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Submarine terraces reveal Late Quaternary tectonic deformation in the intermediate zone between the island shelf and rift zone of the middle part of the Nanseishoto Islands, southwest Japan

机译：潜艇露台显示了日本西南部南风群岛中间部分岛货架和裂口区之间的晚期四元形构造变形

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Hideaki Goto;
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1. Submarine terraces reveal Late Quaternary tectonic deformation in the intermediate zone between the island shelf and rift zone of the middle part of the Nanseishoto Islands, southwest Japan [J] . Oceanographic Literature Review . 2021,第5期

机译：潜艇露台揭示了日本西南部南风群岛中间部分岛货架和裂口区之间的中间区域的晚期四元构造变形
2. Late Quaternary uplift rate inferred from marine terraces, Muroto Peninsula, southwest Japan: Forearc deformation in an oblique subduction zone [J] . Matsuura Tabito Geomorphology . 2015,第apra1期

机译：从日本西南部室户半岛海洋阶地推断的第四纪晚期隆升速率：斜俯冲带中的前臂变形
3. Submarine Depositional Terraces at Salina Island (Southern Tyrrhenian Sea) and Implications on the Late-Quaternary Evolution of the Insular Shelf [J] . Daniele Casalbore, Claudia Romagnoli, Chiara Adami, Geosciences . 2018,第1期

机译：萨利纳岛（南第勒尼安海）的海底沉积阶地及其对岛架第四纪晚期演化的启示
4. A first extensive hydrothermal field associated with Kuroko-type deposit in a Silicic Submarine caldera in a Nascent Rift Zone, Izu-Ogasawara (Bonin) arc, Japan [C] . Iizasa, K., Sasaki, . 2004

机译：日本伊豆小gas原（波宁）弧新生裂谷硅质海底破火山口中与黑子型沉积有关的第一个广阔的热液场
5. INCREMENTAL AND FINITE STRAINS WITHIN DUCTILE SHEAR ZONES, NARRAGANSETT BASIN, RHODE ISLAND (STRUCTURAL, APPALACHIAN TECTONICS). [D] . BURKS, RACHEL JANE. 1985

机译：在罗得岛州纳拉甘塞特盆地，韧性剪切带内的增量应变和有限应变。（结构，阿巴拉契亚构造）。
6. Nd-isotopic composition of Phanerozoic sediments in the Inner Zone of Southwest Japan Arc: implications on provenance characteristics and contribution to formation of mature island arc system [O] . Hiroo Kagami, Yoshinobu Kawano, Toshiyuki Ikawa, 2004

机译：日本西南内部区的植物古代沉积物的ND-同位素组成：对成熟岛弧系统形成的出种特征和贡献的影响
7. Late Quaternary uplift rate inferred from marine terraces, Muroto Peninsula, southwest Japan: Forearc deformation in an oblique subduction zone [O] . Matsuura Tabito 2015

机译：从日本西南部室户半岛海洋阶地推断的第四纪晚期隆升速率：斜俯冲带中的前臂变形

Submarine terraces reveal Late Quaternary tectonic deformation in the intermediate zone between the island shelf and rift zone of the middle part of the Nanseishoto Islands, southwest Japan

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