The Kolárovo gravity and magnetic anomaly body in a subcrop of the Danube Basin: A new geological interpretation

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
D. Plašienka, Miroslav Bielik
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Abstract

: We provide an analysis of the existing 2D and 3D gravimetric and magnetic interpretations of the well-known and significant Kolárovo gravity and magnetic anomaly, as well as present a new geological interpretation of its origin. It follows that the source of these anomalies is a high-density and highly magnetic crustal body with the following parameters: (a) density contrast is between +0.28 and +0.31 g cm −3 , (b) magnetic susceptibility is ~22000×10 −6 units of SI, (c) the depth of the upper boundary varies from ~4.5 to 6.0 km, (d) the depth of the center of the gravity body is between 8.7 and 12.5 km, and (e) the depth of the lower boundary moves in the interval from above 13 to 20 km. These factors and the inferred tectonic position of the Kolárovo body allow for its interpretation as a possible eclogite/ ultramafite body. It occurs within a belt of magnetic and gravity anomalies tracing the Eo-Alpine high-pressure metamorphic complexes from the Eastern Alps to the Western Carpathians via the northern periphery of the Rába–Hurbanovo– Diósjenő fault zone. We assume that the position of the Kolárovo crustal body resulted from the Oligocene–Lower Miocene uplift of the East Alpine–West Carpathian junction caused by the compressional tectonic regime accompanied by crustal thickening, surface uplift, and erosion of units forming the present basement of the Danube Basin. Simulta-neously, exhumation of the orogenic infrastructure occurred, which thus affected the Eo-Alpine metamorphic complexes, including the anomalous Kolárovo body. Subsequently, during the Middle–Late Miocene rifting and subsidence of the Danube Basin, the Kolárovo body was buried to its present position.
多瑙河盆地亚作物中的 Kolárovo 重力和磁异常体:新的地质解释
:我们对著名的科拉罗沃重力和磁力异常的现有二维和三维重力和磁力解释进行了分析,并对其来源提出了新的地质解释。因此,这些异常现象的来源是一个高密度、高磁性的地壳体,其参数如下:(a) 密度对比介于 +0.28 和 +0.31 g cm -3 之间,(b) 磁感应强度约为 22000×10 -6 单位 SI,(c) 上边界深度约为 4.5 至 6.0 千米,(d) 重力体中心深度在 8.7 至 12.5 千米之间,(e) 下边界深度在 13 千米以上至 20 千米之间移动。根据这些因素和推断出的 Kolárovo 岩体的构造位置,可以将其解释为一个可能的夕发岩/超基性岩体。Kolárovo位于从东阿尔卑斯山经Rába-Hurbanovo- Diósjenő断层带北部外围到西喀尔巴阡山的埃奥-阿尔卑斯高压变质复合体的磁力和重力异常带内。我们假定,Kolárovo 地壳体的位置是由于东阿尔卑斯山-西喀尔巴阡山交界处的渐新世-下新世隆起造成的,当时的压缩构造体系伴随着地壳增厚、地表隆起和侵蚀,形成了多瑙河盆地目前的基底。与此同时,造山基底发生了掘起,从而影响了埃奥-阿尔卑斯变质复合体,包括异常的 Kolárovo 岩体。随后,在中新世中晚期多瑙河盆地的断裂和下沉过程中,Kolárovo岩体被掩埋到现在的位置。
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来源期刊
Geologica Carpathica
Geologica Carpathica 地学-地球科学综合
CiteScore
2.40
自引率
23.10%
发文量
26
审稿时长
>12 weeks
期刊介绍: GEOLOGICA CARPATHICA covers a wide spectrum of geological disciplines including geodynamics, tectonics and structural geology, volcanology, stratigraphy, geochronology and isotopic geology, karstology, geochemistry, mineralogy, petrology, lithology and sedimentology, paleogeography, paleoecology, paleobiology and paleontology, paleomagnetism, magnetostratigraphy and other branches of applied geophysics, economic and environmental geology, experimental and theoretical geoscientific studies. Geologica Carpathica , with its 60 year old tradition, presents high-quality research papers devoted to all aspects not only of the Alpine-Carpathian-Balkanian geoscience but also with adjacent regions originated from the Mediterranean Tethys and its continental foreland. Geologica Carpathica is an Official Journal of the Carpathian-Balkan Geological Association.
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