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 the Krndija Mt. (Pannonian Basin, Croatia)
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Significance of the Badenian petroleum source rocks from the Krndija Mt. (Pannonian Basin, Croatia)

机译:来自克尔尼贾山的巴登尼亚石油烃源岩的意义。 (克罗地亚Pannonian盆地)

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Discovery of petroleum source rocks at surface exposures of the Badenian deposits on northern slopes of the Krndija Mt. ?is the first record of petroleum source rocks on a surface outcrop in the Croatian part of the Pannonnian basin. Rocks with increased organic matter content have the characteristics of the prime source rocks. Positive hydrocarbon potential is the consequence of a favorable 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 reductive depositional environment in a mostly shallow sea, formed in protected lagoons during the Badenian period, which was reconstructed using palaeogeomorphological, paleontological, petrographical and organogeochemical analyses. This new petrological data deserve attention as it points out the need for additional geological-geophysical-geochemical research of the petroleum potential of the Badenian deposits in the broad area around Na?ice.
机译:在Krndija山北坡的Badenian矿床的表面暴露中发现石油源岩石。是Pannonnian盆地克罗地亚部分地表露头上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。这些岩石的成因与巴德尼时期在受保护的泻湖中形成的,大部分为浅海的还原性沉积环境有关,并通过古地貌,古生物学,岩石学和有机地球化学分析对其进行了重建。这项新的岩石学数据值得关注,因为它指出有必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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