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表紙
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[OTHERS]
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まえがき
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目次
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I 現在の地殻変動
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Crustal deformationin central Kyusyu, Japan and its tectonic implication : Rifting and spreading of the Beppu-Shimabara Graben
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1-12
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Seismic activity in middle and western Kyushu
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13-18
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Seismic activity and tectonic significance near the volcanic areas in central Kyushu, Japan
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19-34
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II 地溝帯形成史・構造論
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Oita Plain and Beppu Bay : Subsurface structure and geological development around Beppu Bay
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35-42
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Displacement of the Chidiwa Fault since the last 6,000 years on the basis of the facies analysis of the core materials collected from the Karako Lowland in Nagasaki Prefecture, west Kyushu, Japan
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43-52
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Displacement of the depressed areas in the graben, estimated by the altitude of the inland sediments in central Kyushu, Japan
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53-72
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Neogene volcanic activity in central Kyushu in relation to zircon morphology
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73-82
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Pliocene and Quaternary volcanism in central Kyushu, Japan : Hohi Volcanic Zone vs. Shimabara Volcanic Zone
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83-91
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Geotectonic developing history in the Beppu-Kuju graben, central Kyushu, Japan
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93-106
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Tectonic history of the north-western area of "Kuju-Beppu Graben"
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107-127
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The Hohi volcanic zone as a volcano-tectonic depression and its formation tectonics : Three tectonic events caused by subduction of the Philippine Sea plate under the junction of the Southwest Japan Arc and the Ryukyu Arc
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129-148
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Is the Central Kyushu really rifting north to south?
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149-161
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Relationship between sedimentary basins on the shelf area in the East China Sea and the Central Kyushu Rift Valley
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163-173
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Conception of the Beppu-Shimabara graben, its development and problems
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175-192
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CONTENTS
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裏表紙
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CONTENTS
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