東華大學圖書館 |

Language: English

Help

回圖書館首頁

手機版館藏查詢

Back

Switch To: Labeled | MARC Mode | ISBD

Linked to FindBook

Google Book

Amazon

博客來

Anomalous gas volcanism in the Black Sea

Record Type:	Electronic resources : Monograph/item
Title/Author:	Anomalous gas volcanism in the Black Sea/ by Evgeny Shnyukov, Vladimir Kobolev, Valentina Yanko.
Author:	Shnyukov, Evgeny.
other author:	Kobolev, Vladimir.
Published:	Cham :Springer Nature Switzerland : : 2025.,
Description:	xxix, 363 p. :ill. (some col.), digital ;24 cm.
[NT 15003449]:	Geological study of gas volcanism -- Study Area -- Materials and methods -- Types of gas manifestations at the bottom of the Black Sea -- Gas manifestations in the Crimean part of the Black Sea -- Gas manifestations within other parts of the Black Sea -- Gas volcanism and gas hydration on the Black Sea bottom -- Historical evidence of abnormal gas emissions from earthquakes -- Crimean earthquakes of 1927 -- Seismicity of the Azov-Black Sea region -- Mud volcano Golubitskiy as an example of the development of morphostructure under seismic influence -- On the nature of fiery phenomena in the Black Sea -- Interrelation of gas volcanism and biota in the Black Sea -- Conclusion.
Contained By:	Springer Nature eBook
Subject:	Volcanic gases - Black Sea. -
Online resource:	https://doi.org/10.1007/978-3-031-92758-4
ISBN:	9783031927584

Anomalous gas volcanism in the Black Sea
Shnyukov, Evgeny.

Anomalous gas volcanism in the Black Sea[electronic resource] /by Evgeny Shnyukov, Vladimir Kobolev, Valentina Yanko. - Cham :Springer Nature Switzerland :2025. - xxix, 363 p. :ill. (some col.), digital ;24 cm.

Geological study of gas volcanism -- Study Area -- Materials and methods -- Types of gas manifestations at the bottom of the Black Sea -- Gas manifestations in the Crimean part of the Black Sea -- Gas manifestations within other parts of the Black Sea -- Gas volcanism and gas hydration on the Black Sea bottom -- Historical evidence of abnormal gas emissions from earthquakes -- Crimean earthquakes of 1927 -- Seismicity of the Azov-Black Sea region -- Mud volcano Golubitskiy as an example of the development of morphostructure under seismic influence -- On the nature of fiery phenomena in the Black Sea -- Interrelation of gas volcanism and biota in the Black Sea -- Conclusion.

In the Black Sea, an unprecedented intensity of gas discharge of the seabed in the form of jet emissions (gas seeps, torches, flares) and fountains of gas emissions from mud volcanoes have been established, which are described in detail in the monograph. However, the main attention is paid to anomalous single-stage methane emissions as a result of the famous Yalta earthquakes of 1927, accompanied by amazing and mysterious fiery phenomena. An analysis of the available geological and geophysical materials indicates that the fire phenomena were caused by massive methane emissions as a result of a powerful mantle gas-fluid flow into decompaction zones of the crystalline basement along tectonic faults of various scales within the Odessa-Sinop and Circum-Black Sea fault zones. Earthquakes served as a trigger for the activation of tectonic disturbances in the near-bottom sedimentary horizons for the migration of focused deep gas-fluid flows. The deep structure of the source zones and the nature of the seismic process are analyzed, the nature of the manifestations of fire phenomena is assessed. The enormous volumes of gas emissions are noted - millions of cubic meters of methane, which are proposed as a kind of gas plume, the nature of which is associated with zones of deep faults in the upper mantle. Using the geological and geophysical materials obtained in recent years, the authors significantly refined the structural-tectonic construction and localization of gas-mud activity in the Black Sea water area. All these new materials, along with an analysis of the available data on the seismicity of the Crimean region, open up the possibility of explaining the fiery phenomena that were observed during the Yalta earthquakes of 1927 and facilitate the interpretation and understanding of their nature.

ISBN: 9783031927584

Standard No.: 10.1007/978-3-031-92758-4doiSubjects--Topical Terms:

3790645
Volcanic gases
--Black Sea.

LC Class. No.: QE527.75

Dewey Class. No.: 551.230916389

Anomalous gas volcanism in the Black Sea
LDR:03521nmm a2200325 a 4500 001 2414130
003 DE-He213
005 20250806165357.0
006 m d
007 cr nn 008maaau
008 260205s2025 sz s 0 eng d
020 $a 9783031927584 $q (electronic bk.)
020 $a 9783031927577 $q (paper)
024 7 $a 10.1007/978-3-031-92758-4 $2 doi
035 $a 978-3-031-92758-4
040 $a GP $c GP
041 0 $a eng
050 4 $a QE527.75
072 7 $a RNR $2 bicssc
072 7 $a NAT023000 $2 bisacsh
072 7 $a RNR $2 thema
082 0 4 $a 551.230916389 $2 23
090 $a QE527.75 $b .S558 2025
100 1 $a Shnyukov, Evgeny. $3 3449731
245 1 0 $a Anomalous gas volcanism in the Black Sea $h [electronic resource] / $c by Evgeny Shnyukov, Vladimir Kobolev, Valentina Yanko.
260 $a Cham : $b Springer Nature Switzerland : $b Imprint: Springer, $c 2025.
300 $a xxix, 363 p. : $b ill. (some col.), digital ; $c 24 cm.
505 0 $a Geological study of gas volcanism -- Study Area -- Materials and methods -- Types of gas manifestations at the bottom of the Black Sea -- Gas manifestations in the Crimean part of the Black Sea -- Gas manifestations within other parts of the Black Sea -- Gas volcanism and gas hydration on the Black Sea bottom -- Historical evidence of abnormal gas emissions from earthquakes -- Crimean earthquakes of 1927 -- Seismicity of the Azov-Black Sea region -- Mud volcano Golubitskiy as an example of the development of morphostructure under seismic influence -- On the nature of fiery phenomena in the Black Sea -- Interrelation of gas volcanism and biota in the Black Sea -- Conclusion.
520 $a In the Black Sea, an unprecedented intensity of gas discharge of the seabed in the form of jet emissions (gas seeps, torches, flares) and fountains of gas emissions from mud volcanoes have been established, which are described in detail in the monograph. However, the main attention is paid to anomalous single-stage methane emissions as a result of the famous Yalta earthquakes of 1927, accompanied by amazing and mysterious fiery phenomena. An analysis of the available geological and geophysical materials indicates that the fire phenomena were caused by massive methane emissions as a result of a powerful mantle gas-fluid flow into decompaction zones of the crystalline basement along tectonic faults of various scales within the Odessa-Sinop and Circum-Black Sea fault zones. Earthquakes served as a trigger for the activation of tectonic disturbances in the near-bottom sedimentary horizons for the migration of focused deep gas-fluid flows. The deep structure of the source zones and the nature of the seismic process are analyzed, the nature of the manifestations of fire phenomena is assessed. The enormous volumes of gas emissions are noted - millions of cubic meters of methane, which are proposed as a kind of gas plume, the nature of which is associated with zones of deep faults in the upper mantle. Using the geological and geophysical materials obtained in recent years, the authors significantly refined the structural-tectonic construction and localization of gas-mud activity in the Black Sea water area. All these new materials, along with an analysis of the available data on the seismicity of the Crimean region, open up the possibility of explaining the fiery phenomena that were observed during the Yalta earthquakes of 1927 and facilitate the interpretation and understanding of their nature.
650 0 $a Volcanic gases $z Black Sea. $3 3790645
650 0 $a Submarine volcanoes $z Black Sea. $3 3790646
650 1 4 $a Natural Hazards. $3 1005730
650 2 4 $a Geology. $3 516570
650 2 4 $a Paleontology. $3 518862
650 2 4 $a Geophysics. $3 535228
650 2 4 $a Earth Sciences. $3 642591
700 1 $a Kobolev, Vladimir. $3 3790644
700 1 $a Yanko, Valentina. $3 3605897
710 2 $a SpringerLink (Online service) $3 836513
773 0 $t Springer Nature eBook
856 4 0 $u https://doi.org/10.1007/978-3-031-92758-4
950 $a Earth and Environmental Science (SpringerNature-11646)