Relation between Morphometric Parameters of Relief Characterizing the Fracturing of the Upper Part of the Lithosphere and Manifestations of Volcanism in the Malko-Petropavlovsk Zone

IF 0.9 4区 地球科学 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
A. O. Agibalov, O. V. Bergal-Kuvikas, V. A. Zaitsev, V. M. Makeev, A. A. Sentsov
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Abstract

Numerous monogenic volcanic structures and thermal water outlets in the Malko-Petropavlovsk zone of transverse dislocations (MPZ) on the Kamchatka Peninsula have been established to be localized in areas of increased fracturing in the upper part of the earth’s crust. In the paper, we characterize at a quantitative level the association of manifestations of volcanism and hydrothermal–magmatic systems with positive anomalies in the morphometric characteristics of the relief (specific length of “weak” zones and watercourses, density of intersections of rivers and lineaments, and dispersion of slope exposure). A high degree of consistency in the orientations of faults and weak zones are revealed: both rose diagrams show northwestern, meridional, and northeastern directions, while the average circular values of their strikes are 75° and 76°, respectively. According to the Nechaev method (Institute of Physics of the Earth, Russian Academy of Sciences (IPE RAS)), 3D models of tectonic fragmentation of the earth’s crust in the depth range of 2.5–10 km are obtained based on the calculation of the specific lengths of weak zones and watercourses. The Pearson correlation coefficient between the point elements of these voxel models is 0.86. Based on the relation between morphometric characteristics and manifestations of volcanism, we suggest that, in general, the nature of the fracturing reflected in the relief is one of the main factors determining the hydrothermal–magmatic activity of the studied area, which has a great effect on human economic activity.

Abstract Image

表征岩石圈上部断裂的地形参数与马尔科-彼得罗巴甫洛夫斯克地带火山活动表现之间的关系
摘要 堪察加半岛马尔科-彼得罗巴甫洛夫斯克横向错动带(MPZ)中的许多单源火山结构和热水出口已被确定位于地壳上部断裂增加的区域。在本文中,我们从定量的角度描述了火山活动和热液-岩浆系统的表现与地貌形态特征("薄弱 "地带和水道的具体长度、河流和线状物交汇的密度以及斜坡出露的分散性)的正异常之间的联系。断层和薄弱带的走向高度一致:两张玫瑰图均显示西北、经向和东北方向,其走向的平均圆周值分别为 75° 和 76°。根据涅恰耶夫方法(俄罗斯科学院地球物理研究所),在计算薄弱带和水道具体长度的基础上,获得了 2.5-10 千米深度范围内地壳构造破碎的三维模型。这些体素模型的点元素之间的皮尔逊相关系数为 0.86。根据形态特征与火山活动表现之间的关系,我们认为,总体而言,地形所反映的断裂性质是决定所研究地区热液-岩浆活动的主要因素之一,而热液-岩浆活动对人类经济活动具有重大影响。
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来源期刊
CiteScore
1.40
自引率
28.60%
发文量
56
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Atmospheric and Oceanic Physics is a journal that publishes original scientific research and review articles on vital issues in the physics of the Earth’s atmosphere and hydrosphere and climate theory. The journal presents results of recent studies of physical processes in the atmosphere and ocean that control climate, weather, and their changes. These studies have possible practical applications. The journal also gives room to the discussion of results obtained in theoretical and experimental studies in various fields of oceanic and atmospheric physics, such as the dynamics of gas and water media, interaction of the atmosphere with the ocean and land surfaces, turbulence theory, heat balance and radiation processes, remote sensing and optics of both media, natural and man-induced climate changes, and the state of the atmosphere and ocean. The journal publishes papers on research techniques used in both media, current scientific information on domestic and foreign events in the physics of the atmosphere and ocean.
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