Diagenesis of red bed clastic reservoirs in the Central European Basin: how important is organic maturation and migration?

这里建议的研究集中在测试的假设，即主要的成岩特征的二叠纪Rotliegend砂岩储层的北德国盆地/中欧盆地的存在或不存在的烃类成熟产物直接控制。这应该通过比较这些储集层砂岩中的量化成岩现象来完成，这些储集层砂岩来自与烃源岩有和没有水力接触的地区。建议的调查，岩石地球化学和建模方法的基础上，旨在提高我们的有机成熟产物与红层长石砂岩的化学相互作用的知识，并提供成岩作用建模（耦合传输反应模拟）的输入数据。

The study suggested here is concentrated on testing the assumption, that major diagenetic features of the Permian Rotliegend sandstone reservoirs of the North German Basin / Central European Basin are directly controlled by the presence or absence of hydrocarbon maturation products. This should be accomplished by comparing quantified diagenetic phenomena in these reservoir sandstones from areas with and without hydraulic contact to hydrocarbon source rocks. The proposed investigation, based on petrographic-geochemical and modelling approaches, is intended to improve our knowledge of the chemical interaction of organic maturation products with red bed arkosic sandstones and to supply input data for diagenesis modelling (coupled transport reaction simulations).