Accretion Tectonics in the Circum-Pacific Regions

General.- Break-up and Accretion Tectonics.- North America to Northeast Asia.- Recognition, Character, and Analysis of Tectonostratigraphic Terranes in Western North America.- Tectonostratigraphic Terranes of Alaska and Northeastern USSR—A Record of Collision and Accretion.- Accretionary Terranes and Tectonic Evolution of Northeast Siberia.- Accretional and Collisional Eugeosynclinal Folded Systems of the Northwestern Pacific Rim.- Space-Time Distribution of Late Mesozoic to Early Cenozoic Magmatism in East Asia and Its Tectonic Implications.- Hokkaido, North Japan.- Collision Orogenesis and Sedimentation in Hokkaido, Japan.- Mesozoic Arc-Trench Systems in Hokkaido, Japan.- Collision Tectonics in Hokkaido and Sakhalin.- From Subduction to Paleosubductions in Northern Japan.- Disclosing of a Deepest Section of Continental-Type Crust Up-Thrust as the Final Event of Collision of Arcs in Hokkaido, North Japan.- Southwest Japan.- Hida and Mino: Tectonostratigraphic Terranes in Central Japan.- Accretion Tectonics Inferred from Paleomagnetic Measurements of Paleozoic and Mesozoic Rocks in Central Japan.- Accreted Oceanic Reef Complex in Southwest Japan.- Tectonic Environments and Crustal Section of the Outer Zone of Southwest Japan.- Accretionary Melange of Cretaceous Age in the Shimanto Belt in Japan.- Paleomagnetism of the Shimanto Belt in Shikoku, Southwest Japan.- Japan Cenozoic Ophiolite.- Mineoka Ophiolite Belt in the Izu Forearc Area—Neogene Accretion of Oceanic and Island Arc Assemblages on the Northeastern Corner of the Philippine Sea Plate.- Paleomagnetic and Geotectonic Investigation of Ophiolite Suites and Surrounding Rocks in South-Central Honshu, Japan.- Southwest to South Pacific.- A Possible Mechanism of Episodic Spreading of the Philippine Sea.- TertiaryAccretion of Ophiolite Seamounts, North Island, New Zealand.- Roles of Seamount, Rise, and Ridge in Lithospheric Subduction.- Geophysics and Metallogenesis.- Forces Acting on the Subducted Lithosphere Revealed by the Geometry of Deep-Seismic Zones.- Overthrust and Underthrust as a Fundamental Process of Continental Accretion.- Accretion Tectonics and Metallogenesis.