阿伊山脉东南部(喀尔巴阡山脉-巴尔干山脉,塞尔维亚东部)晚巴雷米亚-早阿普提亚-乌尔哥尼亚石灰石

M. Sudar, D. Jovanović, A. Maran, S. Polavder
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引用次数: 21

摘要

本文介绍了在塞尔维亚东部喀尔巴阡-巴尔卡尼德山脉(carpathoo - balkanides)东南坡Boljevac周围部分乌尔哥尼亚石灰石的沉积学和古生物学研究的最新结果。在靠近法卡瓦贾利村的两个地方,生物碎屑灰岩中分离出4种微相类型和1种亚相类型。对所调查的乌尔古尼亚灰岩的沉积环境特征进行了研究和讨论。在有孔虫和藻类丰富的微联系的基础上,精确地确定了有孔虫物种的垂直分布,从而确定了这部分乌尔古尼亚石灰石的时代为晚巴雷米亚-早阿普提亚。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Late Barremian-Early Aptian Urgonian Limestones from the south-eastern Kučaj Mountains (Carpatho-Balkanides, Eastern Serbia)
The newest results of sedimentological and paleontological investigations of part of the Urgonian Limestones studied in the surrounding of Boljevac on the SE slopes of the Ku~aj Mts. (Carpatho-Balkanides, eastern Serbia) are presented. On two localities, near the village Faca Vajali, four types of microfacies and one subtype within the bioclastic limestones were separated. The characteristics of the depositional environments of the investigated Urgonian Limestones were studied and are discussed. At the base of the established rich micro- associations of foraminifera and algae, the vertical distribution of foraminiferal species was precisely defined which enabled the determination the the age of this part of the Urgonian Limestones as Late Barremian-Early Aptian.
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