Quaternary Tephrochronology in Northeast Honshu, Japan
The volcanoes of Quaternary age in Northeast Honshu are distributed along two belts which are named the Nasu and Chokai Volcanic Belts. The Nasu Volcanic Belt is situated along the Backbone Ranges of Northeast Honshu and the Chokai in the Dewa Hilly Lands.
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The Omachi Tephra Formations and Tephrochronology
The tephras supplied from Late Quaternary volcanoes in Central Japan have been distinguished into some tephra regions. In this paper, the author has made the characterization, classification and tephrochronologic consideration of the Omachi Tephra formations, which are developed in the Omachi Tephra region.
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Early human impact on lake cyanobacteria revealed by a Holocene record of sedimentary ancient DNA. [PDF]
Nwosu EC +11 more
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INQUA tephrochronology bibliography”A call for references
Geoscientists conducting basic or applied research with pyroclastic materials may be interested in contributing references to relevant articles for inclusion in the first edition of the INQUA World Bibliography on Quaternary Tephrochronology.The total range of subject matter to be covered in the bibliography has not yet been set but may include ...
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Fast Holocene slip and localized strain along the Liquiñe-Ofqui strike-slip fault system, Chile. [PDF]
Astudillo-Sotomayor L +5 more
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Adaptation of the Endolithic Biome in Antarctic Volcanic Rocks. [PDF]
Hidalgo-Arias A +5 more
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Two-step movement of tsunami boulders unveiled by modified viscous remanent magnetization and radiocarbon dating. [PDF]
Sato T +8 more
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Deep-time paleogenomics and the limits of DNA survival. [PDF]
Dalén L +3 more
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Historical anthropogenic disturbances explain long-term moorland vegetation dynamics. [PDF]
Rowney FM +6 more
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Lake Ohrid's tephrochronological dataset reveals 1.36 Ma of Mediterranean explosive volcanic activity. [PDF]
Leicher N +8 more
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