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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >The use of bisnorhopane as a stratigraphic marker in the Oseberg Back Basin, North Viking Graben, Norwegian North Sea
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The use of bisnorhopane as a stratigraphic marker in the Oseberg Back Basin, North Viking Graben, Norwegian North Sea

机译:在挪威北海北部维京格拉本的Oseberg后盆地中使用双降冰片作为地层标记

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This paper discusses the occurrence of 28,30-dinor-17alpha,18alpha,21beta-hopane (bisnorhopane) in stratigraphically, fairly well preserved Viking Group sections from wells in local depressions in the North Viking Graben Area. The results show the presence of high relative amounts of bisnorhopane in the "Syn-rift sections", whilst the "Post-rift sections" contain little or no bisnorhopane. Since most exploration wells are drilled on structural highs, primarily penetrating the "Post-rift Draupne", this may explain why many analyzed source rock sections in this area contain little bisnorhopane. As a correlation of Draupne sections using the vertical, relative bisnorhopane distributions, it is suggested to be a potential stratigraphic marker for the area, indicating the presence of "Syn-rift Draupne" sediments. The relative bisnorhopane amounts follow a logarithmic reduction with depth and thermal maturity. The bisnorhopane signal is nearly extinguished at 3700 m depth at a maturity of R-0 = 0.9-1.0%. (C) 2004 Elsevier Ltd. All rights reserved.
机译:本文讨论了在北维京格拉本地区局部凹陷的地层中,保存完好的维京族断面中28,30-dinor-17alpha,18alpha,21beta-hopane(bisnorhopane)的发生。结果表明,“ Syn-rift切片”中存在较高的相对含量的bisnorhopane,而“ rift分离后的切片”中几乎没有或没有bisnorhopane。由于大多数勘探井都是在结构性高点上钻出的,主要是穿透“后裂谷”,因此可以解释为什么在该地区许多被分析的烃源岩断层中几乎没有双降冰片。作为使用垂直相对双降冰片分布的Draupne剖面的相关性,建议将其作为该地区的潜在地层标记,表明存在“ Syn-rift Draupne”沉积物。相对双降冰片数量随深度和热成熟度对数减少。 Binorhopane信号在3700 m深度处几乎熄灭,成熟度为R-0 = 0.9-1.0%。 (C)2004 Elsevier Ltd.保留所有权利。

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