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Source Rock Evaluation and Petroleum Processes in the Lower Palaeozoic Strata (Onshore of the Polish Baltic Basin)

机译:源岩评估和石油过程在较低古生代层(波兰波罗的海盆地的陆上)

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The study area comprising the western part of the Polish Baltic Basin is a most important exploration target in Poland in the unconventional resources aspect. Geochemical analyses of 840 rock samples were used in this study. They represented all Lower Palaeozoic stratigraphic horizons. The investigations showed that the samples in whole study area represent active source rocks. The best source-rock parameters are observed in the Upper Cambrian - Tremadocian complex. The all investigated Lower Palaeozoic strata contain oil-prone, low-sulphur Type-II kerogen deposited under anoxic or sub-oxic conditions. The maturity of Lower Palaeozoic strata change from the initial phase of “oil window” in the northeastern part of the area to overmature stage in the southwestern part of analysed area. Numerical modelling of generation and expulsion of hydrocarbons indicates the source rocks reached the complete generation interval from early to late stage. The early stage was reached from the beginning of Devonian to the beginning of the Carboniferous. The main and final generation stages were reached during the middle Devonian – early Tournaisian time. The organic matter reached the transformation degree from several percent to the complete transformation.
机译:该研究领域包含波兰波尔特盆地的西部是波兰在非传统资源方面中最重要的探索目标。本研究使用了840岩样品的地球化学分析。它们代表了所有较低的古生代层的地面视野。该研究表明,整个研究区域中的样品代表活性源岩。在上寒册 - Tremadocian Complex中观察到最佳源岩参数。全部调查的低古生代层含有缺氧或亚氧化局部沉积的油易发,低硫型II Kerogen。从东北部的“油窗”的初始阶段更加古代古生代地层的成熟度到了分析区域的西南部的过度成熟阶段。发电和排出碳氢化合物的数值模拟表明源岩从早期到晚期达到了完整的一代间隔。从德文人的开始到石炭系开始的早期阶段。在中部侦探期间达到了主要和最终一代阶段 - 早期窗陀尼斯时间。有机物质从几个百分点到完全转化达到转化度。

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