ZONES OF RECENT ACTIVATION AND SCHEME OF THE EARTH CRUST PERMEABILITY OF UKRAINE

V. Gordienko, L. Gordienko, J.A. Goncharova, V. Tarasov
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Abstract

An attempt is considered to supplement the criteria for identifying zones of recent activation in the territory of Ukraine with another one — data on the results of studies of helium concentration in ground-water. The previous analysis of information showed that as regional criteria, information can be applied on anomalies in heat flow, increased electrical conductivity of Earth’s crustal and the upper mantle rocks, distribution of mantle gravitational anomalies, and surface uplifts over the past millions of years. They were chosen among others precisely because of the dissemination of relevant information throughout the country. This requirement is also met by the permeability Scheme of the earth’s crust of Ukraine, which is a fragment of the permeability Scheme of the earth’s crust of the European part of the USSR based on the results of helium studies. The principal applicability of such information for solving the problem is shown. Areas of maximum helium concentrations in near-surface waters are indicated, primarily those associated with disjunctive dislocation. Theу are concentrated in the south-west of Ukraine and in Moldova. The disadvantages of the Scheme are noted, due to poor study and significant variations in background gas concentrations, directly caused not by recent activation, but by the peculiarities of helium generation by rocks of the upper part of the earth’s crust. There are inconsistencies between the previously obtained ideas about the activated zones and the data of the Scheme. They are especially large in the Carpathian, Crimean and Donetsk regions, and are noticeable in others. Therefore, it seems necessary, first, to continue research, thicken the network of observations and develop a methodology for analyzing their results.
乌克兰近代活化带与地壳渗透性方案
考虑尝试用另一项标准来补充确定乌克兰境内最近活动区的标准,即关于地下水中氦浓度的研究结果的数据。前人对信息的分析表明,信息可以作为区域标准应用于数百万年来的热流异常、地壳和上地幔岩石电导率增加、地幔重力异常分布、地表隆起等。之所以选择这些机构,正是因为在全国范围内传播了有关的信息。乌克兰地壳渗透性方案也符合这一要求,该方案是苏联欧洲部分基于氦研究结果的地壳渗透性方案的一个片段。说明了这些信息对解决问题的主要适用性。指出了近地表水中最大氦浓度的区域,主要是那些与分离位错有关的区域。他们集中在乌克兰西南部和摩尔多瓦。该方案的缺点是由于研究不足和背景气体浓度的显著变化,这不是由最近的活化直接引起的,而是由地壳上部岩石产生氦气的特性引起的。先前获得的关于活化区域的想法与计划的数据不一致。它们在喀尔巴阡山脉、克里米亚和顿涅茨克地区特别大,在其他地区也很明显。因此,似乎有必要,首先,继续研究,扩大观察网络,并发展一种分析其结果的方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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