An Integrated Approach for Characterizing Source Rocks in Frontier Hydrocarbon Basins by Organic Geochemical Analyses and Stratigraphic Forward Modeling: the Case of the Eastern Mediterranean Region
S. Grohmann, F. Nader, M. Romero-Sarmiento, F. Baudin, R. Littke
{"title":"An Integrated Approach for Characterizing Source Rocks in Frontier Hydrocarbon Basins by Organic Geochemical Analyses and Stratigraphic Forward Modeling: the Case of the Eastern Mediterranean Region","authors":"S. Grohmann, F. Nader, M. Romero-Sarmiento, F. Baudin, R. Littke","doi":"10.3997/2214-4609.201900901","DOIUrl":null,"url":null,"abstract":"Summary In order to better understand petroleum systems in the eastern Mediterranean Sea, an integrated approach is presented to characterize potential source rocks by means of organic geochemistry and stratigraphic forward modeling. Upper Cretaceous and Upper Eocene organic matter-rich deposits were found in the OPD Leg 160 boreholes along the Eratosthenes Seamount, south of Cyprus and within the Upper Miocene strata onshore Cyprus. The geochemical results indicate a mainly marine type of organic matter that was deposited as a result of upwelling systems above the seamount. Onshore, nutrients were derived together with clastic material, leading to increased bio-productivity. These results together with literature data for Cretaceous source rocks along the Levant Margin were the base for a large scale stratigraphic forward model, which was used to simulate the distribution of different sediments including organic matter within the respective intervals. The simulations could reproduce organic matter-rich deposits along the Levant margin as well as on top of the Eratosthenes Seamount. The simulated intervals are in accordance with published facies maps and show relatively small thickness errors compared to depth-converted seismic horizons. These models can provide valuable process-based facies input parameters for petroleum system modelling.","PeriodicalId":6840,"journal":{"name":"81st EAGE Conference and Exhibition 2019","volume":"1 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2019-06-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"81st EAGE Conference and Exhibition 2019","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3997/2214-4609.201900901","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
Summary In order to better understand petroleum systems in the eastern Mediterranean Sea, an integrated approach is presented to characterize potential source rocks by means of organic geochemistry and stratigraphic forward modeling. Upper Cretaceous and Upper Eocene organic matter-rich deposits were found in the OPD Leg 160 boreholes along the Eratosthenes Seamount, south of Cyprus and within the Upper Miocene strata onshore Cyprus. The geochemical results indicate a mainly marine type of organic matter that was deposited as a result of upwelling systems above the seamount. Onshore, nutrients were derived together with clastic material, leading to increased bio-productivity. These results together with literature data for Cretaceous source rocks along the Levant Margin were the base for a large scale stratigraphic forward model, which was used to simulate the distribution of different sediments including organic matter within the respective intervals. The simulations could reproduce organic matter-rich deposits along the Levant margin as well as on top of the Eratosthenes Seamount. The simulated intervals are in accordance with published facies maps and show relatively small thickness errors compared to depth-converted seismic horizons. These models can provide valuable process-based facies input parameters for petroleum system modelling.
为了更好地认识东地中海含油气系统,提出了一种综合的有机地球化学和地层正演模拟方法来表征潜在烃源岩。沿塞浦路斯南部Eratosthenes海山和塞浦路斯陆上上中新世地层,在OPD Leg 160钻孔中发现了上白垩统和上始新统富含有机质的矿床。地球化学结果表明,海山上方的上升流系统沉积了以海相为主的有机质。在陆地上,营养物质与碎屑物质一起产生,从而提高了生物生产力。这些结果结合黎凡特边缘白垩系烃源岩的文献资料,为建立大尺度地层正演模型奠定了基础,并用于模拟不同层段内不同沉积物(包括有机质)的分布。模拟可以重现黎凡特边缘和埃拉托色尼海底山顶部富含有机质的沉积物。模拟的层段与已发表的相图一致,与深度转换的地震层相比,厚度误差相对较小。这些模型可以为油气系统建模提供有价值的基于过程的相输入参数。