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首页> 外文期刊>Acta Geologica Slovaca >Structural, biostratigraphic and petrographic evaluation of the Upper Cretaceous red marlstones and underlying granitoids from the borehole HPJ-1 Ja?ter near Hlohovec (Pova?sky Inovec Mts., Slovakia)
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Structural, biostratigraphic and petrographic evaluation of the Upper Cretaceous red marlstones and underlying granitoids from the borehole HPJ-1 Ja?ter near Hlohovec (Pova?sky Inovec Mts., Slovakia)

机译:从Hlohovec附近的井筒HPJ-1 Jater(斯洛伐克Povasky Sky Inovec Mts。)的上白垩统红色玛石岩和下伏的花岗岩类的结构,生物地层学和岩石学评价

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The article provides the first results of analyses of the core material from the borehole HPJ-1 Ja?ter, located north of Hlohovec in the southern Pova?sky Inovec Mts. (Western Carpathians, Slovakia). The main aim of the borehole was to determine the thickness and characteristics of sedimentary sequence of the Upper Cretaceous Horné Belice Group in a poorly exposed area and to reach its possible substratum. In the initial interval 0–45.8 m, the borehole penetrated deformed sequence of red and pink pelagic marly limestones and marlstones containing planktonic foraminifera. The drilled sediments are of the Late Cenomanian (45.5–41.5 m) and Middle Turonian – Santonian (41.5–34 m) age in the lower part of the sedimentary sequence. Stronger alteration and tectonic overprint of the uppermost interval (34–0 m) prevented a successful biostratigraphic age determination. The lower part of the borehole profile between 45.8–75.5 m is formed by pre-Alpine biotite granodiorites, which are separated from the overlying sedimentary sequence by a normal fault. Several possible interpretations of the tectonic position of the Upper Cretaceous complexes are discussed.
机译:本文提供了对位于南波瓦斯基伊诺韦茨山麓Hlohovec以北的HPJ-1钻孔的岩心材料进行分析的初步结果。 (斯洛伐克西部喀尔巴阡山脉)。钻孔的主要目的是确定暴露程度较差地区的上白垩统霍内贝利采组沉积层的厚度和沉积特征,并达到其可能的基底。在最初的0-45.8 m间隔内,钻孔穿透了红色和粉红色的浮游性灰质灰岩和含有浮游有孔虫的灰岩的变形序列。在沉积层序的下部,已钻出的沉积物为晚切诺曼期(45.5-41.5 m)和中土伦-桑托尼(41.5-34 m)年龄。最上层岩层(34-0 m)的强烈蚀变和构造叠印阻碍了生物地层年龄的成功确定。钻孔剖面的下部在45.8–75.5 m之间是由高山前黑云母花岗闪长岩形成的,它们通过正常断层与上覆的沉积层序分开。讨论了上白垩统复合体构造位置的几种可能解释。

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