Subsidence, heat and mass transfer in the Central European Basin system: A regional 2D basin modelling study

中欧盆地系统的沉降、热量和质量传递：区域二维盆地模型研究

• 批准号: 5427469
• 负责人: Professor Dr. Ralf Littke
• 金额: --
• 依托单位: Department of Geo-Energy
• 依托单位国家: 德国
• 项目类别: Priority Programmes
• 财政年份: 2004
• 资助国家: 德国
• 起止时间: 2003-12-31 至 2009-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/5427469?language=en
• 关键词: Subsidence; heat; mass; transfer; Central

A detailed study is planned to obtain a comprehensive overview on subsidence and sedimentation, uplift and erosion, temperature and maturity evolution and hydrocarbon generation and transport along long regional transects through the Central European Basin system (CEBS). The southernmost line will extend from the West Netherlands Basin close to the London-Brabant High in the southwest towards the Lower Saxony Basin in the northeast crossing the major structural elements. The second line will be a transect from Brandenburg area in eastern Germany towards NE to Poland. It will cross important tectonic elements including the Variscan Front and the inverted Mid-Polish Trough superimposed on the Trans-European Suture Zone.The third line will be directed from the Lower Saxony Basin northwards towards the Norwegian-Danish Basin and will thus cross several important tectonic elements such as the Aller and Elbe Line, the Variscan and Caledonian deformation front and the Ringkøbing-Fyn High. It will allow a comparison of the northern and southern Permian Basin as part of the CEBS. The CEBS has a complex basin evolution reaching maximum burial and hence thermal maturation partly during Mesozoic (e.g. Jurassic, Cretaceous) times and partly during the Tertiary. Furthermore, it is characterized by a highly variable basin fill strongly affecting permeability distribution and heat transfer. This study should provide insight into the complex basin history. The approach will use newest versions of existing basin modelling software and take advantage of an international co-operation of several partner institutes.

计划进行一项详细的研究，以获取有关沉降和沉积，隆升和侵蚀，温度和成熟度进化以及通过中欧盆地系统（CEBS）沿着长区域沿长区域的运输的全面概述。最南端的线将从西南荷兰的西部盆地延伸到西南伦敦 - 布拉伯特高地，朝东北的下萨克森盆地延伸，穿越主要的结构元素。第二行将是从德国东部到东北到波兰的横横。 It will cross important tectonic elements including the Variscan Front and the inverted Mid-Polish Trough superimposed on the Trans-European Suture Zone.The third line will be directed from the Lower Saxony Basin northwards towards the Norwegian-Danish Basin and will thus cross several important tectonic elements such as the Aller and Elbe Line, the Variscan and Caledonian deformation front and the Ringkøbing-Fyn High.它将允许将北二叠纪盆地作为CEB的一部分进行比较。 CEB具有一个复杂的盆地演化，达到了最大埋葬，因此在中生代（例如侏罗纪，白垩纪）时代和部分期间部分在中生代期间的热成熟。此外，它的特征是高度可变的盆地填充强烈影响渗透率分布和传热。这项研究应洞悉复杂的盆地历史。该方法将使用现有的盆地建模软件的最新版本，并利用几家合作伙伴机构的国际合作。