R. Ondrak, R. Lippmann, V. Neumann, R. Gaup, R. Primio, B. Horsfield
{"title":"Modeling Burial History and Fluid-Rock-Interactions of Deep Overpressured Reservoirs in the Central Graben, North Sea","authors":"R. Ondrak, R. Lippmann, V. Neumann, R. Gaup, R. Primio, B. Horsfield","doi":"10.3997/2214-4609-pdb.3.p043","DOIUrl":null,"url":null,"abstract":"P043 MODELING BURIAL HISTORY AND FLUID- ROCK-INTERACTIONS OF DEEP OVERPRESSURED RESERVOIRS IN THE CENTRAL GRABEN NORTH SEA Abstract 1 We study temperature and pressure-controlled inorganic and organic diagenetic processes in a study area of the Central Graben North Sea containing clastic Mesozoic reservoirs situated at depths of 4.5-5 km and temperatures of 170-192°C. The reservoirs are highly overpressured due to rapid burial during the last 2 Ma. We present first results of a basin modeling study focusing on the burial and temperature history of these HPHT-reservoirs. Furthermore we concentrate on organic-inorganic interactions enhancing mineral solubility and increasing porosity. This is","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"39 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"66th EAGE Conference & Exhibition","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3997/2214-4609-pdb.3.p043","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
P043 MODELING BURIAL HISTORY AND FLUID- ROCK-INTERACTIONS OF DEEP OVERPRESSURED RESERVOIRS IN THE CENTRAL GRABEN NORTH SEA Abstract 1 We study temperature and pressure-controlled inorganic and organic diagenetic processes in a study area of the Central Graben North Sea containing clastic Mesozoic reservoirs situated at depths of 4.5-5 km and temperatures of 170-192°C. The reservoirs are highly overpressured due to rapid burial during the last 2 Ma. We present first results of a basin modeling study focusing on the burial and temperature history of these HPHT-reservoirs. Furthermore we concentrate on organic-inorganic interactions enhancing mineral solubility and increasing porosity. This is