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・ Marlies Oostdam
・ Marlies Rostock
・ Marlies Schild
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・ Marlies ter Borg
・ Marlies van Baalen
・ Marlies Veldhuijzen van Zanten
・ Marlies Wagner
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Marlim
・ Marlin
・ Marlin & Associates
・ Marlin (car)
・ Marlin (dinghy)
・ Marlin (disambiguation)
・ Marlin (DRM)
・ Marlin (magazine)
・ Marlin Airport
・ Marlin Barnes
・ Marlin Bay
・ Marlin Briscoe
・ Marlin cabinet
・ Marlin Camp Carbine
・ Marlin Cannon


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Marlim : ウィキペディア英語版
Marlim
Marlim is the name of a giant Brazilian oil field located in the north-eastern part of the Campos Basin, about 110 km offshore Rio de Janeiro, in water depths ranging from 650 to 1,050 m. Marlim means marlin, in Portuguese.
Marlim was originally discovered by well in February 1985. The 75 m column was predominantly unconsolidated sandstone, with a permeability as high as two darcies. The discovery also showed high-gravity oil (17-21 degree API). At the time of discovery, the Marlim reservoir had an oil-in-place volume of about 9 billion barrels and an expectated 1.7 billion barrels of oil in total reserves.〔http://www.offshore-technology.com/projects/marlimpetro/〕
==Geology==
The Marlim field consists of a single Oligocene producing horizon of sandstone turbidites, with an area of 152 km2.〔Candido, A., and Cora, C.A.G., 1992, The Marlim and Albacora Giant Fields, Campos Basin, Offshore Brazil, AAPG Memoir 54, Halbouty, M.T., editor, Tulsa: American Association of Petroleum Geologists, ISBN 0891813330〕 Reflection seismology in 1972 disclosed a faulted anticline and seismic amplitude bright spot, which was drilled by wildcat 1-RJS-219A in 1985 and discovered oil.〔 The stratigraphy of the Campos Basin starts with the Lower Cretaceous Lago Feia Formation a source rock, followed by the Albian Macae Formation consisting of shallow water carbonates overlain by late Albian shales, marls, calcilutites, and turbidite sandstones.〔 From this formation through most of the Cenozoic, the Campos Formation was deposited, consisting of deep water turbiditic sandstones and shales, the main producers in the Albacora and Marlim fields.〔 Finally, the basin was filled by the Ubatuba Formation, consisting of slope and shelf deposits.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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