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GEODYNAMICS 地球动力学
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2019-12-01 DOI: 10.23939/jgd2019.02.005
A. Marchenko, S. Perii, O. Lompas, Y. I. Golubinka, D. A. Marchenko, S. Kramarenko, Abdulwasiu Salawu
This study aims to derive the Earth’s temporally varying Earth’s tensor of inertia based on the dynamical ellipticity , the coefficients , from UT/CSR data. They allow to find the time-varying Earth’s mechanical and geometrical parameters during the following periods: (a) from 1976 to 2020 based on monthly and weekly solutions of the coefficient ; (b) from 1992 to 2020 based on monthly and weekly solutions of the non zero coefficients , related to the principal axes of inertia, allowing to build models their long-term variations. Differences between and , given in various systems, represent the average value , which is smaller than time variations of or , characterizing a high quality of UT/CSR solutions. Two models for the time-dependent dynamical ellipticity were constructed using long-term variations for the zonal coefficient during the past 44 and 27.5 years. The approximate formulas for the time-dependent dynamical ellipticity were provided by the additional estimation of each parameter of the Taylor series, fixing at epoch =J2000 according to the IAU2000/2006 precession-nutation theory. The potential of the time-dependent gravitational quadrupole according to Maxwell theory was used to derive the new exact formulas for the orientation of the principal axes , , via location of the two quadrupole axes. Hence, the Earth’s time-dependent mechanical and geometrical parameters, including the gravitational quadrupole, the principal axes and the principal moments of inertia were computed at each moment during the past 27.5 years from 1992 to 2020. However, their linear change in all the considered parameters is rather unclear because of their various behavior on different time-intervals including variations of a sign of the considered effects due to a jump in the time-series during the time-period 1998 – 2002. The Earth’s 3D and 1D density models were constructed based on the restricted solution of the 3D Cartesian moments inside the ellipsoid of the revolution. They were derived with conditions to conserve the time-dependent gravitational potential from zero to second degree, the dynamical ellipticity, the polar flattening, basic radial jumps of density as sampled for the PREM model, and the long-term variations in space-time mass density distribution. It is important to note that in solving the inverse problem, the time dependence in the Earth's inertia tensor arises due to changes in the Earth's density, but does not depend on changes in its shape, which is confirmed by the corresponding equations where flattening is canceled.
本研究旨在根据UT/CSR数据中的动态椭圆率系数,推导出地球随时间变化的地球惯性张量。它们可以找到以下时期随时间变化的地球力学和几何参数:(a)1976年至2020年,基于系数的月度和每周解;(b) 从1992年到2020年,基于与惯性主轴相关的非零系数的月度和每周解,可以建立其长期变化的模型。不同系统中给出的和之间的差异表示平均值,该平均值小于或的时间变化,表征了UT/CSR解决方案的高质量。利用过去44年和27.5年中纬向系数的长期变化,建立了两个随时间变化的动态椭圆率模型。根据IAU2000/2006岁差章动理论,通过对泰勒级数的每个参数的附加估计,在历元=J2000时,给出了含时动力椭圆率的近似公式。根据麦克斯韦理论,利用含时引力四极的势,通过两个四极轴的位置,导出了主轴取向的新的精确公式。因此,在1992年至2020年的过去27.5年中,地球的时间相关机械和几何参数,包括引力四极、主轴和主惯性矩,都是在每一时刻计算出来的。然而,它们在所有考虑的参数中的线性变化相当不清楚,因为它们在不同时间间隔上的各种行为,包括由于1998-2002年期间时间序列的跳跃而引起的考虑效应的符号变化。地球的三维和一维密度模型是基于旋转椭球内三维笛卡尔矩的有限解构建的。它们是在保持从零到二度的时间相关引力势、动力学椭圆率、极性平坦化、PREM模型采样的密度的基本径向跳跃以及时空质量密度分布的长期变化的条件下导出的。需要注意的是,在求解逆问题时,地球惯性张量的时间依赖性是由于地球密度的变化而产生的,但并不取决于其形状的变化,这一点通过消除平坦化的相应方程得到了证实。
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引用次数: 3
GEODYNAMICS 地球动力学
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2019-12-01 DOI: 10.23939/jgd2019.02.039
L. V. Heneralova, V. Stepanov, N. Bilyk, Ye. Slyvko
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引用次数: 1
GEODYNAMICS 地球动力学
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2019-12-01 DOI: 10.23939/jgd2019.02.048
P. Anakhov
The purpose of the research is to find possible ways to use microseisms, caused by standing waves in water bodies. According to the theory, standing waves arise when two traveling waves, moving towards each other collide. The first of them falls on an obstacle and the second one reflects from it. The conditions of excitation the waves and swinging of damped waves are presented. Evidence shows that the wave pressure at the antinodes at the boundaries of the water medium separation and the soil is proportional to the wave amplitude on the water. The possibility of using standing waves in seismic exploration is confirmed by the observation data of storm microseisms at remote stations. To increase the transmission range, it is advisable to use long-period microseisms, which provide low damping. One method to reduce the risk of an earthquake involves the initiation of weak seismicity by artificial sources in order to periodically relieve excess tectonic stress. One of the most powerful sources of lithospheric deformations is the natural oscillations of the liquid level in large water bodies. The study considers the idea of using the resonance effect of tidal-seiches vibrations to initiate weak seismicity. Artificial excitation of the seiche is achieved when controlling a water culvert. Transmission network supports multiplexing of communication channels with separation by physical nature and transmission media. When managing culverts, seiches oscillations are artificially swung with phase-shift oscillations. Phase shift of the exciting wave relative to the damping wave, in turn, causes variations in seiche periods, which leads to proportional variations in the periods of microseisms. This solution allows encoding messages by the durations of seiches and microseisms, with their subsequent transmission. Hydrological observations revealed the effect of the dependence of surface seiches periods on water depth. The solution of the inverse problem, with the measured seiches period, allows calculating the water body depth. Method of remote measurement has been proposed using the analysis of ground oscillations of seiches origin. Analysis of variations in the electromagnetic radiation of the geological environment has shown that they are determined by the mechanisms of energy conversion of these processes into the energy of the electromagnetic field. The study of these variations allows us to calculate the depth of the water body. Originality. Methods for using microseismic oscillations excited by standing waves are considered in detail. The methods of managing standing waves are presented: by regulating the depth of the reservoir; by regulating the period of the exciting wave; by regulating the phase of the exciting wave. The dependence of the amplitude of the resulting oscillation of standing waves on the phase of the exciting oscillation of the same period was investigated. Innovative developments protected by patents of Ukraine are presented, which imply
这项研究的目的是寻找利用微地震的可能方法,微地震是由水体中的驻波引起的。根据该理论,当两个相互移动的行波碰撞时,就会产生驻波。第一个人落在障碍物上,第二个人从障碍物上反射过来。给出了阻尼波的激励、振荡和振荡条件。有证据表明,在水介质分离和土壤边界的波峰处的波压与水面上的波幅成正比。远站风暴微震观测资料证实了驻波在地震勘探中的可行性。为了增加传输范围,建议使用提供低阻尼的长周期微震。减少地震风险的一种方法是通过人工震源引发弱地震活动,以便周期性地减轻过量的构造应力。岩石圈变形的最有力的来源之一是大水体中液位的自然振荡。该研究考虑了利用潮汐震动的共振效应来引发弱地震活动性的想法。在控制涵洞时,可实现人工激发积水。传输网络支持通信信道的多路复用,通过物理性质和传输介质进行分离。当管理涵洞时,seiches振荡被人为地用相移振荡摆动。激发波相对于阻尼波的相移又引起地震周期的变化,从而导致微震周期的成比例变化。该解决方案允许根据地震和微地震的持续时间对消息进行编码,并进行后续传输。水文观测揭示了地表沉降期对水深的依赖性。反问题的解,与测量的洪水周期,允许计算水体深度。通过对地震震源地震动的分析,提出了遥测地震震源的方法。对地质环境电磁辐射变化的分析表明,它们是由这些过程转化为电磁场能量的机制决定的。对这些变化的研究使我们能够计算出水体的深度。创意。详细讨论了利用驻波激发的微震振荡的方法。提出了控制驻波的方法:通过调节水库深度;通过调节激励波的周期;通过调节激发波的相位。研究了驻波振荡的振幅与同周期激振的相位的关系。介绍了受乌克兰专利保护的创新发展,这意味着由水体驻波引起的微震的经济利用。需要指出的是,使用一种或另一种方法执行特定任务的必要性和可能性,是由在一定时间、一定空间存在的内外客观条件决定的。
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引用次数: 2
GEODYNAMICS
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2019-07-01 DOI: 10.23939/jgd2019.01.017
M. Fys, A. Brydun, M. Yurkiv, А. R. Sohor
Purpose. To create an algorithm for constructing a three-dimensional masses distribution function of the planet and its derivatives taking into account the Stokes constants of arbitrary orders. Being based on this method, the task is to perform the research on the internal structure of the Earth. Methodology. The derivatives of the inhomogeneous mass distribution are presented by linear combinations of biorthogonal polynomials which coefficients are obtained from the system of equations. These equations follow from integral transformations of the Stokes constants, the calculation process is carried out by a sequential approximation and for the initial approximation we take a one-dimensional density model that is consistent with Stokes constants up to the second inclusive order. Next, the coefficients of expansion of the potential of higher orders are determined up to a predetermined order. In this case, the information on the power moments of the density of surface integrals makes it possible to analyze and control the iterative process. Results. The results of calculations using the software according to the described algorithm are obtained. A fairly high degree of approximation (sixth order) of three-dimensional mass distributions function is achieved. Carto diagrams were created being based on the values of deviations of the three-dimensional average distributions (“isodens”), which give a fairly detailed picture of the Earth’s internal structure. The presented maps of “inhomogeneity’s” at characteristic depths (2891 km core – mantle, 5150 km internal – external core) allow us to draw preliminary conclusions about global mass movements. At the same time, the information on derivatives is significant for interpretation. First of all, it should be noted that the gradient of “inhomogeneity’s” is directed toward the center of mass. The presented projections of this gradient on a plane perpendicular to the rotation axis (horizontal plane) show the tendency of spatial displacements. Scientific novelty. Vector diagrams of the gradient, in combination with carto diagrams, give a broad picture of the dynamics and possible mechanisms of mass movement within the planet. To a certain extent, these studies confirm the phenomenon of gravitational convection of masses. Practical significance. The proposed algorithm can be used in order to build regional models of the planet, and numerical results can be used to interpret global and local geodynamic processes inside and on the Earth’s surface.
目的。在考虑任意阶斯托克斯常数的情况下,建立行星及其导数的三维质量分布函数的算法。基于这种方法,任务是对地球内部结构进行研究。方法。用双正交多项式的线性组合来表示非均匀质量分布的导数,其系数由方程组获得。这些方程是由Stokes常数的积分变换得出的,计算过程是通过顺序近似进行的,对于初始近似,我们采用一维密度模型,该模型与Stokes常数一致,直到第二次包含阶。然后,确定高阶势的展开系数,直至预定阶。在这种情况下,曲面积分密度的幂矩信息使得分析和控制迭代过程成为可能。结果。根据所描述的算法,利用该软件进行了计算。实现了三维质量分布函数的相当高的近似度(六阶)。卡托图是根据三维平均分布的偏差值(“等差”)创建的,它提供了地球内部结构的相当详细的图像。所呈现的特征深度(2891公里的地核-地幔,5150公里的内-外地核)的“非均匀性”图使我们能够得出关于全球物质运动的初步结论。同时,衍生品信息对解释具有重要意义。首先,需要注意的是,“非均匀性”的梯度是指向质心的。该梯度在垂直于旋转轴(水平面)的平面上的投影显示了空间位移的趋势。科学的新奇。梯度的矢量图与图相结合,给出了行星内部质量运动的动力学和可能机制的广泛图景。这些研究在一定程度上证实了质量的引力对流现象。现实意义。该算法可用于建立地球区域模型,数值结果可用于解释地球内部和表面的全球和局部地球动力学过程。
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引用次数: 0
GEODYNAMICS 地球动力学
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2019-07-01 DOI: 10.23939/jgd2019.01.028
A. Tserlevych, Y. Shylo, O. Shylo
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引用次数: 1
GEODYNAMICS 地球动力学
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2019-07-01 DOI: 10.23939/jgd2019.01.090
І. Naumko, N. Batsevych, Yu.I. Fedoryshyn, M. Pavlyuk, Yu.S. Myshchyshyn, I. V. Repyn
Purpose. The main purpose of this paper is to investigate the peculiarities of the spatial distribution of thickness and paleorelief of continental flood basalts of Luchychi stratum of Ratne suite of the Ediacaran of the Ratne–Kamin-Kashyrskyi Area in Western Volyn using maps of the thickness and relief of the paleosurface. The study also focuses on correlation between the specified parameters of the stratum and the spatial change of concentrations of native mineralization and its localization relative to the roof (sole) of the stratum. Method. The research applies a number of methods, including field geological surveys; petrography of basalts, structural features (degree of crystallization of mesostasis, structural position of minerals and, in particular, copper, ratio of globular formations and minerals that surround them, relationship between globules), macro- and microtextural features of rocks; geochemical research: determination of the content of the main chemical components of the rocks by the method of gross chemical analysis and copper content; geological and morphostructural studies: construction of a map of paleorelief and thickness of continental flood basalt of the Luchichiv stratum (according to the section of wells). Results. The constructed maps of the thickness and paleo surface of the Luchychi stratum show the spatial variability of the basalt thickness and the reflection of the effective tectonic situation on its paleo surface, which can be "read" by relief elements. It is established that high copper content in basalts is spatially confined to areas of maximum thickness and shifted vertically to the near-roof and, partially, plantar parts of the basalt thickness, and the degree of their crystallization increases in the direction of the inner parts of bodies. This situation with the spatial arrangement of native mineralization indicates the existence within these areas of local isolated thermostated systems. They evolved in their internal parts in conditions close to the intrusive ones (relatively slow decrease in melt temperature, crystallization of rock differences almost devoid of volcanic glass – dolerite-basalts with the transition to dolerites in the central part). Such physicochemical conditions caused long-term migration of gaseous, gaseous-liquid and liquid fluids, providing concomitant extraction, concentration, transfer and deposition not only of native copper, but also a number of petrogenic oxides (alkalis, iron, partially calcium, silicium). The latter subsequently formed a number of low-temperature minerals, the most common of which are zeolites, calcite, and iron compounds. In areas with small and minimum thickness of basalts, the above facts are observed in a reduced form, and in some places are virtually absent. The research has established the complete absence of signs of hydrothermal copper ore mineralization. The latter indicates the lack of evidence about the formation of native mineralization of the hydro
意图本文的主要目的是利用古地表厚度和地形图,研究Volyn西部Ratne–Kamin Kashyrskyi地区埃迪卡拉纪Ratne套Luchychi地层大陆洪流玄武岩厚度和地形的空间分布特征。该研究还侧重于地层的特定参数与天然矿化浓度的空间变化及其相对于地层顶部(底部)的定位之间的相关性。方法该研究采用了多种方法,包括实地地质调查;玄武岩的岩石学、结构特征(中间相的结晶程度、矿物的结构位置,特别是铜的结构位置、球状构造与周围矿物的比例、球状构造之间的关系)、岩石的宏观和微观结构特征;地球化学研究:用总化学分析法和铜含量测定岩石主要化学成分的含量;地质和形态结构研究:绘制Luchichiv地层大陆洪流玄武岩的古地形和厚度图(根据井剖面)。后果构造的Luchychi地层厚度和古表面图显示了玄武岩厚度的空间变异性,以及有效构造情况在其古表面上的反映,可以通过地形元素“读取”。已经确定,玄武岩中的高铜含量在空间上局限于最大厚度的区域,并垂直向玄武岩厚度的近顶部和部分足底移动,并且它们的结晶程度在主体内部的方向上增加。这种天然矿化的空间排列情况表明,在这些区域内存在局部隔离的恒温系统。它们的内部在接近侵入岩的条件下进化(熔体温度下降相对缓慢,岩石差异结晶几乎没有火山玻璃-粗玄玄武岩,中部过渡到粗玄岩)。这种物理化学条件导致气态、气态、液态流体的长期迁移,不仅提供了天然铜的提取、浓缩、转移和沉积,还提供了许多岩石成因氧化物(碱、铁、部分钙、硅)。后者随后形成了许多低温矿物,其中最常见的是沸石、方解石和铁化合物。在玄武岩厚度较小和最小的地区,上述事实以减少的形式观察到,在一些地方几乎不存在。这项研究已经证实完全没有热液铜矿成矿的迹象。后者表明缺乏关于热液型原生矿化形成的证据。我们提供了地质和岩石地球化学事实,这些事实为考虑与作者早期提出的流体液化假说有关的天然铜矿化形成过程的情景提供了依据。科学新颖性。这项研究首次使绘制沃林西部Ratne–Kamin Kashyrskyi地区Luchychi地层玄武岩古表面的厚度和起伏图成为可能。根据实际材料表明,玄武岩体内天然矿化的垂直分布和定位与玄武岩的厚度自然相关。天然铜的值与主体厚度直接相关,在具有最大厚度的区域达到最大值,在最小厚度处达到背景值。实际意义。首次将鲁池池组玄武岩的地质、岩石学、地质和形态结构数据与玄武岩中的铜含量进行了比较。地质生产组织可在进行勘探工作时使用所提出的方法,为Ratne Horst背斜内的North Hirnyky和Rafalvika矿田(矿石节点)的勘探准备有希望的区域。所获得的原始物质可以作为一种新的寻找原生矿化的方法分布在大陆洪流玄武岩分布的其他区域。
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引用次数: 1
GEODYNAMICS
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2019-07-01 DOI: 10.23939/jgd2019.01.043
A. Aliyev, O. Abbasov
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引用次数: 0
GEODYNAMICS 地球动力学
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2019-07-01 DOI: 10.23939/jgd2019.01.005
P. Dvulit, S. Savchuk, I. Sosonka
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引用次数: 1
GEODYNAMICS 地球动力学
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2019-07-01 DOI: 10.23939/jgd2019.01.060
O. Hnylko, S. Hnylko
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引用次数: 1
GEODYNAMICS 地球动力学
IF 0.3 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2018-07-10 DOI: 10.23939/jgd2018.01.040
M. Tsar
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引用次数: 1
期刊
Geodynamics
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