Coseismic geochemical variations in some gas emissions of Umbria region (Central Italy)

被引：20
|
作者：
Heinicke, J
Italiano, F [1 ]
Lapenna, V
Martinelli, G
Nuccio, PM
机构：
[1] CNR, Ist Geochim Fluidi, Palermo, Italy
[2] Saechsiche Akad Wissenschanften Leipzig, Freiburg, Germany
[3] CNR, Ist Metodol Avanzate Anal Ambientale, Potenza, Italy
[4] Serv Geol & Cartog, Reg Emilia Romagna, Italy
[5] Univ Palermo, Dipartimento CFTA, I-90133 Palermo, Italy
来源：
PHYSICS AND CHEMISTRY OF THE EARTH PART A-SOLID EARTH AND GEODESY | 2000年 / 25卷 / 03期
关键词：
D O I：
10.1016/S1464-1895(00)00046-6
中图分类号：
P3 [地球物理学]; P59 [地球化学];
学科分类号：
0708 ; 070902 ;
摘要：
Coseismic geochemical variations have been detected in some gaseous vents and natural springs during the last seismic crisis occurred in Umbria region (Central Apennines), that started on September 26(th), 1997 with several moderate earthquakes (up to Ml 5.8). The results of chemical analyses performed on both gas and water samples taken at a weekly rate, combined with analyses on continuous gas flow rate nearby San Faustino site, suggest that the variations can be interpreted as possible consequence of the crustal permeability changes induced by earthquake shaking. (C) 2000 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码：289 / 293
页数：5
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