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The formation and growth mechanisms of young back-arc spreading ridges from high-resolution bathymetry:The Marsili Seamount(Tyrrhenian Sea,Italy)

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Geoscience Frontiers 2024年第1期15卷 325-338页

作者： Eugenio Nicotra Salvatore Passaro guido ventura Dipartimento di Biologia Ecologia e Scienze della Terra Universitàdella Calabria87036 Arcavacata di RendeCosenzaItaly Istituto di Scienze Marine CNR 80133 NapoliItaly Istituto Nazionale di Geofisica e Vulcanologia 00143 RomaItaly Istituto per lo Studio degli impatti Antropici e Sostenibilitáin ambiente marino CNR 91026 Capo GranitolaTrapaniItaly

The formation and growth mechanisms of Mid-Ocean Ridges(MOR)are relatively well known,whereas those of back-arc spreading ridges are comparatively less known because geophysical,geochemical,and morphological data are scarce and of low *** we present a high-resolution bathymetry of the Marsili Seamount(MS;1 Ma-3 ka),which represents the inflated spreading ridge of the 2 Ma old Marsili back-arc basin associated to the subduction of the Ionian Sea below the Calabrian Arc and Tyrrhenian *** is 70 km long,30 km wide,and its height reaches about 3000 m from surrounding *** new digital bathymetric model has a 5 m grid cell size resolution and covers the MS bathymetry from-1670 mbsl to the top at-491 *** conduct morphometric and morphological analyses of the bathymetry and recognize landforms due to volcanic,tectonic,hydrothermal and gravity *** consists of volcanoes related to fissural and central-type activity,this latter located at the northern and southern tips of the main dike *** swarms represent the surface expression of different ridge segments whose strikes are controlled by the larger scale back-arc spreading processes and by the local occurrence of an active hydrothermal *** latter develops in a flat area between two partly overlapping ridge segments where historical volcanism and extensional processes *** ridges represent the embryonic stage of the formation of transform-like *** volcanoes,the northern of which is characterized by a caldera,form at the tips of MS because the decrease in width of the major volcanic fissures promotes vent localization associated with the formation of sill-like reservoirs from which central-type vents may *** processes affecting the MS flanks are due to shallow seafloor *** collapses affecting the northernmost central-type polygenic volcano must be included in the evaluation of the hazard related to potential *** dipping faul

关键词： Back-arc spreading ridge Morphology Tectonics Volcanism Marsili seamount

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Flow Behavior of Clay-Silt to Sand-Silt Water-Rich Suspensions at Low to High Shear Rates: Implications for Slurries, Transitional Flows, and Submarine Debris-Flows

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Acta Geologica Sinica(English Edition) 2018年第6期92卷 2395-2404页

作者： Pierdomenico DEL GAUDIO guido ventura Istituto Nazionale di Geofisica e Vulcanologia Via di Vigna Murata 60500143 RomeItaly Istituto per l'Ambiente Marino Costiero Consiglio Nazionale delle RicercheNaplesItaly

Water-rich clay to sand suspensions show a shear rate dependent flow behavior and knowledge of the appropriate rheological model is relevant for sedimentological, industrial and hydraulic studies. We present experimental rheological measurements of water-rich(40 to 60 wt%) clay to silt(population A) and silt to sand(population B) suspensions mixed in different proportions. The data evidence a shear rate dependent shear thinning-shear thickening transition. At lower shear rates, the suspensions organize in chains of particles, whereas at higher shear rates, these chains disrupt so increasing the viscosity. The viscosity, consistency and yield stress decrease as the A+B fraction decreases as the content of B particles increases. This behavior reflects the competing effects of the lubrication and frictional processes as a function of particle size and water content. Transitional flows form by the incorporation of small amounts of the finer fraction while ‘oceanic floods’ form at the estuary of rivers and the submarine debris-flows increase their velocity by incorporating water. The critical Reynolds number of the studied suspensions is ～2000±100 suggesting that the grainsize plays a major role in the laminar to turbulent transition. Our results have implications for the modeling of sediment flows and the hazard related to floods.

关键词： rheology water-sediment suspensions slurry sludge transitional flows and mud flows volcanogenic sediment-water flows oceanic floods

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Modeling the multi-level plumbing system of the Changbaishan caldera from geochemical, mineralogical, Sr-Nd isotopic and integrated geophysical data

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Geoscience Frontiers 2021年第5期12卷 17-36页

作者： Jian Yi Pujun Wang Xuanlong Shan guido ventura Chengzhi Wu Jiannan Guo Pencheng Liu Jiahui Li College of Earth Science Jilin UniversityJianshe Street 2199Changchun 130061China Key Laboratory for Evolution of Past Life and Environment in Northeast Asia(Jilin University) Ministry of EducationChangchun 130026China Istituto Nazionale di Geofisica e Vulcanologia Via di Vigna Murata605Roma 00143Italy Istituto per lo Studio degli impatti Antropici e Sostenibilitàin ambiente marino(IAS) Capo Granitola(TP)91021Italy Changbai Mountain Tianchi Volcano Observatory Chibei DistrictAntu 133613China

Changbaishan,an intraplate volcano,is characterized by an approximately 6 km wide summit caldera and last erupted in *** experienced a period of unrest between 2002 and *** activity developed in three main stages,including shield volcano(basalts),cone-construction(trachyandesites to trachytes with minor basalts),and caldera-forming stages(trachytes to comendites).This last stage is associated with one of the more energetic eruptions of the last millennium on Earth,the 946 CE,VEI 7 Millennium Eruption(ME),which emitted over 100 km^(3) of *** to other active calderas,the plumbing system of Changbaishan and its evolution mechanisms remain poorly ***,we merge new whole-rock,glass,mineral,isotopic,and geobarometry data with geophysical data and present a model of the plumbing *** results show that the volcano is characterized by at least three main magma reservoirs at different depths:a basaltic reservoir at the Moho/lower crust depth,an intermediate reservoir at 10-15 km depth,and a shallower reservoir at 0.5-3 km *** shallower reservoir was involved in the ME eruption,which was triggered by a fresh trachytic melt entering a shallower reservoir where a comenditic magma was *** trachytes and comendites originate from fractional crystallization processes and minor assimilation of upper crust material,while the less evolved melts assimilate lower crust ***-eruptive magma mingling occurred during the ME eruption *** magma reservoirs of the caldera-forming stage partly reactivate those of the cone-construction *** depth of the magma storage zones is controlled by the layering of the *** plumbing system of Changbaishan is vertically extensive,with crystal mush reservoirs renewed by the replenishment of new trachytic to trachyandesitic magma from *** other volcanoes,evidence of a basaltic recharge is *** interpretation of the signals preceding possible future erupt

关键词： Changbaishan volcano Caldera Plumbing system Triggering mechanism Storage depth

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通过多时相机载激光雷达数据追踪和调查复杂活动滑坡 —Momaguto滑坡（意大利南部）

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水文地质工程地质技术方法动态 2012年第1期 50-61页

作者： guido ventura 盖利亚（翻译）孙建平（校对） Istituto Nazionale di Geofisica e Vulcanologia Via di Vigna Murata 605 00143 Roma Italy Istituto Nazionale di Geofisica e Vulcanologia sezione Osservatorio VesuvianoVia Diocleziano 328 80124 Napoli Italy 不详

本文论述了对Montaguyo（意大利）活动滑坡的多时相激光雷达的研究。通过四个激光雷达分别获取了2006年5月、2009年7月、2010年4月、2010年6月的数字地形模型。通过对选定形态参数的解译（表面粗糙度、地形表面残差）以及这些参数时空... 详细信息

本文论述了对Montaguyo（意大利）活动滑坡的多时相激光雷达的研究。通过四个激光雷达分别获取了2006年5月、2009年7月、2010年4月、2010年6月的数字地形模型。通过对选定形态参数的解译（表面粗糙度、地形表面残差）以及这些参数时空变化的统计分析能够进行滑坡的再现和追踪。已经完成滑坡边界的监控，进行了隆起和沉降区、形变量和／或堆积物、垂直和水平位移的平均速率（退缩的平均速率和滑坡前端的推进速率）估算。对在不同时间影响滑坡的形变结构（陡坡、裂缝、褶皱）进行了制图；其中一些结构表征了滑坡即将进入不稳定过程的前兆或提供了结构位置相关信息。识别了不同的活动（如岩崩和泥石流）和几何形状（例如沟渠流动），检测了由人工排水和地面处理／清理工作引起的地形特征随时间的变化。我们根据激光雷达获得的信息能够解译滑坡的运动。研究结果表明，利用机载激光雷达能够提供重力．控制过程相关监测策略的新观点。

关键词：机载激光雷达(Airbome LiDAR)滑坡监测形态参数地形变化时空分析

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