Minerals Report - International Seabed Authority

Minerals Report - International Seabed Authority Minerals Report - International Seabed Authority

05.02.2013 Views

CHAPTER 20 STATUS REPORT ON THE DATA AND REPORTING REQUIREMENTS OF BRAZIL’S OFFSHORE MINING POLICY AS IT RELATES TO PROSPECTING AND EXPLORATION Roberto Alfradique Vieira de Macedo, Petroleum Engineer, MSc. and Lawyer President’s Office, Petrobrás, Brazil Walter Sá Leitão, Lawyer, Legal Department, Petrobr”as, Brazil This paper presents a brief summary on the occurrence of mineral resources offshore Brazil, the country’s experience with exploration and production of oil and natural gas – the only relevant mining activity on the seabed, and a panorama of the legal framework regulating the industry. Brazilian offshore mining activities, up to now, are restricted to the exploration for and production of oil and natural gas. Some other minerals have been prospected or even produced, but this activity has been limited and has not been of economic significance. Before discussing the oil and natural gas offshore industry, a brief description of the other offshore minerals will be presented. 1. Mineral Resources to be found offshore Brazil In several countries, such as Denmark, France and Canada, for instance, offshore sand and gravel supplies are added to onshore supplies to meet the demand for this resource. Japan is the main producer of offshore sand and gravel with 35 % of its needs coming from offshore sources. Offshore sand and gravel are the most important superficial sedimentary deposits, economically speaking, and the easiest ones to exploit among the mineral resources existing offshore Brazil. Since they are low-unitary-value minerals, transportation is a significant portion of its final cost; hence, economic exploitation is restricted to areas close to shore. Thus, sand and gravel do not have significance in this study. Additionally, there are no regulations governing its exploration and mining. Similar to sand and gravel, limestone is also a relatively low-unitaryvalue mineral whose transportation cost is significant, although not as INTERNATIONAL SEABED AUTHORITY 818

important as in the case of the former. Nowadays, national limestone demand is supplied by onshore production, but, in the medium term, exploitation of offshore resources is anticipated. Offshore Brazil is considered the longest and most continuous carbonaceous environment in the world, extending from the Pará River in the north of the country (5° S). It is relatively narrow, shallow, at warm (25 to 39°C), high salinity (30 % to 38 %) waters. Its width varies from 8 km, in front of Salvador, to 113 km, in the northeast of the country. For the purposes of the workshop, limestone does not have significance in this study. Phosphate, a sedimentary mineral whose main component is a variety of apatite called flourapatite carbonate, often occurs as nodules. Offshore phosphates supply, presently, 70 to 80 % of the world demand, and are the biggest known resources in the world. In general, the phosphate content of Brazilian offshore sediments is very low. Known deposits are considered economically insignificant, and the industrial utilisation of this resource is minimal, compounded by the water depths at which deposits occur and the lack of technology. The production of sub-sea phosphates is not foreseen for the next few decades, in Brazil. Sub-sea placers are exploited around the world. The main examples are cassiterite in Southeast Asia and diamonds in Namibia. In Brazil, some heavy metals occur along the coast from Pará, in the north of the country, up to Rio Grande do Sul, in the extreme south. Offshore mining activity is restricted to coastal deposits. Polymetallic nodules, or manganese nodules, generally occur at ultra deep waters, around 4,000 meters of water depth, in oceanic basins In Brazil, there is only one record of polymetallic nodules off the northeast coast, at a depth of 2,200 meters. Polymetallic sulphides were only found onshore two decades ago. In 1977, the first offshore discovery occurred next to the Galapagos Islands. Generally, the known deposits are found on meso-oceanic mountain ranges, at about 2,500 meters of water depth. In Brazil, the only place where polymetallic sulphides may occur is at the meso-oceanic mountain ridge close to the St. Peter and St. Paul rocks. INTERNATIONAL SEABED AUTHORITY 819

important as in the case of the former. Nowadays, national limestone demand<br />

is supplied by onshore production, but, in the medium term, exploitation of<br />

offshore resources is anticipated. Offshore Brazil is considered the longest and<br />

most continuous carbonaceous environment in the world, extending from the<br />

Pará River in the north of the country (5° S). It is relatively narrow, shallow, at<br />

warm (25 to 39°C), high salinity (30 % to 38 %) waters. Its width varies from 8<br />

km, in front of Salvador, to 113 km, in the northeast of the country. For the<br />

purposes of the workshop, limestone does not have significance in this study.<br />

Phosphate, a sedimentary mineral whose main component is a variety<br />

of apatite called flourapatite carbonate, often occurs as nodules. Offshore<br />

phosphates supply, presently, 70 to 80 % of the world demand, and are the<br />

biggest known resources in the world. In general, the phosphate content of<br />

Brazilian offshore sediments is very low. Known deposits are considered<br />

economically insignificant, and the industrial utilisation of this resource is<br />

minimal, compounded by the water depths at which deposits occur and the<br />

lack of technology. The production of sub-sea phosphates is not foreseen for<br />

the next few decades, in Brazil.<br />

Sub-sea placers are exploited around the world. The main examples<br />

are cassiterite in Southeast Asia and diamonds in Namibia. In Brazil, some<br />

heavy metals occur along the coast from Pará, in the north of the country, up<br />

to Rio Grande do Sul, in the extreme south. Offshore mining activity is<br />

restricted to coastal deposits.<br />

Polymetallic nodules, or manganese nodules, generally occur at ultra<br />

deep waters, around 4,000 meters of water depth, in oceanic basins In Brazil,<br />

there is only one record of polymetallic nodules off the northeast coast, at a<br />

depth of 2,200 meters.<br />

Polymetallic sulphides were only found onshore two decades ago. In<br />

1977, the first offshore discovery occurred next to the Galapagos Islands.<br />

Generally, the known deposits are found on meso-oceanic mountain ranges,<br />

at about 2,500 meters of water depth. In Brazil, the only place where<br />

polymetallic sulphides may occur is at the meso-oceanic mountain ridge close<br />

to the St. Peter and St. Paul rocks.<br />

INTERNATIONAL SEABED AUTHORITY 819

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