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  • ―白木微小地震観測所テレメータ観測網による―
    浅野 周三, 三浦 勝美, 井上 義弘, 三浦 礼子, 石桁 征夫, 吉井 敏尅
    地震 第2輯
    1986年 39 巻 2 号 229-240
    発行日: 1986/06/25
    公開日: 2010/03/11
    ジャーナル フリー
    Recently the telemetering seismic network of Shiraki Micro-Earthquake Observatory, Earthquake Research Institute, University of Tokyo, has been constructed in Chugoku District and its vicinity, Western Japan by the fourth stage of National Earthquake Prediction Project. There are seven seismic observation sites in the network, three of which are linked by the telephone lines and four of which, newly installed, are linked by radio to Shiraki Micro-Earthquake Observatory. The latter four are located in the southern part of the network. Thus, the accuracy of hypocenter determination has been improved, especially in the southern part. According to hypocenter determination based on the revised Ichikawa-Mochizuki travel-time table, the following features of the seismic activity in the period from July, 1983 to October, 1984 were obtained:
    1. In the land area of Chugoku District, earthquakes occurred in the upper part of the crust.
    2. In the southern region of 34°N latitude line, most of earthquakes took place in the upper mantle. An east-west cross section of hypocenters clearly shows a simple Wadati-Benioff seismic zone with a thickness of about 20km, but a north-south cross section of hypocenters shows complicated seismic zones, possibly more than two. The dip of the seismic zone west of 132°E is a little larger than that east of 132°E in the east-west cross section.
    Furthermore, detailed description is given to main events during the period from July, 1983 to October, 1984, such as earthquakes M6.8 and M5.2 on August 26, 1983 and June 25, 1984, respectively.
  • 糖尿病療養指導における,理学療法士の役割
    伊藤 隆弘, 山田 礼子, 千葉 ゆか, 三浦 礼子, 戸田 いく子, 加納 伸介
    理学療法学Supplement
    2016年 2015 巻 P-DM-03-2
    発行日: 2016年
    公開日: 2016/04/28
    会議録・要旨集 フリー
    【はじめに,目的】糖尿病療養指導において,評価・治療は専門性を増してきており,各職種が専門性を生かしつつ密接な連携を保つチームアプローチが必要となっている。A病院では平成24年度より多職種による糖尿病サポートチーム活動を開始,平成27年度にはチーム内に日本糖尿病療養指導士6名,糖尿病認定看護師1名となったが,常勤の糖尿病専門医は不在である。その中で今回,2型糖尿病(ペットボトル症候群)・緩徐進行型1型糖尿病疑いにより16日間の教育入院となったA氏にチームアプローチを行い,その有効性と今後の課題について検討したので報告する。【方法】30代男性,身長172.4cm,体重119.3kg,BMI 40.1,仕事は軽作業。口渇・多飲を認め近医受診,A病院紹介入院。入院時,随時血糖値350mg/dl,HbA1c15.2%。主治医より病状と治療方針の説明後,糖尿病認定看護師より全般的な療養指導と心理的ケアを中心とした面談を実施。管理栄養士より,A氏・家族に栄養指導を実施。薬剤師より,インスリン・内服薬について説明。病棟看護師より,インスリン自己注射・自己血糖測定(以下SMBG,mg/dl)技術を指導。理学療法士より,運動療法とともに,入院前生活を考慮した自主練習指導を実施。運動療法実施に際して,実施内容を他職種に伝達,運動後にSMBGを行い低血糖の予防と運動効果の自己認識を促した。情報共有方法は,カルテ・口頭での伝達とともに,必要時チームカンファレンスを実施。【結果】入院15日目,SMBGは100~152。入院期間中,食事・運動・薬物各療法について一定の理解がなされ,自主的に食事を撮影する,散歩をする等,療養意欲の向上が認められた。退院97日後,SMBGは90~120,随時血糖値125mg/dl・HbA1c6.0%,体重123kg。食事・運動・薬物各療法のコンプライアンスは低下したが自己認識しており,飲料は無糖の物を選択,仕事は立ち仕事を率先して行っている等,ある程度の療養意欲は認められた。【結論】チーム活動前に比べ,各職種が担当する療養指導内容の相互理解が深まり,療養指導項目が細分化されるとともに補完が図られた。また,カルテ・口頭での伝達,チームカンファレンスによる情報共有により,治療・療養指導方針の統一が図られ,的確な療養指導が可能となった。入院時は経過に伴い血糖値は低下,運動療法効果も認識し,また退院後の各値も良好であり,一定の治療・療養指導は図られたと考えられる。しかし,入院時に比しコンプライアンスは低下,体重も増加しており,自己認識・療養意欲は確認されたが,退院後の実情に合わせた療養指導が必要と考えられた。A病院は常勤の糖尿病専門医が不在であり,退院後の療養指導体制も確立されておらず,環境変化に合わせた十分な療養指導は行えていない。今回のチームアプローチの効果を基に,今後は各職種の役割と連携を確立するとともに,外来受診等に合わせた継続的な療養指導体制の構築が必要と考える。
  • 中岩 勝
    日本燃焼学会誌
    2008年 50 巻 153 号 235-241
    発行日: 2008年
    公開日: 2018/01/26
    ジャーナル フリー
  • 佃 為成, 三浦 勝美
    地震 第2輯
    2002年 55 巻 2 号 91-96
    発行日: 2002/10/31
    公開日: 2010/11/17
    ジャーナル フリー
    A viscoelastic bending moment theory is applied to the subducting slab of the Philippine Sea plate. The slab is steeply bent at the northern end of the Kyushu-Ryukyu subduction zone compared with at the southern part of the arc. The plate boundary on the cross section of the slab beneath Aki-Nada, Iyo-Nada and Bungo Channel, sea regions between Kyushu and Shikoku Islands, represents an arc of a circle, as demonstrated by the microearthquake distribution during over 10 years. The elastic bending moment is evaluated based on this geometry, where the deformation due to viscosity is reduced applying a Maxwell viscoelastic theory. The bending is too large in strength to ascribe it only to the force of negative buoyancy of the slab. We here assume the horizontal pressure generated by the spreading mantle flow accompanying upwelling magmas at the volcanic area in northern Kyushu, where extensive ground movements have been detected by geodetic measurements. The exerted uniform pressure to bend the slab is estimated to amount to (σ=) 72 MPa, when we take the following model constants as standards : the thickness of the slab h = 30 km, Young modulus of the slab (E=) 1.8 x 105 MPa, Poisson's ratio (ν=) 0.27, an average elapsed time since the subduction of the slab initiated (t=) 1.9 × 106 y, the time constant of the viscoelastic slab (τ=) 3.0 × 105y, and the excess density of the slab compared with the surrounding athenosphere (Δρ=) 0.06 × 103 kg/m3. The region of the highest seismic activity is located at the vicinity of the upper locked portion of the plate, where destructive earthquakes have frequently occurred. The 2001 Geiyo earthquake of M6.4 was one of them and took place at the eastern end of this active seismic zone. The focal mechanism of the event shows normal faulting as similarly as those of the majority of small earthquakes in the seismic active region. The main cause of this large earthquake is considered to be the bending force of the plate.
  • 高橋 直季, 平松 良浩, 古本 宗充, 三宅 学, 平田 直
    地震 第2輯
    2003年 56 巻 1 号 89-94
    発行日: 2003/06/02
    公開日: 2010/03/11
    ジャーナル フリー
  • 纐纈 一起, 古村 孝志
    地震 第2輯
    2002年 55 巻 2 号 97-105
    発行日: 2002/10/31
    公開日: 2010/11/17
    ジャーナル フリー
    The significant attenuation of seismic motion in the west of the 2001 Geiyo earthquake is inferred from strong motion distributions, observed seismograms and their spectra. Since this attenuation is identified even in the distribution of borehole motions, that is assumed to arise in a deeper part like the mantle wedge. If we assume a low-Q zone in the mantle wedge, a strong motion simulation with Qs = 20-30 can reproduce the observations. This zone may be related to dehydration of the Philippine sea plate.
  • 蔵下 英司, 徳永 雅子, 平田 直, 岩崎 貴哉, 小平 秀一, 金田 義行, 伊藤 潔, 西田 良平, 木村 昌三, 井川 猛
    地震 第2輯
    2002年 54 巻 4 号 489-505
    発行日: 2002/04/25
    公開日: 2010/03/09
    ジャーナル フリー
    Large earthquakes occur along the Nankai trough, SW Japan, where the Philippine Sea plate is subducting beneath southwestern Japan arc. To understand tectonics related to the occurrence of these large earthquakes, we need to elucidate crustal and upper mantle structures of the subducting Philippine Sea plate and the overlying southwestern Japan arc. In the summer of 1999, we conducted a highly dense onshore-offshore integrated seismic experiment in the eastern part of Shikoku Island and the adjacent Nankai trough, SW Japan. Controlled seismic signals both from land explosives and air-gun sources were recorded by the land seismic stations. We obtained high signal-to-noise ratio data along the entire length of the land profile.
    Analyzing these explosive and air-gun data recorded by the land seismic stations, we could obtain a detailed geometry of the subducting Philippine Sea plate and the crustal and upper mantle structure beneath eastern Shikoku Island. The signals from the air-gun source are especially useful to reveal a structure of an ocean-continental transition zone, which is not obtained using only land explosive data. The uppermost crust beneath eastern Shikoku Island is covered with a surface layer with velocities of 4.0-5.0km/s. The surface velocity shows a remarkable lateral change at the geological boundary between granitic rocks and an accretionary belt. The velocity of the uppermost crust is obtained as 5.7km/s. The island arc Moho is about 33km deep beneath northeastern Shikoku Island and the crustal thickness seems to thin toward the north. Beneath the southern edge of the land profile, the top of the subducting Philippine Sea plate is located at a depth of about 18km with a dip angle of approximately 12 degrees. The subduction angle steepens beneath this point. The top of the subducting plate can be traced to a depth of about 30km, almost parallel to the Wadati-Benioff seismic plane. This subduction angle is shallower than that beneath the Kii peninsula. Hypocenter distribution associated with the underthrusting of the Philippine Sea plate beneath eastern Shikoku Island is located beneath the subducting oceanic Moho. The seismicity underlies a contact zone between the nreanic and island-arc crusts.
  • 堀井 幸江, 桑名 篤, 八戸 真弓, 草塲 新之助
    RADIOISOTOPES
    2021年 70 巻 1 号 19-27
    発行日: 2021/01/15
    公開日: 2021/01/15
    ジャーナル オープンアクセス

    カキ果実の放射性物質による汚染状況を把握するため,複数のカキ圃場で土壌及び果実の137Csならびに133Cs濃度を測定した。3年間調査した果実の137Cs濃度は低下する傾向の圃場が多く,移行係数については,年度間に有意な差はみられなかった。事故後5~7年が経過した時点では,地上部汚染の影響が低下しており,土壌から果実へのセシウムの移行も限定的であると考えられた。土壌の133Cs濃度は各圃場とも同程度であったが,果実の133Cs濃度が他の圃場と比較してより高い圃場があった。

  • 木村 昌三, 岡野 健之助
    地震 第2輯
    1994年 47 巻 1 号 11-19
    発行日: 1994/06/14
    公開日: 2010/03/11
    ジャーナル フリー
    The seismic activity in Shikoku is characterized by two different focal depth ranges. One of the ranges is in the upper crust and another one in the uppermost mantle to about 40km depth. This study examines the seismic activity in the latter region. We reveal that the thickness of the focal distribution of these earthquakes is at most 5km by improving of hypocenter determination. Such a thin focal distribution suggests that the generation of these mantle earthquakes is not due to descending of the oceanic plate, but is more easily comprehensible as a boundary phenomenon between the continental and the oceanic basements.
    The other focal distribution which appears to descend under Kyushu nearly to the west is observed in the region west to Shikoku. This study shows a possibility that these two focal distributions are not directly related with each other and that the generation of these mantle earthquakes in Shikoku is restricted by the Median Tectonic Line.
  • 好野 奈美子, 小林 浩幸, 内田 智子, 島崎 由美
    雑草研究
    2009年 54 巻 3 号 139-146
    発行日: 2009年
    公開日: 2009/10/03
    ジャーナル フリー
    ダイズ栽培にリビングマルチとして用いるムギ類の抑草効果を検証するために,層別刈取法および日射量測定フィルムを用いて栽培圃場における垂直群落構造および受光量を調査した。リビングマルチとして用いたムギ類の乾物重は播種後約30日および約50日でダイズの2∼8倍になり,リビングマルチ区におけるムギ類とダイズのLAIの合計は播種後約30日で慣行区におけるダイズのLAIの9倍以上,約50日では慣行区の4倍以上になった。播種後約50日のリビングマルチ区では株元および条間で地表面の相対受光量がほぼ10%以下になったのに対して,慣行区ではダイズの株元であっても10%以下にならなかった。リビングマルチ区の雑草の乾物重は播種後約30日では慣行区の2分の1以下になった。リビングマルチ区のダイズの生育はリビングマルチのムギ類や,さらにダイズとムギ類の条間を狭くすることによって初期生育は抑制されるが、播種後50日ころには回復した。本研究により,リビングマルチは旺盛な初期生育により速やかに地表面の日射量を低下させ,初期生育の緩慢なダイズの被陰力を補って効率よく抑草できることが明らかになった。
  • 佐藤 隆司, 当舎 利行, 長 秋雄, 増田 幸治
    地震 第2輯
    1994年 46 巻 4 号 405-412
    発行日: 1994/03/14
    公開日: 2010/03/11
    ジャーナル フリー
    Although the Median Tectonic Line (MTL) fault system in Shikoku, southwest Japan, is one of the most active faults during the late Quaternary in Japan, the present-day seismicity along the MTL is not so remarkable. However microseismic activities have recently been reported in some regions along the MTL in Shikoku. It has been pointed out that these activities are those at segment boundaries of the MTL fault system. We carried out a temporal microseismic observation in one of these regions, the region around borders between Ehime, Kagawa and Tokushima prefectures, in order to determine the earthquake hypocenters precisely so that we can discuss the hypocenter distribution in context of the tectonics of the MTL. The seismometer network consisted of six observation points and had its areal extent of about 10km by 10km. Surface trace of the Ikeda fault goes through the network with its strike of N75°E. About 10km to the west of the network, there is a segment boundary of the MTL fault system which divides the Ikeda fault and the Ishiduchi fault. Hypocenters of 82 earthquakes are located during November 1990-August 1991. The seismic activity is high beneath the network, and no hypocenter is located near the segment boundary of the Ikeda and Ishiduchi faults. Most events located in the southern side of the MTL are in a depth range of 5-8km, and the distribution is almost flat or slightly inclines toward south from the MTL. The distribution pattern of the hypocenters in the northern side of the MTL is widely different from that in the southern side. The hypocenter depth increases with being away northward from the surface trace of the MTL. Although the number of events located is too few to conclude that the distribution is planar, the dip angle of about 50° is measured from a cross-sectional view on a vertical plane perpendicular to the strike of the MTL. The gap in the hypocenter distribution just beneath the MTL dipping almost vertically to the north, which has been reported by KIMURA and OKANO (1992) as an evidence that the MTL is near vertical, is not found in the present study.
  • XVI 秋田県玉川温泉における湯治概況ならびにCMIを主とした医学的調査
    平上 博資, 長岡 志郎, 青島 周明, 菅田 〓
    日本温泉気候物理医学会雑誌
    1967年 30 巻 3-4 号 73-86
    発行日: 1967/03/25
    公開日: 2010/08/06
    ジャーナル フリー
    The results obtained from a survey of balneal treatment and medical researches made mainly by means of the CMI card method at Tamagawa Spa in Akita Prefecture are summarized as follows;
    1) The spa visitors were about 540 in number, women being twice as many as men. Classified into age group, the number of visitors was almost equal in each group, and classified into occupations, farmers were the largest in number.
    2) The visitors came from nearly all parts of Japan, but the majority of them were from Akita Prefecture: 61.7%. Of all the visitors, 52.1% came either for treatment or for recuperation and 31.9% for recreation.
    3) This survey revealed that visitors without diseases were 47.9%. Of those who visited the consulting room, the patients with the circulatory diseases were the largest in number.
    4) The occurrence of bathing reaction was observed in 37.9%, and those with dermatitis were 21.2%.
    5) Those who drank hot-spring waters were 28.4%.
    6) The majority of visitors stayed for one or two weeks, bathing three to four times a day.
    7) Only 5.5% of visitors came there under doctor's directions, and 6.8%, of them came having information from newspaper or magazine articles. Most of the visitors came there based on their own experience or on others' recommendation.
    8) In the CMI, of 236 visitors, 67 were classified into the 1st group (28.4%), 88 into the 2nd group (37.3%), 56 into the 3rd group (23.7%), and 25 into the 4th group (10.6%). Of 108 controls, 45 were classified into 1st group (41.7%), 43 into the 2nd group (39.8%), 17 into the 3rd group (15.7%) and 3 into the 4th group (2.8%). Thus the 3rd and 4th group were quite large in number among the spa visitors. Very few of the visitors over 60 years of age belonged to the 3rd and 4th group. The number of men and women was almost equal in each group.
    9) Those who belonged to the 3rd and 4th group were found in the patients with circulatory diseases more than in those with other diseases.
    10) No relation seemed to exsist between the ratio of the body length to weight and CMI classification.
    11) Of the visitors, 62.4% had the systolic hypertension and 48.9% diastolic hypertension. No definite relation was observable between blood pressure and CMI classification.
    12) Of the visitors, studied by means of the CMI card method, 112 visitors were chosen at random for electrocardiograms, of whom 10 were classified into the abnormal group (8.9%), 38 into the semi-abnormal group (33.9%), and 64 into the normal group (57.2%). Incidence of the 3rd and 4th group was high in the abnormal electrocardiogram group.
    The incidence of the 3rd and 4th group is higher in the cases with sinus tachycardia, arrhythmia, abnormal p wave, bundle branch block and severe ST-T change than in the subjects with sinus bradycardia, prolonged P-Q interval, premature beat, left ventricular hypertrophy and slight ST-T change.
    13) CMI card method was useful for screening neurosis out of the mass.
  • 富澤 芳亜
    経済史研究
    2025年 28 巻 205-216
    発行日: 2025/01/31
    公開日: 2025/03/06
    ジャーナル フリー
  • 内田 智子, 小林 浩幸, 好野 奈美子
    日本作物学会紀事
    2011年 80 巻 3 号 277-283
    発行日: 2011年
    公開日: 2011/08/01
    ジャーナル フリー
    前作のオオムギを登熟期に刈り敷き,不耕起でダイズを栽培するオオムギカバークロップ―不耕起ダイズ栽培には増収効果が認められるが,養分的な効果がその要因であることが示唆されている.その一つとして,ダイズのアーバスキュラー菌根菌(以下AM菌)感染率向上によるリン吸収の促進が考えられる.AM菌による生育促進効果の報告は,生育初期についてのものがほとんどだが,本研究では子実生産と関係の深い着莢期以降のダイズの生育,AM菌感染率,収穫期のリン集積量および根粒重についてカバークロップ―ダイズ栽培1作目および3作目の二つの圃場で調査を行い,AM菌がダイズ収量に及ぼす影響を解析した.その結果,1作目圃場では,ダイズ収量は単作区に比較してカバークロップ区で高かったが,3作目圃場では,両区間の差異は明らかでなかった.カバークロップ区では,1作目,3作目圃場ともに着莢期のAM菌感染率は高かった.葉色値は1作目圃場では子実肥大期から成熟始期まで単作区より高い傾向がみられたが,3作目圃場では開花始期および成熟始期のみで高かった.根粒重はカバークロップ区で高い傾向が認められた.これらのことから1作目圃場のカバークロップ区では,着莢期までAM菌感染率が高く維持されたことによるリン吸収の促進と,AM菌感染率の向上による根粒菌着生期間の拡大に伴う窒素吸収の増加が増収に貢献したと判断された.一方,3作目圃場におけるカバークロップ区では窒素が制限要因となって増収効果がみられなかったものと考えられた.
  • 好野 奈美子, 小林 浩幸, 内田 智子, 島崎 由美, 敖 敏, 飛奈 宏幸
    日本作物学会紀事
    2012年 81 巻 1 号 18-26
    発行日: 2012年
    公開日: 2012/01/26
    ジャーナル フリー
    リビングマルチは環境保全や省力的な雑草防除として注目されているが,実用化や普及のためには事前にリビングマルチ−ダイズ栽培の適地および適期を判定することが重要である.そこで,リビングマルチの生育予測モデル作成のための基本的知見を得るため,リビングマルチとして用いるオオムギおよびコムギの現存量の推移を圃場試験と人工気象室を用いたポット試験によって調査し,現存量と気温,日射および日長の関係について解析した.圃場試験の結果,全品種とも播種時期が遅くなるほど最大乾物重は小さくなり,晩播では雑草防除に必要な生育量を得られなかった.また,いずれの播種期でもコムギ品種の方がオオムギ品種よりも生育が良好であり,一方,オオムギ品種の方がコムギ品種よりも早く枯死した.低温下におけるポット試験の結果,コムギだけでなくオオムギも収穫期までに枯死しなかった.次に,圃場試験およびポット試験を含めた栽培試験データを用いて,気温と日射によってどの程度までムギ類現存量を説明できるかを相関と重回帰分析で検証した.その結果,オオムギは気温によって生育に大きな影響を受けるため,得られる現存量を気温と日射量によって26~41%説明できることが明らかとなった.一方,コムギはオオムギに比べて気温と日射によって説明できる割合が小さく,推定精度を上げるためには土壌条件も検証する必要がある.
  • 江元 智子, 津村 紀子, 古屋 裕, 濃尾地震断層域合同地震観測グループ
    地震 第2輯
    2015年 68 巻 2 号 17-29
    発行日: 2015/07/10
    公開日: 2015/10/06
    ジャーナル フリー
    To determine crustal structure of the Neodani Fault zone, where the largest inland Nobi earthquake occurred in 1891, an active-source seismic experiment was carried out in the northern Mino region, central Japan. The shots were recorded by seismic array stations settled across the Neodani Fault Zone and we applied seismic reflection analysis to the data and obtained reflection profiles of the crust. Then we estimated crustal velocity by forward modeling using travel times of first break and reflected waves. We found significant reflections with duration of 2 s around 10 s two way travel time. Based on comparisons with other reflection profiles, we interpreted the events to come from the laminated lower crust within the overriding plate. The depth of the laminated crust varies across the Neodani Fault Zone, which is shallower in the southwest than in the northeast, implying that displacement along the Neodani faults extends to the deep crust. In the southwestern part of study area, the top of the Philippine Sea plate (PSP) estimated from travel time tomography is shallower than the lower limit of the laminated lower crust. We thus suggest that the subducting PSP may contact with the bottom of the overriding crust beneath the northern Mino district.
  • ―南海トラフから大和海盆北縁まで―
    伊藤 谷生, 佐藤 比呂志
    地学雑誌
    2010年 119 巻 2 号 235-244
    発行日: 2010/04/25
    公開日: 2010/07/06
    ジャーナル フリー
     The first attempt to make a crustal-scale cross-section of a trench-arc-backarc sea system has been successfully accomplished from the Nankai trough to the northern margin of the Yamato basin across Southwest Japan, using three seismic profiles: Nankai trough to Japan Sea coast (Ito et al., 2009), Oki trough (Tanaka and Ogusa, 1981), and Yamato basin (Sato et al., 2006). The section contains much new information that will be useful for research on the structural development of the Japanese island arc. The highlight of the information is the substantial difference in the structure between the Outer and the Inner zones. The Outer zone is constructed mainly by N-dipping accretionary complexes in its upper crust with a poorly developed lower crust. On the contrary, the Inner zone exhibits predominantly horizontal structures in its upper crust, beneath which thick horizontal lower crustal laminations occur as in the continental lower crust. Furthermore a 10-km-thick lens-shaped olivine-pyroxene cumulate body underlies the lower crust. The N-dipping Median Tectonic Line juxtaposes two substantially different zones from the upper to lower crusts
     The section, however, has the following serious defects caused by the poor specifications of the seismic profilings used here: (1) Shallow structures (<about several km) are poorly imaged, which makes it difficult to interpret geological structures. (2) Seismic images beneath the on-and-offshore zones of the Japan Sea coast are missing, which also makes it difficult to understand the rifting process associated with the opening of the Japan Sea. Thus, a new crustal-scale cross-section that is free from these defects is necessary. Fortunately, both the theory and the techniques of seismic profiling have advanced tremendously recently. This situation enables us to conduct seismic profiling along a long seismic line simultaneously on both land and sea (so-called “integrated land-and-sea seismic profiling”), and to provide a new section. The new section is expected to replace the former one soon.
  • 松崎 伸一, 大野 裕記, 池田 倫治, 福島 美光
    地震 第2輯
    2003年 56 巻 3 号 267-279
    発行日: 2003/12/25
    公開日: 2010/03/11
    ジャーナル フリー
    Using hypocentral data of JMA from 1997 to 2000, we determined upper surface shape of the Philippine Sea plate around Iyo-nada.
    The contour lines indicate that the Philippine Sea plate is spreading northward from Iyo-nada to Aki-nada in west Setonai-kai area. From 3-D bird's eye view, slight dent of the plate-upper surface, possibly due to buckling, can be seen at bound of the plate subducting around Iyo-nada area.
    It is considered that in addition to the plate bending, change of local tectonics from buckling to spreading may contribute to seismicity of the Iyo-nada area events. As well as this change may contribute to the source mechanism of small events and cyclic Geiyo earthquake.
  • 日本農村医学会雑誌
    1980年 29 巻 3 号 178-201,316
    発行日: 1980/08/15
    公開日: 2011/08/11
    ジャーナル フリー
  • 長谷川 昭
    地震 第2輯
    1991年 44 巻 Supplement 号 329-340
    発行日: 1991/07/24
    公開日: 2010/03/11
    ジャーナル フリー
    Recently, telemetered microearthquake observation networks have been developed, and data acquisition and processing procedures have been automated in many networks, including automatic hypocenter determinations by using computers. As a result the detection capability and the accuracy of hypocenter determination of microearthquakes have been tremendously improved, which made a great advance in detailed microearthquake studies. We present a brief review on recent studies of seismicity based on microearthquake observations, focusing on spatial and temporal distributions of microearthquakes and their related problems.
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