Takehiko Suzuki
Biographic Data
| ID | 4129490 |
|---|---|
| NAME | Takehiko Suzuki |
| GIVEN NAMES | Takehiko |
| FAMILY NAME | Suzuki |
| SIGNATURE | SUZUKI T |
| AFFILIATIONS | Tokyo Metropolitan University |
| ORCID | 0000-0002-6474-1698 |
| VERIFIED | Yes |
| TOTAL WORKS | 13 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 13 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1996 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 0 |
Two Early Pleistocene Tephras Detected within the Kazusa Group in the Kanto Plain
Two previously described tephras are correlated with tephra layers at several areas in the Kanto Plain, including the Sayama Hills, beneath the Musashino Uplands and the Tama Hills in western part of the plain, the Choshi district, the Boso Peninsula, and the northern part of the Miura Peninsula, defining them as SYG-Kd29 and Ob3-Kd31B. The eruption ages for SYG-Kd29 and Ob3-Kd31B are precisely determined from a chronological framework composed o…
The Formation of Late Pleistocene and Holocene Sand Dunes on Kikaijima Island, Nansei Islands
Coastal sand dunes dating to the latter part of the late Pleistocene were constructed at substantially lower sea levels on Kikaijima Island. They are preserved because of large-magnitude uplifts ascertained from occurrences of outstanding late Pleistocene and Holocene coral terraces. In addition, because Holocene sand dunes occur close to those of Marine Oxygen Isotope Stage 3 (MIS 3), the island is ideal for examining the environments of the for…
Tephrostratigraphy and Eruption History of Kozushima Volcano, Izu Islands, Central Japan during the Last 30,000 Years
Kozushima is a volcanic island, located in the northern part of the Izu Islands, approximately 170 km SSW of central Tokyo. The volcanism of Kozushima Volcano started at 80-60 ka and formed monogenetic volcanoes. The latest eruption occurred in AD 838, and was associated with the formation of the lava dome and pyroclastic cone of Tenjo-san. In order to contribute to the long-term forecasting of volcanic eruptions on the Izu Islands off Tokyo, the…
Sequence of Early Pleistocene Shirakawa ignimbrites and their identifications in distal areas in Northeast Japan
Studies of the Quaternary in Japan
Recognition of Hakone-TAu11 tephra and sea-level change from MIS 6 to 5 around Mito, northeast Kanto, central Japan
Enhancing tephrochronology and its application (INTREPID project)
Identification of Lower Pleistocene tephras under Tokyo and reconstruction of Quaternary crustal movements, Kanto Tectonic Basin, central Japan
Sakurajima-Satsuma (Sz-S) and Noike-Yumugi (N-Ym) tephras
Hiroshi Machida – Respected tephrochronologist, teacher, leader
Shinji Nagaoka (1958–2011)
Analysis of titanomagnetite within weathered middle Pleistocene KMT tephra and its application for fluvial terrace chronology, Kanto Plain, central Japan
Discharge rates of fallout tephra and frequency of plinian eruptions during the last 400,000 years in the southern Northeast Japan Arc
No prominent works on this page.
Discharge rates of fallout tephra and frequency of plinian eruptions during the last 400,000 years in the southern Northeast Japan Arc
Analysis of titanomagnetite within weathered middle Pleistocene KMT tephra and its application for fluvial terrace chronology, Kanto Plain, central Japan
Enhancing tephrochronology and its application (INTREPID project)
Identification of Lower Pleistocene tephras under Tokyo and reconstruction of Quaternary crustal movements, Kanto Tectonic Basin, central Japan
Sakurajima-Satsuma (Sz-S) and Noike-Yumugi (N-Ym) tephras
Hiroshi Machida – Respected tephrochronologist, teacher, leader
Shinji Nagaoka (1958–2011)
Recognition of Hakone-TAu11 tephra and sea-level change from MIS 6 to 5 around Mito, northeast Kanto, central Japan
Studies of the Quaternary in Japan
Sequence of Early Pleistocene Shirakawa ignimbrites and their identifications in distal areas in Northeast Japan
The Formation of Late Pleistocene and Holocene Sand Dunes on Kikaijima Island, Nansei Islands
Coastal sand dunes dating to the latter part of the late Pleistocene were constructed at substantially lower sea levels on Kikaijima Island. They are preserved because of large-magnitude uplifts ascertained from occurrences of outstanding late Pleistocene and Holocene coral terraces. In addition, because Holocene sand dunes occur close to those of Marine Oxygen Isotope Stage 3 (MIS 3), the island is ideal for examining the environments of the for…
Tephrostratigraphy and Eruption History of Kozushima Volcano, Izu Islands, Central Japan during the Last 30,000 Years
Kozushima is a volcanic island, located in the northern part of the Izu Islands, approximately 170 km SSW of central Tokyo. The volcanism of Kozushima Volcano started at 80-60 ka and formed monogenetic volcanoes. The latest eruption occurred in AD 838, and was associated with the formation of the lava dome and pyroclastic cone of Tenjo-san. In order to contribute to the long-term forecasting of volcanic eruptions on the Izu Islands off Tokyo, the…
Two Early Pleistocene Tephras Detected within the Kazusa Group in the Kanto Plain
Two previously described tephras are correlated with tephra layers at several areas in the Kanto Plain, including the Sayama Hills, beneath the Musashino Uplands and the Tama Hills in western part of the plain, the Choshi district, the Boso Peninsula, and the northern part of the Miura Peninsula, defining them as SYG-Kd29 and Ob3-Kd31B. The eruption ages for SYG-Kd29 and Ob3-Kd31B are precisely determined from a chronological framework composed o…
Geology (13 works) · Geology and Paleoclimatology Research (11 works) · Volcano (10 works) · Paleontology (9 works) · Tephra (9 works) · earthquake and tectonic studies (6 works) · Geochemistry (6 works) · Tephrochronology (5 works) · Geography (4 works) · Geological and Geochemical Analysis (4 works)