Temporal and apatial variations of the Cenozoic volcanic rocks from the Notrheast Japan

日本东北部新生代火山岩的时空变化

• 批准号: 03302022
• 负责人: SHUTO Kenji
• 金额: $ 6.91万
• 依托单位: Niigata University
• 依托单位国家: 日本
• 项目类别: Grant-in-Aid for Co-operative Research (A)
• 财政年份: 1991
• 资助国家: 日本
• 起止时间: 1991 至 1993
• 项目状态: 已结题
• 来源: https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-03302022/
• 关键词: Volcanic history; Northeast Japan arc; Southwesr Japan; Japan Sea back-arc basin; K-Ar age; Sr and Nd isotopes; The spreading of the Japan Sea; Source; マントル; Sr同位体比; Nd同位体比; 日本拡大; 火山フロント; 起源マントル; 漸新世; 中新世; 漸新世〜第四紀; Ncl同位体比; 火山岩組成の時間的変遷

The results obtained from this research project are summarized as follows.1) The excellent petrological investigations have been made for numerous Cenozoic volcanic rocks from various localities in the Kyushu, Chugoku Hokuriku, northern Kanto, Tohoku and southwestern and northeastern Hokkaido discricts. Basaltic rocks dredged from the Okushiri Ridge, off western Hokkaido were also described prtographically. These petrological data may play an important role in revealing not only the origin of these volcanic rocks from each field but also the tectonic events around the circum Japan Sea region.2) K-Ar age determination has been carried out for many Tertiary volcanic rocks, especially those from the Northeast Japan arc. Our new data and the available rediometric age data for the Tertiary volcanic rocks provided by many previous workers have made it possible to distinguish the three different volcanic fronts in the NE Japan arc in temporal and spacial distribution.3) Based on Sr and Nd iso … More topic data for Tertiary and Quaternary basaltic rocks from the NE and SW Japan arcs, relationships are discussed between the temporal variation on magma source characteristics and the opening of the Japan Sea back-arc basin. Basaltic rocks from the back-arc side of the NE Japan arc during 35 0 Ma can be divided into two different groups with respect to initial Sr isotopic ratios, initial epsilonNd values and ages. One is characterized by higher Sri ratios (0.7040-0.7058) and lower epsilonNd values (0-+3) and the other by lower Sri ratios (0.7029-0.7040) and higher epsilonNd values (+3-+8). The former basaltic activity has taken place continuously during 30-10 Ma, whereas the latter activity occurred mainly in two periods ; i.e. ; at around 34-35 Ma and after 15 Ma. Similar evidences are also observed in basaltic rocks from the transitional zone to the back-arc side where basaltic activity characterized by higher Sri ratios took place continuously during 15-0 Ma, whereas that by lower Sri ratios occurred at around 15 Ma and after 3 Ma. These evidences suggest that the sub-continental mantle beneath the NE Japan arc may have constructed layred structure ; upper isotopically enriched (Sri=0.7040-0.7058, epsilonNd=0-+3) and lower depleted (Sri=0.7029-0.7040, epsilonNd=+3-+8) layrs. Basaltic magmas with enriched isotopic nature are considered to have been formed from the upper layr, while those with depleted isotopic one from the lower layr. Less

本研究取得的主要成果如下：1）对九州、中国、北陆、北方关东、东北、北海道西南、东北等地的新生代火山岩进行了大量的岩石学研究。从北海道西部的奥尻海岭挖掘出的玄武岩也被描述为原岩。这些岩石学资料不仅对揭示各矿田火山岩的成因，而且对环日本海地区的构造事件也有重要作用。2）对许多第三纪火山岩，特别是东北日本弧的火山岩进行了K-Ar年龄测定。结合前人提供的第三纪火山岩的放射性年龄资料，可以区分日本东北弧三个不同的火山前缘的时空分布 ...更多信息 利用日本弧东北部和西南部第三纪和第四纪玄武质岩石的专题资料，讨论了岩浆源区特征的时间变化与日本海弧后盆地开启的关系。35.0Ma期间日本弧东北弧弧后侧的玄武岩可分为两个不同的组方面的初始Sr同位素比值，初始ε Nd值和年龄。一种是具有较高的Sri比（0.7040-0.7058）和较低的ε Nd值（0-+3），另一种是具有较低的Sri比（0.7029-0.7040）和较高的ε Nd值（+3-+8）。前者在30-10 Ma期间持续发生，后者主要发生在34-35 Ma前后和15 Ma以后两个时期。在过渡带至弧后侧的玄武岩中也观察到类似的证据，在15-0 Ma期间，具有较高Sri比值特征的玄武岩活动持续发生，而具有较低Sri比值特征的玄武岩活动则发生在15 Ma左右和3 Ma以后。这些证据表明，东北日本弧之下的陆下地幔可能具有层状结构，上部同位素富集（Sri=0.7040-0.7058，ε Nd =0-+3），下部同位素亏损（Sri=0.7029-0.7040，ε Nd =+3-+8）。同位素富集的玄武岩浆来自上地幔，同位素亏损的玄武岩浆来自下地幔。少

项目成果

Ohki Jyun-ichi: "Shifting of the volcanic fronts during Farly to Late Miocene in the Northeast Japan arc." The Island Arc.2. 87-93 (1993)

Ohki Jyun-ichi：“日本东北弧远至晚中新世期间火山锋的移动。”

Shuto Kenji: "The relationships between drastic changes in Sr isotope ratios of magma sousces beneath the N E Japan arc and the spreading of the Japan Sea back-arcbasin" Mineralogy and Petrogy. 49. 71-90 (1993)

Shuto Kenji：“日本东北弧下方岩浆源的锶同位素比的剧烈变化与日本海弧后盆地扩张之间的关系”矿物学和岩石学。

Watanabe Naoki: "K-Arages of the Miocene volcanic rocks from the Tomsri area in the Shimokita Peninsula,Northeast Japan arc." 岩鉱. 88. 352-358 (1993)

渡边直树：“日本东北部岛弧 Tomsri 地区中新世火山岩的 K-Arages。”88. 352-358 (1993)

Naoki Watanabe: "K-Ar ages of the Miocene volcanic rocks from the Tomari area in the Shimokita Peninsula, Northeast Japan arc" J.Min.Pet.Econ.Geol.88. 352-358 (1993)

Naoki Watanabe：“日本东北部下北半岛泊地区中新世火山岩的 K-Ar 年龄”J.Min.Pet.Econ.Geol.88。

Watanabe Naoki: "K-Ar ages of the Miocene volcanic rocks from the Tomari area in the Shinokita Peninsula,Northeast Japan arc." 岩鉱. 88. 352-358 (1993)

渡边直树：“日本东北部岩矿弧泊地区中新世火山岩的 K-Ar 年龄。”