discoveries<br />
are estimated as almost 600 Mmtoe. The Kuito discovery was brought onstream<br />
first, late in 1999, and the other one, Girassol (in 1350 m of<br />
seawater) is due on-stream in 2001.<br />
Figure 11: Angola offshore concession blocks and fields (modified from Raposo 12)<br />
INTERNATIONAL SEABED AUTHORITY 504