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Unconventional reservoir potential of the upper Permian Zechstein Group: a slope to basin sequence stratigraphic and sedimentological evaluation of carbonates and organic-rich mudrocks, Northern Germany

机译:上二叠纪Zechstein组的非常规储层潜力:德国北部碳酸盐岩和富含有机质泥岩的斜坡至盆地层序地层学和沉积学评估

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摘要

The Late Permian Zechstein Group in northeastern Germany is characterized by shelf and slope carbonates that rimmed a basin extending from eastern England through the Netherlands and Germany to Poland. Conventional reservoirs are found in grainstones rimming islands created by pre-existing paleohighs and platform-rimming shoals that compose steep margins in the north and ramp deposits in the southern part. The slope and basin deposits are characterized by debris flows and organic-rich mudstones. Lagoonal and basinal evaporites formed the seal for these carbonate and underlying sandstone reservoirs. The objective of this investigation is to evaluate potential unconventional reservoirs in organic-rich, finegrained and/or tight mudrocks in slope and basin as well as platform carbonates occurring in this stratigraphic interval. Therefore, a comprehensive study was conducted that included sedimentology, sequence stratigraphy, petrography, and geochemistry. Sequence stratigraphic correlations from shelf to basin are crucial in establishing a framework that allows correlation of potential productive facies in fine-grained, organic-rich basinal siliceous and calcareous mudstones or interfingering tight carbonates and siltstones, ranging from the lagoon, to slope to basin, which might be candidates for forming an unconventional reservoir. Most organic-rich shales worldwide are associated with eustatic transgressions. The basal Zechstein cycles, Zl and Z2, contain organic-rich siliceous and calcareous mudstones and carbonates that form major transgressive deposits in the basin. Maturities range from over-mature (gas) in the basin to oil-generation on the slope with variable TOC contents. This sequence stratigraphic and sedimentologic evaluation of the transgressive facies in the Zl and Z2 assesses the potential for shale-gas/oil and hybrid unconventional plays. Potential unconventional reservoirs might be explored in laminated organic-rich mudstones within the oil window along the northern and southern slopes of the basin. Although the Zechstein Zl and Z2 cycles might have limited shale-gas potential because of low thickness and deep burial depth to be economic at this point, unconventional reservoir opportunities that include hybrid and shale-oil potential are possible in the study area.
机译:德国东北部的晚二叠纪Zechstein组的特征是陆架碳酸盐岩和斜坡碳酸盐岩,这些碳酸盐岩圈定了从英格兰东部到荷兰和德国再到波兰的盆地。在由早先存在的古隆起和平台边缘浅滩形成的粒状岛边缘岛中发现了常规的储层,这些北部北部构成陡峭的边缘,而南部则形成斜坡沉积。斜坡和盆地沉积物的特征是泥石流和富含有机物的泥岩。泻湖和盆地蒸发物形成了这些碳酸盐岩和下层砂岩储层的密封。这项研究的目的是评估斜坡和盆地中富含有机物,细粒和/或致密泥岩中潜在的非常规油藏,以及在该地层间隔中发生的台地碳酸盐岩。因此,进行了包括沉积学,层序地层学,岩石学和地球化学在内的综合研究。从架子到盆地的层序地层相关性对于建立一个框架是至关重要的,该框架可以使细粒的,富含有机物的盆地硅质和钙质泥岩或指状碳酸盐和粉砂岩(从泻湖到斜坡到盆地)之间潜在的生产相相关,这可能是形成非常规水库的候选人。世界上大多数富含有机物的页岩都与海侵有关。基础的Zechstein循环Z1和Z2包含富含有机质的硅质和钙质泥岩和碳酸盐,这些碳酸盐形成了盆地中的主要海侵沉积物。从盆地中的过成熟(天然气)到具有不同TOC含量的斜坡上的生油,其成熟度不等。 Z1和Z2海侵相的层序地层学和沉积学评估评估了页岩气/油和非常规混合油藏的潜力。潜在的非常规油藏可能在盆地北坡和南坡的油窗内的层状富含有机质的泥岩中进行勘探。尽管Zechstein Z1和Z2循环可能由于页岩气厚度低和埋藏深度大而限制了页岩气潜力,但在该地区,包括混合和页岩油潜力在内的非常规油藏机会还是有可能的。

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