1997年鹿児島県北西部地震余震域内の基盤から土壌までを切る断層の露頭

In 1997, two strong earthquakes occurred on March 26 (Mj6.6) and May 13 (Mj6.4) in the northwestern part of Kagoshima Prefecture, Japan (termed the 1997 Northwestern Kagoshima Earthquakes). However no seismogenic faults associated with these earthquakes had previously been recognized at the surface....

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Published inChishitsugaku zasshi Vol. 124; no. 5; pp. 361 - 366
Main Authors 関根, 秀太郎, 笠原, 敬司, 林, 広樹, 内田, 嗣人, 武田, 哲也, 吉崎, 那都, 向吉, 秀樹, 後藤, 和彦
Format Journal Article
LanguageJapanese
Published Tokyo 一般社団法人 日本地質学会 15.05.2018
Japan Science and Technology Agency
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ISSN0016-7630
1349-9963
DOI10.5575/geosoc.2018.0006

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Abstract In 1997, two strong earthquakes occurred on March 26 (Mj6.6) and May 13 (Mj6.4) in the northwestern part of Kagoshima Prefecture, Japan (termed the 1997 Northwestern Kagoshima Earthquakes). However no seismogenic faults associated with these earthquakes had previously been recognized at the surface. In this study, we report structural observations from newly recognized fault outcrops located 1.5 and 2 km southwest of the epicenter of the Mj6.6 earthquake. One outcrop consists of the Miocene Shibi-san Granodiorite, which is unconformably overlain by lower sandy loam, lower humic soil, upper sandy loam, and upper humic soil layers that are clearly offset by steeply dipping faults. We measured ~ 40 cm of vertical separation of the contact between the lower sandy loam and lower humic soil layers along a WNW-trending fault, above which the ground surface flexed upward by about 20 cm. The second outcrop is a streambed exposure of the Shibi-san Granodiorite that shows a 30-cm-thick layer of foliated cataclasite along a fault plane, with textural evidence of sinistral slip.
AbstractList In 1997, two strong earthquakes occurred on March 26 (Mj6.6) and May 13 (Mj6.4) in the northwestern part of Kagoshima Prefecture, Japan (termed the 1997 Northwestern Kagoshima Earthquakes). However no seismogenic faults associated with these earthquakes had previously been recognized at the surface. In this study, we report structural observations from newly recognized fault outcrops located 1.5 and 2 km southwest of the epicenter of the Mj6.6 earthquake. One outcrop consists of the Miocene Shibi-san Granodiorite, which is unconformably overlain by lower sandy loam, lower humic soil, upper sandy loam, and upper humic soil layers that are clearly offset by steeply dipping faults. We measured ~ 40 cm of vertical separation of the contact between the lower sandy loam and lower humic soil layers along a WNW-trending fault, above which the ground surface flexed upward by about 20 cm. The second outcrop is a streambed exposure of the Shibi-san Granodiorite that shows a 30-cm-thick layer of foliated cataclasite along a fault plane, with textural evidence of sinistral slip.
Author 笠原, 敬司
武田, 哲也
林, 広樹
内田, 嗣人
吉崎, 那都
向吉, 秀樹
関根, 秀太郎
後藤, 和彦
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References Miyamachi, H., Iwakiri, K., Yakiwara, H., Goto, K. and Kakuta, T., 1999, Fine structure of aftershock distribution of the 1997 Northwestern Kagoshima Earthquakes with a three-dimensional velocity model. Earth Planets Space, 51, 233–246.
大庭 昇(Oba, N.), 1957, 鹿児島県北西部の紫尾花崗閃緑岩および捕獲岩類(Shibi granodiorite and xenoliths in the north-western part of Kagoshima Prefecture).鹿児島大理科報告(Sci. Rep. Kagoshima Univ.), 6, 83–98.
[URL1]災科学技術研究所(National Research Institute for Earth Science and Disaster Resilience), 地震ハザードステーション(Japan Seismic Hazard Information) J-SHIS Map, http://www.j-shis.bosai.go.jp//map
Takeda, T., Kasahara, K., Hayashi, H., Abe, S. and Goto, K., 2015, Relationship between crustal structure and source fault of 1997 Kagoshima Earthquake(M6.6), Japan, based on relocated hypocenters and seismic reflection data. 48th Annu. Fall Meet. Amer. Geophys. Union, S11A-2779.
Wessel, P. and Smith, W. H. F., 1998, New, improved version of the Generic Mapping Tools released. EOS Trans. AGU, 79, 579.
九州活断層研究会(Research Group for Active Faults of Kyushu), 1997, 鹿児島北西部地震被害調査報告書(Disaster Report of the 1997 Northwestern Kyushu Earthquake) .53p
鹿児島大学理学部(Faculty of Science, Kagoshima University), 1997, 1997年3月26日と5月13日に鹿児島県北西部で発生した地震(M6.5, M6.2)(The earthquakes with M6.3(March 26, 1997) and with M6.2(May 13, 1997) occurred in Northwestern Kagoshima Prefecture).予知連会報(Rep. CCEP), 58, 630–637
Murata, A., 1987, Hokusatsu Bend and clockwise rotation of the Southwest Japan Arc. Jour. Fac. Sci., Univ. Tokyo, 21, 333–349.
活断層研究会編(The Research Group for Active Faults, ed.), 1991, 新編日本の活断層-分布図と資料(Active Faults in Japan, New Edition: Distribution Maps and Related Materials).東京大学出版会(Univ. Tokyo Press), 437p
村上真幸・藤原 智・飛田幹男・新田 浩・中川弘之・小沢慎三郎・矢来博司(Murakami, M., Fujiwara, S., Tobita, M., Nitta, K., Nakagawa, H., Ozawa, S. and Yarai, H.), 1997, 国土地理院における干渉SARによる地殻変動検出技術の進展(Progress in SAR Interferometry for the Detection of Crustal Deformation by the Ceographical Survey Institute).地理院時報(Jour. GSI), 88, 1–9
町田 洋・新井房夫(Machida, H. and Arai, F., eds.), 2003, 新編 火山灰アトラス:日本列島とその周辺(Atlas of Tephra in and around Japan: revised edition).東京大学出版会(Univ. Tokyo Press), 336 p
国土地理院(Geographical Survey Institute Japan), 1998, 九州・沖縄地方の地殻変動(Crustal Movements in the Kyushu and Okinawa Districts).予知連会報(Rep. CCEP), 59, 592–610
宮町宏樹・岩切一宏・津野拓士・清水 力・福満修一郎・金子和弘……清水 洋(Miyamachi, H., Iwakiri, K., Tsuno, T., Shimizu, C., Fukumitsu, S., Kaneko, K.,…, Shimizu, H.), 1998, 1997年鹿児島県北西部地震の臨時余震観測(Temporary Seismic Observation of Aftershocks for the 1997 Northwestern Earthquakes in Kagoshima Prefecture).北海道大地球物理学研報(Geophys. Bull. Hokkaido Univ.), 61, 85–97
村田明広(Murata, A.), 1999, 北薩屈曲と鹿児島県北西部地震(1997年3月26日, 5月13日)(Hokusatsu Bend and Kagoshima-ken Hokuseibu Earthquakes of March 26 and May 13, 1997).構造地質(Jour. Tectonic Res. Group Japan), 43, 93–97.
井村隆介・岩松 暉・隈元幸司(Imura, R., Iwamatsu, A. and Kumamoto, K.), 1997, 1997年3-5月に発生した鹿児島県北西部の地震被害(Disaster caused by the earthquake at northwestern Kagoshima Prefecture of March and May, 1997).鹿児島県地学会誌(Jour. Assoc. Earth Sci. Kagoshima), 76, 29–35. English translation from the original written in Japanese.
References_xml – reference: 活断層研究会編(The Research Group for Active Faults, ed.), 1991, 新編日本の活断層-分布図と資料(Active Faults in Japan, New Edition: Distribution Maps and Related Materials).東京大学出版会(Univ. Tokyo Press), 437p.
– reference: 九州活断層研究会(Research Group for Active Faults of Kyushu), 1997, 鹿児島北西部地震被害調査報告書(Disaster Report of the 1997 Northwestern Kyushu Earthquake) .53p.
– reference: 鹿児島大学理学部(Faculty of Science, Kagoshima University), 1997, 1997年3月26日と5月13日に鹿児島県北西部で発生した地震(M6.5, M6.2)(The earthquakes with M6.3(March 26, 1997) and with M6.2(May 13, 1997) occurred in Northwestern Kagoshima Prefecture).予知連会報(Rep. CCEP), 58, 630–637.
– reference: 村田明広(Murata, A.), 1999, 北薩屈曲と鹿児島県北西部地震(1997年3月26日, 5月13日)(Hokusatsu Bend and Kagoshima-ken Hokuseibu Earthquakes of March 26 and May 13, 1997).構造地質(Jour. Tectonic Res. Group Japan), 43, 93–97.
– reference: [URL1]災科学技術研究所(National Research Institute for Earth Science and Disaster Resilience), 地震ハザードステーション(Japan Seismic Hazard Information) J-SHIS Map, http://www.j-shis.bosai.go.jp//map/.
– reference: 村上真幸・藤原 智・飛田幹男・新田 浩・中川弘之・小沢慎三郎・矢来博司(Murakami, M., Fujiwara, S., Tobita, M., Nitta, K., Nakagawa, H., Ozawa, S. and Yarai, H.), 1997, 国土地理院における干渉SARによる地殻変動検出技術の進展(Progress in SAR Interferometry for the Detection of Crustal Deformation by the Ceographical Survey Institute).地理院時報(Jour. GSI), 88, 1–9.
– reference: 井村隆介・岩松 暉・隈元幸司(Imura, R., Iwamatsu, A. and Kumamoto, K.), 1997, 1997年3-5月に発生した鹿児島県北西部の地震被害(Disaster caused by the earthquake at northwestern Kagoshima Prefecture of March and May, 1997).鹿児島県地学会誌(Jour. Assoc. Earth Sci. Kagoshima), 76, 29–35. English translation from the original written in Japanese.
– reference: Murata, A., 1987, Hokusatsu Bend and clockwise rotation of the Southwest Japan Arc. Jour. Fac. Sci., Univ. Tokyo, 21, 333–349.
– reference: 国土地理院(Geographical Survey Institute Japan), 1998, 九州・沖縄地方の地殻変動(Crustal Movements in the Kyushu and Okinawa Districts).予知連会報(Rep. CCEP), 59, 592–610.
– reference: 大庭 昇(Oba, N.), 1957, 鹿児島県北西部の紫尾花崗閃緑岩および捕獲岩類(Shibi granodiorite and xenoliths in the north-western part of Kagoshima Prefecture).鹿児島大理科報告(Sci. Rep. Kagoshima Univ.), 6, 83–98.
– reference: 町田 洋・新井房夫(Machida, H. and Arai, F., eds.), 2003, 新編 火山灰アトラス:日本列島とその周辺(Atlas of Tephra in and around Japan: revised edition).東京大学出版会(Univ. Tokyo Press), 336 p.
– reference: Takeda, T., Kasahara, K., Hayashi, H., Abe, S. and Goto, K., 2015, Relationship between crustal structure and source fault of 1997 Kagoshima Earthquake(M6.6), Japan, based on relocated hypocenters and seismic reflection data. 48th Annu. Fall Meet. Amer. Geophys. Union, S11A-2779.
– reference: 宮町宏樹・岩切一宏・津野拓士・清水 力・福満修一郎・金子和弘……清水 洋(Miyamachi, H., Iwakiri, K., Tsuno, T., Shimizu, C., Fukumitsu, S., Kaneko, K.,…, Shimizu, H.), 1998, 1997年鹿児島県北西部地震の臨時余震観測(Temporary Seismic Observation of Aftershocks for the 1997 Northwestern Earthquakes in Kagoshima Prefecture).北海道大地球物理学研報(Geophys. Bull. Hokkaido Univ.), 61, 85–97.
– reference: Miyamachi, H., Iwakiri, K., Yakiwara, H., Goto, K. and Kakuta, T., 1999, Fine structure of aftershock distribution of the 1997 Northwestern Kagoshima Earthquakes with a three-dimensional velocity model. Earth Planets Space, 51, 233–246.
– reference: Wessel, P. and Smith, W. H. F., 1998, New, improved version of the Generic Mapping Tools released. EOS Trans. AGU, 79, 579.
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Snippet In 1997, two strong earthquakes occurred on March 26 (Mj6.6) and May 13 (Mj6.4) in the northwestern part of Kagoshima Prefecture, Japan (termed the 1997...
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SubjectTerms 1997 Northwestern Kagoshima Earthquake
active fault
Earthquakes
Fault lines
Faults
Loam
Miocene
Outcrops
Sandy loam
Seismic activity
Soil
Soil surfaces
Soils
Title 1997年鹿児島県北西部地震余震域内の基盤から土壌までを切る断層の露頭
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