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首页> 外文期刊>Journal of the Geological Society >Structural features of the July-August 2001 Mount Etna eruption: evidence for a complex magma supply system
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Structural features of the July-August 2001 Mount Etna eruption: evidence for a complex magma supply system

机译:2001年7月至8月埃特纳火山喷发的结构特征:复杂岩浆供应系统的证据

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摘要

We describe the evolution of the volcanic activity and deformation patterns observed at Mount Etna during the July–August 2001 eruption. Seismicity started at 3000 m below sea level on 13 July, accompanied by moderate ground swelling. Ground deformation culminated on 16 July with the development of a NE–SW graben c. 500 m wide and c. 1 m deep in the Cisternazza area at 2600–2500 m above sea level on the southern slope of the volcano. On 17 July, the eruption started at the summit of Mount Etna from the SE Crater (central–lateral eruptive system), from which two radial, c. 30 m wide, c. 3000 m long fracture zones, associated with eruptive fissures, propagated both southward (17 July) and northeastward (20 July). On 18 July, a new vent formed at 2100 m elevation, at the southern base of the Montagnola, followed on the next day by the opening of a vent further upslope, at 2550 m (eccentric eruptive system). The eruption lasted for 3 weeks. Approximately 80% of the total lava volume was erupted from the 2100 m and the 2550 m vents. The collected structural data suggest that the Cisternazza graben developed as a passive local response of the volcanic edifice to the ascent of a north–south eccentric dyke, which eventually reached the ground surface in the Montagnola area (18–19 July). In contrast, the two narrow fracture zones radiating from the summit are interpreted as the lateral propagation, from the conduit of the SE Crater, of north–south- and NE–SW-oriented shallow dykes, 2–3 m wide. The evolution of the fracture pattern together with other volcanological data (magma ascent and effusion rate, eruptive style, petrochemical characteristics of the erupted products, and petrology of xenoliths within magma) suggest that the eccentric and central–lateral eruptions were fed by two distinct magmatic systems. Examples of eccentric activity accompanied by central–lateral events have never been described before at Etna.
机译:我们描述了在2001年7月至8月爆发的埃特纳火山上观察到的火山活动和形变的演变过程。地震于7月13日在海平面以下3000 m开始,并伴有中等程度的地面膨胀。随着 NE–SW抓斗c的发展,地面 变形在7月16日达到顶点。宽500 m和c。火山南坡 上海拔2600–2500 m的Cisternazza 区域深1 m。 7月17日,爆发是从SE火山口(中央-侧面喷发 系统)在埃特纳火山的山顶上开始的,其中两个放射线为c。宽30 m与爆发裂缝相关的3000 m长 断裂带向南(7月17日)和东北(7月20日)传播。 7月18日 在Montagnola的南部 基地的2100 m高处形成了一个新的通风口,第二天又打开了 在2550 m(偏心喷发系统)处进一步向上喷口。 喷发持续了3周。从2100 m和2550 m的喷口喷出的熔岩总量约为80%。 收集的结构数据表明,Cisternazzagrapen 作为火山大厦 对南北偏心堤坝上升的被动局部响应而发展,最终 到达蒙塔尼奥拉地区的地表(18-19 < sup> 7月)。相比之下,从山顶辐射出 的两个狭窄裂缝区域被解释为从东南部火山口的管道向南和向南传播的横向传播 NE-SW定向的浅堤,宽2–3 m。断裂模式的演变 以及其他火山岩数据 (岩浆上升和渗出速率,喷发类型,喷出产品的石油化学特征)以及岩浆内的异岩岩 的岩石学表明,偏心和中央-外侧 喷发是由两个不同的岩浆系统提供的。以前在Etna从未描述过偏心活动伴有中央-侧面事件 的例子。

著录项

  • 来源
    《Journal of the Geological Society》 |2003年第4期|531-544|共14页
  • 作者单位

    Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Piazza Roma 2, 95123 Catania, Italy (e-mail: neri@ct.ingv.it);

    Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Piazza Roma 2, 95123 Catania, Italy (e-mail: neri@ct.ingv.it);

    Dip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italy;

    Dip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italy;

    Dip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italy;

    Dip. Scienze Geologiche Roma TRE, Largo S.L. Murialdo 1, 00146 Rome, Italy;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Mount Etna; July–August 2001 Eruption; magmas; dykes;

    机译:埃特纳火山;2001年7月至8月爆发;岩浆堤防;

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