Minerals Report - International Seabed Authority
Minerals Report - International Seabed Authority Minerals Report - International Seabed Authority
CHAPTER 13 PETROLEUM POTENTIAL AND DEVELOPMENT PROSPECTS IN DEEP-SEA AREAS OF THE WORLD V. I. Vysotsky, Petroleum Institute JSC VNIIZarbezhgeologia, Moscow, Russian Federation A. I. Gloumov, Russian Ministry of Natural Resources Moscow, Russian Federation In the oil industry, the term “deepwater” is applied to the deeper parts of the World’s Oceans with water depths of more than 500m. At these depths, the offshore extensions of marginal sedimentary basins and, less frequently, oceanic-type basins are located. About 120 of the known 511 sedimentary basins of the world have volume-balance methods. The total recoverable oil and condensate reserves are 36 Gt; gas, 63 TM 3 . The bulk of resources occur in the basins along the Atlantic Ocean margins. Deepwater hydrocarbon exploration began in the 1980s. Exploration work was particularly active in the Campos basin (Brazil), Gulf of Mexico (US sector), and West Africa (Angola, Nigeria). By the end of the century, exploratory wells reached sea depths of 3000 m, and development wells, depths of 2000 m. By the beginning of 2000, a total of 190 oil and gas fields with aggregate reserves of about 3 Gtoe had been discovered in deepwater areas. In the next 5 years, deepwater oil expenditure will exceed $70 billion forecasted spending. 1. Introduction The term “deepwater” has become quite common at the present stage of offshore petroleum exploration and development, and it carries a geological, and technical and economic sense. Geologically, it refers to the deeper parts of the World’s Oceans with water depths greater than 500 m. Passive and active continental margins, trenches, island-arc slopes, the continental rise, and the deep-sea basins of the World’s Oceans are located at these depths. In some parts of the World’s Oceans, these zones exhibit considerable petroleum potential. From the technical and economic perspective, these areas are the offshore areas where fixed bottomsupported drilling or production platforms cannot be used. Hydrocarbon prospecting and development at these water depths require special technical means and economic estimates. INTERNATIONAL SEABED AUTHORITY 484
At present, the technical and economic limit for permanent offshore platforms is a water depth of 300 metres in the North Atlantic (North and Norwegian seas) and 450 metres, in regions with less harsh environments. In future, the depth limit for permanent offshore platforms may be extended by means of new, stronger and more elastic materials. Exploratory drilling in water depths up to 400 metres dates back to the 1960s. Field development in water depths more than 200 metres began in the 1980s, when deepwater petroleum exploration rapidly expanded. In the 1990s, hydrocarbon exploration and development extended into new areas at even greater water depths. L. Weeks, an American scientist presented the first estimate of offshore hydrocarbon resources in 1971 at the 8th Petroleum Congress in Moscow. He estimated the offshore recoverable hydrocarbon resources of the World’s Oceans as 320 Gtoe (1 toe = 100 m 3 gas), consisting of 230 Gt 1 oil and 90 Tm 3 2 gas. In the following 20 years, new recoverable hydrocarbon resource estimates were regularly published. They varied from 100–150 Gtoe 3 to 1.5-2 Ttoe, primarily due to poor geologic knowledge of the World’s Oceans, the use of different sets of data, and assumptions of different geologic or economic allowances and limits. In all cases, however, the petroleum potential of deepwater areas (deeper than 500 metres of water) was never discussed independently. The Research institute VNIIZarubezhgeologia (Moscow, Russia) has repeatedly estimated deepwater oil and gas resources of the World’s Oceans within the framework of the quantitative estimation of world petroleum potential. The latest estimate that it made was in 1996, and was based on the available geologic and economic data. 2. Sedimentary Basins As The Main Object Of Hydrocarbon Resource Estimation Sedimentary basins of various sizes, structure and geologic history are considered the main object of hydrocarbon resource exploration. These basins are morphologically expressed in the modern crustal 1 Gt. Gigatonnes equal to one billion metric tons (tonnes) = 1000 million tonnes. 2 Tm3 - Tera cubic metres = 1012 cubic metres 3 Gtoe – Gigatonnes of oil equivalent INTERNATIONAL SEABED AUTHORITY 485
- Page 442 and 443: Table 3: Geochemistry of known mass
- Page 444 and 445: Detailed exploration has not been c
- Page 446 and 447: flotation, can separate the ferroma
- Page 448 and 449: The crushed and ground ore can be c
- Page 450 and 451: 3.2. Assumptions made for each kind
- Page 452 and 453: alloys or even manganese ore in the
- Page 454 and 455: ought the nickel price to a top. Th
- Page 456 and 457: Because the metal market economy is
- Page 458 and 459: 14. J. -P. Lenoble (1992), Future d
- Page 460 and 461: 31. J. Francheteau, D. Needham, P.
- 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 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 512 and 513: The extremely harsh environment bro
- 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
CHAPTER 13<br />
PETROLEUM POTENTIAL AND DEVELOPMENT PROSPECTS IN<br />
DEEP-SEA AREAS OF THE WORLD<br />
V. I. Vysotsky, Petroleum Institute<br />
JSC VNIIZarbezhgeologia, Moscow, Russian Federation<br />
A. I. Gloumov, Russian Ministry of Natural Resources<br />
Moscow, Russian Federation<br />
In the oil industry, the term “deepwater” is applied to the deeper<br />
parts of the World’s Oceans with water depths of more than 500m. At<br />
these depths, the offshore extensions of marginal sedimentary basins and,<br />
less frequently, oceanic-type basins are located. About 120 of the known<br />
511 sedimentary basins of the world have volume-balance methods. The<br />
total recoverable oil and condensate reserves are 36 Gt; gas, 63 TM 3 . The<br />
bulk of resources occur in the basins along the Atlantic Ocean margins.<br />
Deepwater hydrocarbon exploration began in the 1980s. Exploration work<br />
was particularly active in the Campos basin (Brazil), Gulf of Mexico (US<br />
sector), and West Africa (Angola, Nigeria). By the end of the century,<br />
exploratory wells reached sea depths of 3000 m, and development wells,<br />
depths of 2000 m. By the beginning of 2000, a total of 190 oil and gas fields<br />
with aggregate reserves of about 3 Gtoe had been discovered in deepwater<br />
areas. In the next 5 years, deepwater oil expenditure will exceed $70<br />
billion forecasted spending.<br />
1. Introduction<br />
The term “deepwater” has become quite common at the present<br />
stage of offshore petroleum exploration and development, and it carries a<br />
geological, and technical and economic sense. Geologically, it refers to the<br />
deeper parts of the World’s Oceans with water depths greater than 500 m.<br />
Passive and active continental margins, trenches, island-arc slopes, the<br />
continental rise, and the deep-sea basins of the World’s Oceans are located<br />
at these depths. In some parts of the World’s Oceans, these zones exhibit<br />
considerable petroleum potential. From the technical and economic<br />
perspective, these areas are the offshore areas where fixed bottomsupported<br />
drilling or production platforms cannot be used. Hydrocarbon<br />
prospecting and development at these water depths require special<br />
technical means and economic estimates.<br />
INTERNATIONAL SEABED AUTHORITY 484