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Introduction to Volcanic Seismology 2nd edition, Volume 6 [Mīkstie vāki]

(Research Professor, Center for Volcanological Research, Colima University, Mexico)
  • Formāts: Paperback / softback, 474 pages, height x width: 229x152 mm, weight: 910 g
  • Sērija : Developments in Volcanology
  • Izdošanas datums: 14-Dec-2011
  • Izdevniecība: Elsevier Science Ltd
  • ISBN-10: 044456375X
  • ISBN-13: 9780444563750
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  • Formāts: Paperback / softback, 474 pages, height x width: 229x152 mm, weight: 910 g
  • Sērija : Developments in Volcanology
  • Izdošanas datums: 14-Dec-2011
  • Izdevniecība: Elsevier Science Ltd
  • ISBN-10: 044456375X
  • ISBN-13: 9780444563750
Citas grāmatas par šo tēmu:

Volcanic seismology represents the main, and often the only, tool to forecast volcanic eruptions and to monitor the eruption process. This book describes the main types of seismic signals at volcanoes, their nature and spatial and temporal distributions at different stages of eruptive activity. Following from the success of the first edition, published in 2003, the second edition consists of 19 chapters including significant revision and five new chapters. Organized into four sections, the book begins with an introduction to the history and topic of volcanic seismology, discussing the theoretical and experimental models that were developed for the study of the origin of volcanic earthquakes. The second section is devoted to the study of volcano-tectonic earthquakes, giving the theoretical basis for their occurrence and swarms as well as case stories of volcano-tectonic activity associated with the eruptions at basaltic, andesitic, and dacitic volcanoes. There were 40 cases of volcanic eruptions at 20 volcanoes that occurred all over the world from 1910 to 2005, which are discussed. General regularities of volcano-tectonic earthquake swarms, their participation in the eruptive process, their source properties, and the hazard of strong volcano-tectonic earthquakes are also described. The third section describes the theoretical basis for the occurrence of eruption earthquakes together with the description of volcanic tremor, the seismic signals associated with pyroclastic flows, rockfalls and lahars, and volcanic explosions, long-period and very-long-period seismic signals at volcanoes, micro-earthquake swarms, and acoustic events. The final section discuss the mitigation of volcanic hazard and include the methodology of seismic monitoring of volcanic activity, the examples of forecasting of volcanic eruptions by seismic methods, and the description of seismic activity in the regions of dormant volcanoes.

This book will be essential for students and practitioners of volcanic seismology to understand the essential elements of volcanic eruptions.

  • Provides a comprehensive overview of seismic signals at different stages of volcano eruption.
  • Discusses dozens of case histories from around the world to provide real-world applications.
  • Illustrations accompany detailed descriptions of volcano eruptions alongside the theories involved.

Recenzijas

Praise for the first edition: "...This book will be on the shelves of every geophysicist. I am delighted to report that it is useful, fun to read, full of information and worth rereading." --Natural Hazards

Papildus informācija

Illustrates, with detailed observations of numerous case studies, the elements of volcanic earthquakes at different stages of eruptive activity
Preface to the Second Edition xiii
Preface to the First Edition xv
1 Introduction
1(8)
1.1 Terms and Definitions
1(5)
1.1.1 Volcanic Terms
1(4)
1.1.2 Tectonic Terms
5(1)
1.1.3 Seismological Terms
6(1)
1.2 Subject of the Book
6(3)
Acknowledgments
7(2)
2 Seismicity at Volcanoes
9(20)
2.1 History of Seismic Monitoring of Volcanic Activity
9(5)
2.2 Classification of Volcanic Earthquakes
14(6)
2.3 Sequences of Volcanic Earthquakes
20(9)
2.3.1 Sequences of Volcano-Tectonic Earthquakes
20(7)
2.3.2 Sequences of Eruption Earthquakes
27(2)
3 Fundamentals of Volcanic Seismology
29(20)
3.1 Magma Flow within the Volcanic Conduit
29(3)
3.1.1 Magma Flow Regimes
30(1)
3.1.2 Modeling of Magma Flow Regimes
31(1)
3.2 Experimental Studies of the Volcanic Processes and Their Applications for the Seismic Sources
32(9)
3.2.1 Experimental Grounds of the Brittle Fracturing in the Rocks at High Temperatures and High Pressure
32(3)
3.2.2 Experimental Grounds of the Origin of Seismic Signals During the Magma Ascending Within the Volcanic Conduit
35(6)
3.3 General Description of the Source of Seismic Signals at Volcanoes
41(8)
3.3.1 Equivalent Force System Acting in the Earthquake Source
41(1)
3.3.2 Green's Functions
41(1)
3.3.3 Single Force
41(1)
3.3.4 Seismic Moment Tensor
42(1)
3.3.5 Waveform Inversion
43(6)
4 Origin of Volcano-Tectonic Earthquakes
49(18)
4.1 Migration of Magma and Its Seismic Potential
49(4)
4.2 Volcanism and Tectonics
53(6)
4.3 Source Nature of Volcano-Tectonic Earthquakes
59(4)
4.3.1 Waveform and Spectra
59(2)
4.3.2 Tensor Representation of the Source of Volcano-Tectonic Earthquake
61(2)
4.4 Models of Volcano-Tectonic Earthquake Sequences
63(4)
5 Volcano-Tectonic Earthquakes at Basaltic Volcanoes: Case Studies
67(32)
5.1 Volcano-Tectonic Earthquakes Associated with Shield Volcanoes
67(4)
5.1.1 Kilauea Volcano, Hawaii
67(4)
5.2 Volcano-Tectonic Earthquakes Associated with Stratovolcanoes
71(11)
5.2.1 Mount Etna, Sicily
71(7)
5.2.2 Oshima Volcano, Izu Islands
78(1)
5.2.3 Klyuchevskoy Volcano, Kamchatka
79(3)
5.3 Volcano-Tectonic Earthquakes Associated with Fissure Eruptions
82(8)
5.3.1 New Tolbachik Volcanoes, Kamchatka
83(3)
5.3.2 The 2005-2009 Ethiopia Rifting Episode
86(4)
5.4 Volcano-Tectonic Earthquakes Associated with Caldera Collapse
90(2)
5.4.1 Fernandina Volcano, Galapagos Islands
90(2)
5.5 Volcano-Tectonic Earthquakes Associated with Submarine Eruptions
92(7)
5.5.1 Teishi Knoll Volcano, Izu Islands
92(2)
5.5.2 Miyakejima Volcano, Izu Islands
94(5)
6 Volcano-Tectonic Earthquakes at Andesitic Volcanoes: Case Studies
99(22)
6.1 Volcano-Tectonic Earthquakes Associated with Volcanic "Directed Blasts"
99(6)
6.1.1 Bezymianny Volcano, Kamchatka
100(1)
6.1.2 Sheveluch Volcano, Kamchatka
101(4)
6.2 Volcano-Tectonic Earthquakes Associated with Phreatic and Phreato-Magmatic Explosions
105(10)
6.2.1 El Chichon Volcano, Mexico
105(1)
6.2.2 Volcan de Colima, Mexico
105(2)
6.2.3 Popocatepetl Volcano, Mexico
107(4)
6.2.4 Soufriere Hills Volcano, Montserrat
111(4)
6.3 Volcano-Tectonic Earthquakes Associated with Lava Extrusions
115(4)
6.3.1 Volcan de Colima, Mexico
115(4)
6.4 Volcano-Tectonic Earthquakes Associated with Flank Eruptions
119(2)
6.4.1 Sakurajima Volcano, Japan
119(2)
7 Volcano-Tectonic Earthquakes at Dacitic Volcanoes: Case Studies
121(24)
7.1 Volcano-Tectonic Earthquakes Associated with Summit Eruptions
121(15)
7.1.1 Mount St. Helens, Cascades
121(6)
7.1.2 Usu Volcano, Hokkaido
127(2)
7.1.3 Unzen Volcano, Kyushu
129(3)
7.1.4 Pinatubo Volcano, Luzon
132(4)
7.2 Volcano-Tectonic Earthquakes Associated with Flank Eruptions
136(9)
7.2.1 Usu Volcano, Hokkaido
137(8)
8 General Properties of Volcano-Tectonic Earthquake Swarms
145(16)
8.1 Properties of Volcano-Tectonic Earthquake Swarms Inferred from the Data of
Chapters 5-7
145(5)
8.1.1 Temporal Variations
145(3)
8.1.2 Spatial Distributions
148(1)
8.1.3 Posteruption Seismic Activity
149(1)
8.1.4 Duration of Seismic Swarms Prior to Eruption
150(1)
8.1.5 Position of a Volcanic Event According to the Stage of Volcano-Tectonic Earthquake Swarm
150(1)
8.2 Additional Data About Volcano-Tectonic Earthquake Swarm Properties
150(6)
8.2.1 Size of Volcano-Tectonic Earthquake Swarm Area
150(1)
8.2.2 Earthquake Swarm Duration
151(2)
8.2.3 Magnitude---Frequency Relations of Events in Volcano-Tectonic Earthquake Swarms
153(3)
8.3 Some Regularities in the Volcano-Tectonic Earthquake Swarms Proclaiming Reawakening of Andesitic and Dacitic Volcanoes
156(5)
8.3.1 Relationship Between the Duration of Stage 1 and the VEI of Forthcoming Explosion
158(1)
8.3.2 Relationship Between the Duration of Stage 2 and Postexplosion Dome Building
159(1)
8.3.3 The Conceptual Model of Reawakening Process
159(2)
9 Source Properties of Volcano-Tectonic Earthquakes
161(28)
9.1 Focal Mechanisms of Volcano-Tectonic Earthquakes: Double-Couple and Non-Double-Couple Models
161(7)
9.1.1 Double-Couple Model
161(4)
9.1.2 Non-Double-Couple Model
165(3)
9.2 Source Spectral Characteristics of Volcano-Tectonic Earthquakes
168(9)
9.2.1 Spectra of Total Records of Volcano-Tectonic Earthquakes
170(1)
9.2.2 Spectral Source Characteristics of Volcano-Tectonic Earthquakes
171(6)
9.3 Temporal Variations of the Source Spectral Characteristics and Focal Mechanisms of Volcano-Tectonic Earthquakes in the Course of Volcanic Activity
177(5)
9.3.1 Corner Frequencies Variations
177(3)
9.3.2 Stress-Drop Variations
180(2)
9.3.3 Stress Field Rotations
182(1)
9.4 Seismo-Tectonic Deformations in the Volcanic Region
182(7)
10 Significant Volcano-Tectonic Earthquakes and Their Role in Volcanic Processes
189(28)
10.1 Selection of Significant Volcano-Tectonic Earthquakes that Occurred in the Twentieth Century
191(1)
10.2 Focal Rupturing of Significant Volcano-Tectonic Earthquakes and Its Role in Volcanic Processes
191(8)
10.2.1 Rupturing of the Magnitude Mw 5.2 Earthquake Preceding the 1989 Teishi Knoll Submarine Eruption
193(2)
10.2.2 Rupturing of the Magnitude Mw 7.1 Earthquake Preceding the 1996 Akademia Nauk Volcano Subaqual Eruption
195(1)
10.2.3 Rupturing of the Magnitude Mw 5.6 Earthquake Preceding the 1996 Grimsvøtn Volcano Subglacial Eruption
196(3)
10.3 The Magnitude 7 Volcano-Tectonic Earthquakes in Volcanic Processes
199(4)
10.3.1 Event No. 2, Katmai, Alaska
200(1)
10.3.2 Event No. 3, Sakurajima, Japan
201(2)
10.4 Seismic Hazard of Significant Volcano-Tectonic Earthquakes
203(14)
10.4.1 Maximum Magnitude Mmax
204(7)
10.4.2 Attenuation of Earthquake Intensity with Distance for Volcanic Earthquakes
211(2)
10.4.3 Recurrence Time
213(2)
10.4.4 Estimation of the Seismic Hazard of Volcanic Activity of Volcan de Colima, Mexico
215(2)
11 Origin of Eruption Earthquakes
217(20)
11.1 Volcanic Processes Generating Seismic Signals of Eruption Earthquakes
217(2)
11.1.1 Processes Within the Volcanic Conduit
217(1)
11.1.2 Volcanic Flows
217(2)
11.2 Source Mechanisms of Eruption Earthquakes
219(5)
11.2.1 A Force System Equivalent to a Volcanic Eruption
219(3)
11.2.2 Seismic Moment Tensors of Some Non-Double-Couple Sources of Eruption Earthquakes
222(2)
11.3 Models of the Eruption Earthquake Sources
224(13)
11.3.1 Models Based on the Vibration of Magma-Filled Structures
224(4)
11.3.2 Models Based on Degassing Process of Magma
228(7)
11.3.3 Modeling of Seismic Signals Generated by Pyroclastic Flows and Rockfalls
235(2)
12 Volcanic Tremor
237(24)
12.1 Seismograms and Spectra
237(1)
12.2 Location of Volcanic Tremor
237(1)
12.2.1 Oshima Volcano, Izu Islands
237(1)
12.2.2 Etna Volcano, Sicily
238(1)
12.3 Volcanic Tremors in Eruptive Process
238(6)
12.3.1 Etna Volcano, Sicily
239(1)
12.3.2 Pavlof Volcano, Alaska
240(1)
12.3.3 Kilauea Volcano, Hawaii
241(1)
12.3.4 Klyuchevskoy Volcano, Kamchatka
242(2)
12.4 Relationship Between the Intensity of Volcanic Tremor and Volcanic Events
244(2)
12.5 Special Cases of Volcanic Tremors
246(15)
12.5.1 Isolated Tremors
246(6)
12.5.2 Banded Tremor
252(4)
12.5.3 Long-Period Tremor
256(2)
12.5.4 Deep Tremor
258(3)
13 Seismic Signals Associated with Pyroclastic Flows, Rockfalls, and Lahars
261(34)
13.1 Occurrence of Pyroclastic Flows, Rockfalls, and Lahars During Volcanic Eruptions
261(1)
13.2 Seismic Signals Associated with Pyroclastic Flows and Rockfalls: Waveforms and Spectra
261(12)
13.2.1 Seismic Signals of Pyroclastic Flows Produced by the Partial Collapse of Lava Dome
263(2)
13.2.2 Seismic Signals of Pyroclastic Flows Produced by the Collapse of Eruption Column
265(2)
13.2.3 Seismic Signals of Pyroclastic Flows Produced by the Explosive Destruction of Growing Lava Dome
267(3)
13.2.4 Seismic Signals Produced by Rockfall
270(2)
13.2.5 Spectral Characteristics
272(1)
13.3 Occurrences of Earthquakes Associated with Pyroclastic Flows and Rockfalls
273(1)
13.4 Relationship Between the Pyroclastic Flow and Rockfall Earthquakes and Seismo-Volcanic Activity During Lava Emission
273(3)
13.5 Quantification of Pyroclastic Flow and Rockfall Earthquakes
276(6)
13.5.1 Quantification of Pyroclastic Flow and Rockfall Earthquakes Occurring Due to Partial Collapse of the Lava Dome and Recorded by Short-Period Instruments at Volcan de Colima, Mexico
278(2)
13.5.2 Relationship Between the Magnitude of Pyroclastic Flow and Rockfall Earthquakes and the Volume of Pyroclastic Flows
280(1)
13.5.3 Relationship Between the Amplitude of Long-Period Records of Pyroclastic Flow and Rockfall Earthquakes and the Volume of Pyroclastic Flows
281(1)
13.6 Location Pyroclastic Flows Using the Amplitude Signals of Earthquakes
282(1)
13.7 Seismic Signals Associated with Lahars: Waveforms and Spectra
282(5)
13.8 Seismic Signals as a Source of Information About the Lahar Structure
287(3)
13.9 Seismic Tracking of Lahars
290(2)
13.10 Comparison of the Seismic Characteristics of Pyroclastic Flows and Lahars
292(3)
14 Seismic Signals Associated with Volcanic Explosions
295(32)
14.1 Waveforms and Spectra
296(3)
14.1.1 Strombolian Explosions
296(1)
14.1.2 Vulcanian Explosions
297(1)
14.1.3 Phreato-Magmatic Explosions
297(2)
14.2 Nature of the Seismic Signals of Explosive Earthquakes
299(6)
14.2.1 Comparison of the Contemporary Video and Seismic Records During an Explosion
299(3)
14.2.2 Type of Waves Composing the Seismic Signal of an Explosion
302(3)
14.3 Sources of Explosion Earthquakes and Their Quantification
305(13)
14.3.1 Multiple Source of Explosions
307(4)
14.3.2 Two-Stage Model of Explosive Process
311(3)
14.3.3 Relationship Between the Seismic Moment of Preliminary LP Phase and the Energy of Explosions for Sakurajima Volcano
314(4)
14.3.4 Volcanic Explosive Process as a Source of Hybrid Earthquakes
318(1)
14.4 Location of Explosion Earthquakes
318(1)
14.4.1 Location of the Initial Sub-Events from Waveform Inversion
318(1)
14.5 Explosion Sequences
319(3)
14.6 Explosion Earthquakes in Eruptive Process
322(5)
15 Long-Period and Very Long-Period Seismic Signals at Volcanoes
327(28)
15.1 Waveforms and Spectra
327(10)
15.1.1 Long-Period Seismic Signals
327(1)
15.1.2 Very Long-Period Seismic Signals
328(3)
15.1.3 Occurrences of LP and VLP Events
331(3)
15.1.4 Nature of LP and VLP Seismic Signals
334(3)
15.2 Geometry of the Sources of LP and VLP Seismic Signals
337(2)
15.3 Type of Fluid Within the Fluid-Filled Cracks
339(8)
15.3.1 Crack Model
340(1)
15.3.2 Complex Frequencies of the LP Seismic Signal for Different Fluids
341(1)
15.3.3 Identification of the Type of Fluid from LP Seismic Signals
341(6)
15.4 Location of the Sources of LP and VLP Events
347(4)
15.5 Conceptual Models of the Relationship Between the Sources of the LP and VLP Seismic Signals and Their Role in Eruptive Process
351(4)
16 Swarms of Microearthquakes Associated with Effusive and Explosive Activity at Volcanoes
355(26)
16.1 Waveforms and Spectra
355(2)
16.2 Structure of Microearthquake Swarms
357(5)
16.3 Microearthquake Swarms in Eruption Process
362(9)
16.3.1 Kizimen volcano, Kamchatka
362(2)
16.3.2 Stromboli volcano, Aeolean Islands
364(2)
16.3.3 Mount St. Helens, Cascades
366(1)
16.3.4 Ubinas volcano, Peru
367(1)
16.3.5 Volcan de Colima, Mexico
368(3)
16.4 Nature of Microearthquakes
371(10)
16.4.1 Similarity Between the Microearthquake Waveforms and the Seismic Signals Well-Associated with the Volcanic Events
371(4)
16.4.2 Quantification of Microearthquakes
375(5)
16.4.3 Nature of Microearthquakes Resolved from Waveform Inversion
380(1)
17 Acoustic Waves Generated by Volcanic Eruptions
381(26)
17.1 Infrasonic Acoustic Waves from Small Volcanic Explosions (VEI 1 and 2)
381(9)
17.1.1 Waveforms and Spectra
382(1)
17.1.2 Families of Infrasonic Signals
383(1)
17.1.3 Source Location of the Infrasonic Events
383(3)
17.1.4 Relationship Between the Amplitudes of the Seismic and Infrasonic Signals
386(4)
17.2 Long-Period Acoustic and Acoustic-Gravity Waves from Large Volcanic Explosions (VEI 4--6)
390(3)
17.2.1 Near-Field Waveforms of the Long-Period Acoustic Waves
390(1)
17.2.2 Far-Field Registrations of the Long-Period Acoustic Waves
391(2)
17.3 Acoustic Waves Produced by the Lava Dome Collapse and the Propagation of Pyroclastic Flow and Rockfalls
393(6)
17.3.1 Dome Collapse
393(2)
17.3.2 Pyroclastic Flow Propagation
395(3)
17.3.3 Large Rockfall Propagation
398(1)
17.4 Acoustic Waves Produced During Volcanic Microearthquake Swarms ("Drumbeats")
399(2)
17.5 Utility of the Acoustic Signals for Volcano Activity Monitoring
401(6)
17.5.1 Estimation of the Energy of Eruptive Events
401(2)
17.5.2 Reconstruction of the Process of Dome Collapses and Pyroclastic Flow Movement
403(2)
17.5.3 Monitoring of Phreatic and Strombolian Explosions
405(2)
18 Seismic Monitoring of Volcanic Activity and Forecasting of Volcanic Eruptions
407(26)
18.1 Methodology of Seismic Monitoring of Volcanic Activity
407(9)
18.1.1 Seismic Networks Around Volcanoes
407(3)
18.1.2 Initial Processing of Seismic Data
410(2)
18.1.3 Automatic Classification of the Seismic Signals
412(4)
18.1.4 Location of Seismic Events
416(1)
18.2 Applications of Volcanic Seismicity to the Forecasting of Volcanic Eruptions and Predicting of Volcanic Hazards
416(17)
18.2.1 Methods Based on the Statistical Variations in the Parameters of Volcano-Tectonic Earthquakes
417(7)
18.2.2 Chronicle of Some Forecasting of Volcanic Eruptions Based on Seismic Monitoring
424(9)
19 Seismic Activity at Dormant Volcanic Structures: A Problem of Failed Eruption
433
19.1 Failed Eruptions: Case Studies
433(12)
19.1.1 Failed Eruptions at Large Calderas
433(4)
19.1.2 Failed Eruptions at Strato-Volcanoes
437(3)
19.1.3 Failed Eruptions in Rift Settings
440(5)
19.2 Modeling of Magma Ascent Resisting
445(6)
19.2.1 Experimental Study of the Ascent of a Fixed Magma Volume
446(1)
19.2.2 Arrest of Propagating Dyke Due to Mechanical Barriers and Density Stratification in an Upper Crustal Horizon
447(4)
19.3 Monitoring of the Seismic Activity at Dormant Volcanoes
451
19.3.1 Monitoring of Andesitic and Dacitic Dormant Volcanoes
452(1)
19.3.2 Monitoring of Basaltic Dormant Volcanoes
453(4)
References
457
Prof. Vyacheslav Zobin graduated from the Novosibirsk State University, Novosibirsk, Russia, in 1966, and obtained his PhD in Physics and Mathematics (Volcanic Seismology) at the Institute of Physics of the Earth, Moscow, Russia, in 1978. From 1966 to 1996 he worked at the Institute of Volcanology, Petropavlovsk-Kamchatsky, Russia, and has since worked as Research Professor at the Center for Volcanological Research, Colima University, Colima, Mexico. Prof. Zobin is a prolific author in the areas of volcanic seismology and seismic hazard, with many published research articles, and with books published in three languages: Russian, Spanish, and English.