Depth geological relations of the wider area of Belgrade - based on the wells and geophysical data

D. Marinović, L. Rundić
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Abstract

The subject work covers the Belgrade wider area with a total area of about 2,000 km2. The authors integrated the principal geological and geophysical data provided by surface works and multidisciplinary elements from the fifty-two wells with depths between 33 and 2,733 m. Explicit paleontological findings of specialized analytists with determinations of macro- and microfauna and flora are presented both from Neogene formations and the older basinal floor. In addition to conventional petrological descriptions of rocks, microscopic determinations of intrusive and extrusive magmatites were also cited. From the enclosed basin space, the mineralization of deep aquifers is also correlative positioned. From the geophysical data for wells deeper than 400 m, records of well logging measurements were used, with markers based on which valid stratigraphic delimitations were made. Seismic survey sections were the basis for spatial shaping of Neogene sedimentation and basin floor configuration. For in-depth geological interpretations, published and repository gravimetric and geomagnetic maps of different sizes and years were consulted. The authors focused primarily on factometric indicators without entering into variable and debatable theoretical schematizations, especially orogenically complex of subbasin tectonics, in dissonant relations with the younger disjunctive shaped configuration which is visually shown in the reference cross-sections both vertically and laterally
贝尔格莱德大范围地区的深部地质关系——基于井和地球物理资料
这一主题工作涉及贝尔格莱德更广泛的地区,总面积约为2 000平方公里。作者综合了地面工作提供的主要地质和地球物理数据以及深度在33至2733米之间的52口井的多学科元素。明确的古生物学发现的专业分析与确定的大型和小型动物和植物区系,从新近纪地层和更古老的盆地底板。除了对岩石的常规岩石学描述外,还引用了侵入和喷出岩浆岩的显微测定。从封闭的盆地空间来看,深层含水层的成矿作用也进行了相关定位。根据深度超过400米的井的地球物理数据,使用测井测量记录,并在此基础上进行有效的地层划界。地震剖面是新近系沉积空间塑造和盆地底板构造的基础。为了进行深入的地质解释,参考了已出版的和存储的不同尺寸和年份的重力和地磁图。作者主要关注因子指标,而没有进入可变的和有争议的理论图式,特别是造山复杂的次盆地构造,在与年轻的分离形构型的不协调关系中,在垂直和横向的参考截面上都可以直观地显示出来
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