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Department Of Earth And Planetary Sciences Tokyo Institute Of Technology | 論文
- Rapid and simultaneous determination of multi-element abundances and U-Pb age for zircon crystal using UV laser ablation ICP-MS technique: critical evaluation of the technique with 91500 zircon standard
- 沖縄トラフと小笠原孤の電気伝導度構造
- A discovery of deformed oolite from metemorphic rocks of the Main Central Thrust zone in Western Nepal (特集:ヒマラヤ山脈とインド洋に記録された環境変動)
- Origin of high orbital eccentricity and inclination of asteroids
- Pacific-type orogeny revisited : Miyashiro-type orogeny proposed
- Petrology of peridotite xenoliths in alkali basalt (11Ma) from Boun, Korea: an insight into the upper mantle beneath the East Asian continental margin
- MAXI GSC Observations of a Spectral State Transition in the Black Hole Candidate XTE J1752-223
- 地震ダイナモ効果の観測 (地磁気永年変化,地震発生と電磁気シグナル)
- Subhorizontal boundary between ultrahigh-pressure and low-pressure metamorphic units in the Sulu-Tjube area of the Kokchetav Massif, Kazakhstan
- Kinematic analysis of ultrahigh-pressure-high-pressure metamorphic rocks in the Chaglinka-Kulet area of the Kokchetav Massif, Kazakhstan
- FLUOROKINOSHITALITE AND FLUOROTETRAFERRIPHLOGOPITE : NEW SPECIES OF FLUORO-MICA FROM BAYAN OBO, INNER MONGOLIA, CHINA
- Collisions between protoplanets: data analysis and classification
- Full waveform moment tensor inversion by reciprocal finite difference Green's function
- Inclusion-trail geometry of albite porphyroblasts in a fold structure in the Sambagawa Belt, central Shikoku, Japan
- Observational Possibility of the "Snow Line" on the Surface of Circumstellar Disks with the Scattered Light
- Superplume Project : Towards a new view of whole Earth dynamics
- 地球ダイナモのシミュレ-ション (特集 物理科学,この1年--1998年の物理科学ニュ-ス総まとめと,今後の展望)
- F. Krause and K. -H. Radler: Mean-Field Magnetohydrodynamics and Dynamo Theory, Pergamon Press, Oxford and New York, 271ページ, 21.5×15.5cm, 10,800円.
- 四国中央部高知市北方の黒瀬川メランジ帯〔英文〕
- Geochemistry of the oldest MORB and OIB in the Isua Supracrustal Belt, southern West Greenland : Implications for the composition and temperature of early Archean upper mantle
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