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首页> 外文期刊>Geologia Croatica: a journal of the Institute of Geology Zagreb and Croatian Geological Society >Significance of the Badenian petroleum source rocks from Krndija Mt.(Pannonian Basin, Croatia)
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Significance of the Badenian petroleum source rocks from Krndija Mt.(Pannonian Basin, Croatia)

机译:克尔尼贾山(克罗地亚潘诺尼盆地)的巴登尼亚石油烃源岩的意义

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摘要

Discovery of petroleum source rocks at surface exposures of the Badenian deposits on the northern slopes of Krndija Mt. is the first record of petroleum source rocks at outcrop in the Croatian part of the Pannonnian basin. Rocks with increased organic matter content have the characteristics of prime source rocks. Positive hydrocarbon potential is the consequence of a favourable type of organic facies. Type II kerogen is of mostly marine algal origin, but with somewhat more pronounced terrigenic lipid content. Source rocks are in the immature, diagenetic period of thermal transformation. Genesis of these rocks is related to the reducing depositional environment in a mostly shallow sea, formed in protected lagoons during the Badenian period, which was reconstructed using palaeogeomorphological, palaeontological, petrographical and organogeochemical analyses. These new petrological data deserve attention as they highlight the need for additional geological-geophysical-geochemical research of the petroleum potential of the Badenian deposits in the broad area around Nasice.
机译:在Krndija山北坡的Badenian矿床的表面暴露中发现石油源岩。是Pannonnian盆地克罗地亚部分露头的石油烃源岩的第一个记录。有机质含量增加的岩石具有原始烃源岩的特征。正烃势是有机相有利类型的结果。 II型干酪根主要来自海洋藻类,但其陆生脂质含量却更为明显。烃源岩处于热转变的不成熟成岩时期。这些岩石的成因与减少的沉积环境有关,该沉积环境是在巴登尼亚时期在受保护的泻湖中形成的,大部分为浅海的环境,该沉积环境是通过古地貌,古生物学,岩石学和有机地球化学分析重建的。这些新的岩石学数据值得关注,因为它们突显了需要对纳西采周围广阔地区的巴登尼亚矿床的石油潜力进行额外的地质-地球物理-地球化学研究。

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