Local magnetic anomalies of the Ukrainian Shield as indicators of the manifestation of different-age stages of focal-channel magmatism

IF 0.6 Q4 GEOCHEMISTRY & GEOPHYSICS Geofizicheskiy Zhurnal-Geophysical Journal Pub Date : 2023-05-14 DOI:10.24028/gj.v45i2.278322
V. A. Yentin, O. Gintov, M. Orlyuk, A. Marchenko
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Abstract

A special class of local small sizes of subisometric magnetic field anomalies (AMF) of the Ukrainian Shield (USh) is considered here. Such AMF are united by the volcanogenic-intrusive-tubular origin of the sources associated with the assumed source-channel manifestations of pulsed plutonic-degassing processes of the Earth. The geological study of such anomalies indicates the enrichment of their sources with mineralization of dark, noble, non-ferrous and rare metals. Some of these AMF (Zhdanivska group, Rivnenska) in general contours coincide with local gravitational minima due to decompaction and grinding of the rocks that cause them, despite the basic-ultrabasic composition. Other anomalies, on the contrary, fully correspond to the maxima of gravity due to the enrichment of rocks with magnetite (Pischansk AMF) or ilmenite (Stremigorodsk AMF) on an industrial scale. In the section, all the studied sources of anomalies have a funnel-shaped (sometimes fungal-shaped) or stock-like shape, which indicates the focal-channel type of their genesis. A characteristic feature of some of the studied AMF are peculiarities of the magnetization vector of their sources, which has variable directions in the section and is often subhorizontal (Kalyniv group of anomalies, Rivne and Stremigorod AMF), which is unusual for the USh latitudes. This indicates a multiphase and separation in time formation of the sources of these anomalies from the Archean-Proterozoic time of formation of the surrounding USh rocks. This time may be either Proterozoic (Stremigorod AMF), or Phanerozoic (Rivnenska AMP — early Paleozoic). A number of similar in size and concentrically-zonal shape of Cenozoic AMF has been established, for example, within the TransCarpathian fault zone. The obtained results show that within the Ukrshield there is a certain number of small-sized structures associated with different-age focal-channel manifestations of pulsed intrusive and plutonic-degassing processes of the Earth, which are much more widespread than it has been supposed. This does not only extend the prospecting possibilities for new types of minerals associated with the processes of magmatism and degassing of the Earth, but also contains a new additional information in the context of the universal history of the Ukrshield formation and its ore potential
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乌克兰地盾局部磁异常作为震源通道岩浆活动不同年龄阶段表现的标志
本文考虑了乌克兰地盾(USh)局部小尺度亚等距磁场异常(AMF)的一类特殊现象。这些AMF是由火山-侵入-管状来源与假定的地球脉冲岩体-脱气过程的源-通道表现相联系而统一起来的。这些异常的地质研究表明,这些异常的来源富集,成矿作用主要是暗金属、贵金属、有色金属和稀有金属。这些AMF (Zhdanivska群,Rivnenska)中的一些在一般轮廓上与局部引力极小值一致,这是由于导致它们的岩石的分解和研磨,尽管它们是碱性-超碱性组成。相反,其他异常完全符合重力最大值,这是由于在工业规模上富含磁铁矿(Pischansk AMF)或钛铁矿(strremigorodsk AMF)。在剖面上,所研究的异常源均呈漏斗状(有时呈真菌状)或块状,表明其成因为焦点水道型。所研究的一些AMF的一个特征是其来源的磁化矢量的独特性,其在剖面中具有可变方向,并且通常是亚水平的(Kalyniv组异常,Rivne和strremigorod AMF),这在USh纬度是不寻常的。这表明这些异常源与周围USh岩石的太古宙-元古代形成时期存在多阶段和时间上的分离。这段时间可能是元古代(strremigorod AMF)或显生宙(Rivnenska AMP -早古生代)。例如,在喀尔巴阡断裂带内,已经建立了许多大小和同心带形状相似的新生代AMF。结果表明,在乌克兰盾内存在一定数量的小型构造,这些构造与地球脉冲侵入和深部脱气过程的不同年龄的焦点通道表现有关,其分布范围远比想象的要广泛。这不仅扩大了与岩浆作用和地球脱气过程有关的新型矿物的勘探可能性,而且还在乌克兰盾地层的普遍历史及其矿石潜力的背景下包含了新的附加信息
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来源期刊
Geofizicheskiy Zhurnal-Geophysical Journal
Geofizicheskiy Zhurnal-Geophysical Journal GEOCHEMISTRY & GEOPHYSICS-
自引率
60.00%
发文量
50
期刊最新文献
Electrical conductivity anomalies study New palaeomagnetic data for Palaeoproterozoic AMCG complexes of the Ukrainian Shield Depth structure of the Transcarpathian Depression (Ukrainian part) according to density modeling data Development of the methodology of energy and environmental safety of Ukraine based on own geothermics The effect of the mantle and core matter phase state on the course of geodynamic processes
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