Study of some precursory phenomena for the umbria earthquake of September 19, 1979

Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative t...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Alessio, M. [verfasserIn] Allegri, L. Bella, F. Della Monica, G. Ermini, A. Improta, S. Biagi, P. F.

Format:	Artikel
Sprache:	Englisch

Erschienen:	1980

Schlagwörter:	Radon Radon Concentration Precursory Phenomenon Radon Content Pseudostationary Phase

Anmerkung:	© Società Italiana di Fisica 1980

Übergeordnetes Werk:	Enthalten in: Il Nuovo Cimento C - Kluwer Academic Publishers, 1978, 3(1980), 6 vom: Nov., Seite 589-600
Übergeordnetes Werk:	volume:3 ; year:1980 ; number:6 ; month:11 ; pages:589-600

Links:	Volltext

DOI / URN:	10.1007/BF02507185

Katalog-ID:	OLC2055363719

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520			\|a Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative to some points of observation show an anomaly during the period from the beginning of May to September 19, when the Umbria earthquake took place. This anomaly seems to be a clear manifestation of precursory phenomena of the earthquake: the value of the magnitude, calculated on the basis of the anomaly duration, is in good agreement with the one derived from the seismograms. The fact that no precursory phenomena were observed at other observation points in the same region is put in relation with the different mobility of the sites exhibited during the measurements.
650		4	\|a Radon
650		4	\|a Radon Concentration
650		4	\|a Precursory Phenomenon
650		4	\|a Radon Content
650		4	\|a Pseudostationary Phase
700	1		\|a Allegri, L. \|4 aut
700	1		\|a Bella, F. \|4 aut
700	1		\|a Della Monica, G. \|4 aut
700	1		\|a Ermini, A. \|4 aut
700	1		\|a Improta, S. \|4 aut
700	1		\|a Biagi, P. F. \|4 aut
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952			\|d 3 \|j 1980 \|e 6 \|c 11 \|h 589-600

Indexfelder

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allfields	10.1007/BF02507185 doi (DE-627)OLC2055363719 (DE-He213)BF02507185-p DE-627 ger DE-627 rakwb eng 530 VZ 16,13 ssgn Alessio, M. verfasserin aut Study of some precursory phenomena for the umbria earthquake of September 19, 1979 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Società Italiana di Fisica 1980 Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative to some points of observation show an anomaly during the period from the beginning of May to September 19, when the Umbria earthquake took place. This anomaly seems to be a clear manifestation of precursory phenomena of the earthquake: the value of the magnitude, calculated on the basis of the anomaly duration, is in good agreement with the one derived from the seismograms. The fact that no precursory phenomena were observed at other observation points in the same region is put in relation with the different mobility of the sites exhibited during the measurements. Radon Radon Concentration Precursory Phenomenon Radon Content Pseudostationary Phase Allegri, L. aut Bella, F. aut Della Monica, G. aut Ermini, A. aut Improta, S. aut Biagi, P. F. aut Enthalten in Il Nuovo Cimento C Kluwer Academic Publishers, 1978 3(1980), 6 vom: Nov., Seite 589-600 (DE-627)129367362 (DE-600)161886-6 (DE-576)014741970 1124-1896 nnns volume:3 year:1980 number:6 month:11 pages:589-600 https://doi.org/10.1007/BF02507185 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-AST SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 GBV_ILN_32 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_170 GBV_ILN_2012 GBV_ILN_2279 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4155 GBV_ILN_4306 GBV_ILN_4319 GBV_ILN_4323 AR 3 1980 6 11 589-600
spelling	10.1007/BF02507185 doi (DE-627)OLC2055363719 (DE-He213)BF02507185-p DE-627 ger DE-627 rakwb eng 530 VZ 16,13 ssgn Alessio, M. verfasserin aut Study of some precursory phenomena for the umbria earthquake of September 19, 1979 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Società Italiana di Fisica 1980 Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative to some points of observation show an anomaly during the period from the beginning of May to September 19, when the Umbria earthquake took place. This anomaly seems to be a clear manifestation of precursory phenomena of the earthquake: the value of the magnitude, calculated on the basis of the anomaly duration, is in good agreement with the one derived from the seismograms. The fact that no precursory phenomena were observed at other observation points in the same region is put in relation with the different mobility of the sites exhibited during the measurements. Radon Radon Concentration Precursory Phenomenon Radon Content Pseudostationary Phase Allegri, L. aut Bella, F. aut Della Monica, G. aut Ermini, A. aut Improta, S. aut Biagi, P. F. aut Enthalten in Il Nuovo Cimento C Kluwer Academic Publishers, 1978 3(1980), 6 vom: Nov., Seite 589-600 (DE-627)129367362 (DE-600)161886-6 (DE-576)014741970 1124-1896 nnns volume:3 year:1980 number:6 month:11 pages:589-600 https://doi.org/10.1007/BF02507185 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-AST SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 GBV_ILN_32 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_170 GBV_ILN_2012 GBV_ILN_2279 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4155 GBV_ILN_4306 GBV_ILN_4319 GBV_ILN_4323 AR 3 1980 6 11 589-600
allfields_unstemmed	10.1007/BF02507185 doi (DE-627)OLC2055363719 (DE-He213)BF02507185-p DE-627 ger DE-627 rakwb eng 530 VZ 16,13 ssgn Alessio, M. verfasserin aut Study of some precursory phenomena for the umbria earthquake of September 19, 1979 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Società Italiana di Fisica 1980 Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative to some points of observation show an anomaly during the period from the beginning of May to September 19, when the Umbria earthquake took place. This anomaly seems to be a clear manifestation of precursory phenomena of the earthquake: the value of the magnitude, calculated on the basis of the anomaly duration, is in good agreement with the one derived from the seismograms. The fact that no precursory phenomena were observed at other observation points in the same region is put in relation with the different mobility of the sites exhibited during the measurements. Radon Radon Concentration Precursory Phenomenon Radon Content Pseudostationary Phase Allegri, L. aut Bella, F. aut Della Monica, G. aut Ermini, A. aut Improta, S. aut Biagi, P. F. aut Enthalten in Il Nuovo Cimento C Kluwer Academic Publishers, 1978 3(1980), 6 vom: Nov., Seite 589-600 (DE-627)129367362 (DE-600)161886-6 (DE-576)014741970 1124-1896 nnns volume:3 year:1980 number:6 month:11 pages:589-600 https://doi.org/10.1007/BF02507185 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-AST SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 GBV_ILN_32 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_170 GBV_ILN_2012 GBV_ILN_2279 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4155 GBV_ILN_4306 GBV_ILN_4319 GBV_ILN_4323 AR 3 1980 6 11 589-600
allfieldsGer	10.1007/BF02507185 doi (DE-627)OLC2055363719 (DE-He213)BF02507185-p DE-627 ger DE-627 rakwb eng 530 VZ 16,13 ssgn Alessio, M. verfasserin aut Study of some precursory phenomena for the umbria earthquake of September 19, 1979 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Società Italiana di Fisica 1980 Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative to some points of observation show an anomaly during the period from the beginning of May to September 19, when the Umbria earthquake took place. This anomaly seems to be a clear manifestation of precursory phenomena of the earthquake: the value of the magnitude, calculated on the basis of the anomaly duration, is in good agreement with the one derived from the seismograms. The fact that no precursory phenomena were observed at other observation points in the same region is put in relation with the different mobility of the sites exhibited during the measurements. Radon Radon Concentration Precursory Phenomenon Radon Content Pseudostationary Phase Allegri, L. aut Bella, F. aut Della Monica, G. aut Ermini, A. aut Improta, S. aut Biagi, P. F. aut Enthalten in Il Nuovo Cimento C Kluwer Academic Publishers, 1978 3(1980), 6 vom: Nov., Seite 589-600 (DE-627)129367362 (DE-600)161886-6 (DE-576)014741970 1124-1896 nnns volume:3 year:1980 number:6 month:11 pages:589-600 https://doi.org/10.1007/BF02507185 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-AST SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 GBV_ILN_32 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_170 GBV_ILN_2012 GBV_ILN_2279 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4155 GBV_ILN_4306 GBV_ILN_4319 GBV_ILN_4323 AR 3 1980 6 11 589-600
allfieldsSound	10.1007/BF02507185 doi (DE-627)OLC2055363719 (DE-He213)BF02507185-p DE-627 ger DE-627 rakwb eng 530 VZ 16,13 ssgn Alessio, M. verfasserin aut Study of some precursory phenomena for the umbria earthquake of September 19, 1979 1980 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Società Italiana di Fisica 1980 Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative to some points of observation show an anomaly during the period from the beginning of May to September 19, when the Umbria earthquake took place. This anomaly seems to be a clear manifestation of precursory phenomena of the earthquake: the value of the magnitude, calculated on the basis of the anomaly duration, is in good agreement with the one derived from the seismograms. The fact that no precursory phenomena were observed at other observation points in the same region is put in relation with the different mobility of the sites exhibited during the measurements. Radon Radon Concentration Precursory Phenomenon Radon Content Pseudostationary Phase Allegri, L. aut Bella, F. aut Della Monica, G. aut Ermini, A. aut Improta, S. aut Biagi, P. F. aut Enthalten in Il Nuovo Cimento C Kluwer Academic Publishers, 1978 3(1980), 6 vom: Nov., Seite 589-600 (DE-627)129367362 (DE-600)161886-6 (DE-576)014741970 1124-1896 nnns volume:3 year:1980 number:6 month:11 pages:589-600 https://doi.org/10.1007/BF02507185 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-AST SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 GBV_ILN_32 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_170 GBV_ILN_2012 GBV_ILN_2279 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4155 GBV_ILN_4306 GBV_ILN_4319 GBV_ILN_4323 AR 3 1980 6 11 589-600
language	English
source	Enthalten in Il Nuovo Cimento C 3(1980), 6 vom: Nov., Seite 589-600 volume:3 year:1980 number:6 month:11 pages:589-600
sourceStr	Enthalten in Il Nuovo Cimento C 3(1980), 6 vom: Nov., Seite 589-600 volume:3 year:1980 number:6 month:11 pages:589-600
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Radon Radon Concentration Precursory Phenomenon Radon Content Pseudostationary Phase
dewey-raw	530
isfreeaccess_bool	false
container_title	Il Nuovo Cimento C
authorswithroles_txt_mv	Alessio, M. @@aut@@ Allegri, L. @@aut@@ Bella, F. @@aut@@ Della Monica, G. @@aut@@ Ermini, A. @@aut@@ Improta, S. @@aut@@ Biagi, P. F. @@aut@@
publishDateDaySort_date	1980-11-01T00:00:00Z
hierarchy_top_id	129367362
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id	OLC2055363719
language_de	englisch
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author	Alessio, M.
spellingShingle	Alessio, M. ddc 530 ssgn 16,13 misc Radon misc Radon Concentration misc Precursory Phenomenon misc Radon Content misc Pseudostationary Phase Study of some precursory phenomena for the umbria earthquake of September 19, 1979
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topic_title	530 VZ 16,13 ssgn Study of some precursory phenomena for the umbria earthquake of September 19, 1979 Radon Radon Concentration Precursory Phenomenon Radon Content Pseudostationary Phase
topic	ddc 530 ssgn 16,13 misc Radon misc Radon Concentration misc Precursory Phenomenon misc Radon Content misc Pseudostationary Phase
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title	Study of some precursory phenomena for the umbria earthquake of September 19, 1979
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title_full	Study of some precursory phenomena for the umbria earthquake of September 19, 1979
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author_browse	Alessio, M. Allegri, L. Bella, F. Della Monica, G. Ermini, A. Improta, S. Biagi, P. F.
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title_sort	study of some precursory phenomena for the umbria earthquake of september 19, 1979
title_auth	Study of some precursory phenomena for the umbria earthquake of September 19, 1979
abstract	Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative to some points of observation show an anomaly during the period from the beginning of May to September 19, when the Umbria earthquake took place. This anomaly seems to be a clear manifestation of precursory phenomena of the earthquake: the value of the magnitude, calculated on the basis of the anomaly duration, is in good agreement with the one derived from the seismograms. The fact that no precursory phenomena were observed at other observation points in the same region is put in relation with the different mobility of the sites exhibited during the measurements. © Società Italiana di Fisica 1980
abstractGer	Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative to some points of observation show an anomaly during the period from the beginning of May to September 19, when the Umbria earthquake took place. This anomaly seems to be a clear manifestation of precursory phenomena of the earthquake: the value of the magnitude, calculated on the basis of the anomaly duration, is in good agreement with the one derived from the seismograms. The fact that no precursory phenomena were observed at other observation points in the same region is put in relation with the different mobility of the sites exhibited during the measurements. © Società Italiana di Fisica 1980
abstract_unstemmed	Summary The data relative to measurements of the radon content in ground water and variations in the apparent vertical at two stations in Latium, one near Mentana and another near Antrodoco, are examined. At every station, observations were made in several points. The experimental results relative to some points of observation show an anomaly during the period from the beginning of May to September 19, when the Umbria earthquake took place. This anomaly seems to be a clear manifestation of precursory phenomena of the earthquake: the value of the magnitude, calculated on the basis of the anomaly duration, is in good agreement with the one derived from the seismograms. The fact that no precursory phenomena were observed at other observation points in the same region is put in relation with the different mobility of the sites exhibited during the measurements. © Società Italiana di Fisica 1980
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title_short	Study of some precursory phenomena for the umbria earthquake of September 19, 1979
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author2	Allegri, L. Bella, F. Della Monica, G. Ermini, A. Improta, S. Biagi, P. F.
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