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電子書籍・電子雑誌EPS : Earth, Planets and Space
Volume number70
Complex mi...

Complex microseismic activity and depth-dependent stress field changes in Wakayama, southwestern Japan

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Complex microseismic activity and depth-dependent stress field changes in Wakayama, southwestern Japan

Call No. (NDL)
Z4-B128
Bibliographic ID of National Diet Library
11067477
Persistent ID (NDL)
info:ndljp/pid/11067477
Material type
記事
Author
Sumire Maedaほか
Publisher
Springer Nature
Publication date
2018-02-07
Material Format
Paper・Digital
Journal name
EPS : Earth, Planets and Space 70(21)
Publication Page
-
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We examined the spatial relationship between seismicity and upper crustal structure in the Wakayama region, northwestern Kii Peninsula, Japan, by inve...

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Digital

Material Type
記事
Author/Editor
Sumire Maeda
Toru Matsuzawa
Shinji Toda
Publication, Distribution, etc.
Publication Date
2018-02-07
Publication Date (W3CDTF)
2018-02-07
Periodical title
EPS : Earth, Planets and Space
No. or year of volume/issue
70(21)
Volume
70(21)
ISSN (Periodical Title)
1880-5981
ISSN-L (Periodical Title)
1343-8832
Text Language Code
eng
Persistent ID (NDL)
info:ndljp/pid/11067477
Collection (Materials For Handicapped People:1)
Collection (particular)
国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
Acquisition Basis
オンライン資料収集制度
Date Accepted (W3CDTF)
2018-04-12T16:47:48+09:00
Date Captured (W3CDTF)
2018-04-12
Format (IMT)
application/pdf
Access Restrictions
国立国会図書館内限定公開
Service for the Digitized Contents Transmission Service
図書館・個人送信対象外
Availability of remote photoduplication service
Periodical Title (Persistent ID (NDL))
info:ndljp/pid/11067456
Data Provider (Database)
国立国会図書館 : 国立国会図書館デジタルコレクション

Digital

Summary, etc.
We examined the spatial relationship between seismicity and upper crustal structure in the Wakayama region, northwestern Kii Peninsula, Japan, by investigating microearthquake focal mechanisms and the local stress field. The focal mechanisms of most events studied fall into three categories: (1) normal faulting with N–S-oriented T-axes mainly occurring at shallow depths, (2) reverse faulting with E–W-oriented P-axes dominating at intermediate depths, and (3) strike-slip faulting with N–S-oriented T-axes and E–W-oriented P-axes mainly seen at greater depths. The stress field varies with depth: the shallow part is characterized by a strike-slip-type stress regime with N–S tension and E–W compression, while the deep part is characterized by an E–W compressional stress regime consistent with reverse faulting. The depth-dependent stress regime can be explained by thermal stress caused by a heat source, as expected from geophysical observations. Geologic faults, acting as weak planes, might contribute to generate shallow normal fault-type and deeper strike-slip fault-type microearthquakes.
Access Restrictions
インターネット公開
Rights (production)
© The Author(s) 2018. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
Is Referenced By
Crustal dynamics: unified understanding of geodynamic processes at different time and length scales
The Wakayama earthquake swarm in Japan
Influence of crustal lithology and the thermal state on microseismicity in the Wakayama region, southern Honshu, Japan
Spatiotemporal variations in the stress field in the northeasternmost part of the NE Japan arc : constraints from microearthquakes
Causes of the N–S compressional aftershocks of the E–W compressional 2008 Iwate–Miyagi Nairiku earthquake (M7.2) in the northeastern Japan arc
References
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Changes in seismic activity following the 2011 Tohoku-oki earthquake: Effects of pore fluid pressure
Widespread distribution of ascending fluids transporting mantle helium in the fore-arc region and their upwelling processes: Noble gas and major element composition of deep groundwater in the Kii Peninsula, southwest Japan
Lateral variation of the cutoff depth of shallow earthquakes beneath the Japan Islands and its implications for seismogenesis
Changes in the stress field after the 2008 <i>M</i>7.2 Iwate‐Miyagi Nairiku earthquake in northeastern Japan
Determining changes in the state of stress associated with an earthquake via combined focal mechanism and moment tensor analysis: Application to the 2013 Awaji Island earthquake, Japan
New, improved version of generic mapping tools released
Triangle diagrams: ternary graphs to display similarity and diversity of earthquake focal mechanisms
Use of focal mechanisms to determine stress: A control study
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Non‐volcanic seismic swarms triggered by circulating fluids and pressure fluctuations above a solidified diorite intrusion
Spatial distribution of earthquakes in the Kii peninsula, Japan, south of the Median Tectonic Line
Intraslab seismicity and thermal stress in the subducted Cocos plate beneath central Mexico
Determination of stress from slip data: Faults and folds
The 3-D tectonic stress fields in and around Japan inverted from centroid moment tensor data of seismic events
Jurassic-Early cretaceous tectonic evolution of the Southern Chichibu terrane, southwest Japan
3He/4He ratios in well gases in the Kinki district, SW Japan: surface appearance of slab-derived fluids in a non-volcanic area in Kii Peninsula
Earthquake generating stresses in a descending slab
Aqueous fluids derived from a subducting slab: Observed high 3He emanation and conductive anomaly in a non-volcanic region, Kii Peninsula southwest Japan
Paragenesis of sodic pyroxene-bearing quartz schists: implications for the P-T history of the Sanbagawa belt
Seismic and geodetic evidence for the existence of hot materials beneath the Wakayama swarm activity, southwestern Japan
The youngest blueschist belt in SW Japan: implication for the exhumation of the Cretaceous Sanbagawa high‐<i>P/T</i> metamorphic belt
Crustal stress field in southern California and its implications for fault mechanics
Geographical distribution of <sup>3</sup>He/<sup>4</sup>He ratios in Japan: Implications for arc tectonics and incipient magmatism
近畿トライアングル周縁域の地震活動の相関とその地学的意義
紀伊半島西部の秩父帯・黒瀬川帯
Double-planed structure of intermediatedepth seismic zone and thermal stress in the descending plate.
Regional variations of the cutoff depth of seismicity in the crust and their relation to heat flow and large inland-earthquakes.
Geothermal gradient and heat flow data in and around Japan (I): apprasial of heat flow from geothermal gradient data
1996年8月11日宮城県鬼首付近に発生した地震について
Tomographic evidence for the mantle upwelling beneath southwestern Japan and its implications for arc magmatism
Seismic activity near the Moriyoshi-zan volcano in Akita Prefecture, northeastern Japan : implications for geofluid migration and a midcrustal geofluid reservoir
Outline of the 2011 off the Pacific coast of Tohoku Earthquake (Mw 9.0) : seismicity: foreshocks, mainshock, aftershocks, and induced activity
Non-volcanic seismic swarm and fluid transportation driven by subduction of the Philippine Sea slab beneath the Kii Peninsula, Japan
Data Provider (Database)
国立情報学研究所 : CiNii Research
Bibliographic ID (NDL)
11067477
NAID
120006517788
120006989892