Variations in Event-Bed Thickness-Frequency Distributions Near Volcanic Islands: Indicators of Varied Geological Processes

IF 2.9 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Yu-Chun Chang, José C. F. Kling, Julie C. Schindlbeck-Belo, Neil C. Mitchell, Kan-Hsi Hsiung, Toshiya Kanamatsu
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Abstract

A variety of subaerial and submarine events, including mass-wasting and volcanism, can generate sediment gravity flows and fallout deposits that are preserved in deep-water stratigraphic records. This study examines whether event beds with differing depositional and transport histories exhibit distinct thickness-frequency distributions. Analyzing over 4,500 event beds from seven drilling sites near Montserrat, the Izu Arc, the Kyushu-Palau Ridge, and Gran Canaria, the analyses explore variations in event-bed characteristics across different climatic periods, volcanic stages, and geomorphological settings. Statistical methods include characterizing thickness-frequency distributions and assessing subset similarity using t-tests and smoothed distribution patterns. The data-driven results indicate discernible differences where dominant geological processes vary. For example, volcanic growth stages at the Kyushu–Palau Ridge produced thicker, coarser, and more frequent event beds compared with quiescent stages. Similarly, beds from the north slope of Gran Canaria—where submarine canyons enhanced sediment delivery—were nearly twice as thick as those from the south. In contrast, indistinguishable characteristics between the rear and frontal Izu Arc subsets after 3 Ma are attributed to the development of an extensional zone supplying material to both arc sides. Comparable distributions were also observed within intervals with minimal geological differences. The reliability of this analytical approach depends on high-quality sediment recovery, as drilling-related disturbances may obscure primary depositional signals. Beyond stratigraphic characterization, the method shows broader potential for identifying the provenance of volcanic glass shards through geochemical comparisons and for evaluating the statistical compatibility of data sets from neighboring sites, ensuring sufficient sample size for robust integrated analyses.

Abstract Image

火山岛附近事件层厚度-频率分布的变化:不同地质过程的指标
各种陆上和海底事件,包括物质消耗和火山活动,可以产生沉积物重力流和沉降物沉积,这些沉积被保存在深水地层记录中。本研究探讨了具有不同沉积和运输历史的事件层是否表现出不同的厚度频率分布。研究人员分析了蒙特塞拉特、伊祖弧、九州-帕劳山脊和大加那利岛附近七个钻探点的4500多个事件层,探讨了不同气候时期、火山阶段和地貌环境下事件层特征的变化。统计方法包括表征厚度频率分布和使用t检验和平滑分布模式评估子集相似性。数据驱动的结果表明,在主导地质作用不同的地方,存在明显的差异。例如,与静止阶段相比,九州-帕劳山脊的火山生长阶段产生了更厚、更粗、更频繁的事件层。同样,来自大加那利岛北坡的河床——海底峡谷加强了沉积物的输送——几乎是来自南部的两倍厚。相比之下,在3 Ma之后,伊豆弧前后亚群之间难以区分的特征归因于向弧两侧提供物质的伸展带的发育。在地质差异最小的区间内也观察到类似的分布。这种分析方法的可靠性取决于高质量的沉积物回收,因为钻井相关的干扰可能会掩盖原始沉积信号。除了地层学表征之外,该方法还显示出更广泛的潜力,可以通过地球化学比较确定火山玻璃碎片的来源,并评估来自邻近地点的数据集的统计兼容性,确保足够的样本量进行稳健的综合分析。
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来源期刊
Geochemistry Geophysics Geosystems
Geochemistry Geophysics Geosystems 地学-地球化学与地球物理
CiteScore
5.90
自引率
11.40%
发文量
252
审稿时长
1 months
期刊介绍: Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged. Areas of interest for this peer-reviewed journal include, but are not limited to: The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution Principles and applications of geochemical proxies to studies of Earth history The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.
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