GRANITIC MAGMA GENESIS IN OCEANIC ARC SETTING AND CONTINENTAL CRUST FORMING PROCESSES

大洋弧环境中的花岗岩岩浆成因和大陆地壳形成过程

• 批准号: 08454154
• 负责人: ARIMA Makoto
• 金额: $ 2.82万
• 依托单位: YOKOHAMA NATIONAL UNIVERSITY
• 依托单位国家: 日本
• 项目类别: Grant-in-Aid for Scientific Research (B)
• 财政年份: 1996
• 资助国家: 日本
• 起止时间: 1996 至 1997
• 项目状态: 已结题
• 来源: https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-08454154/
• 关键词: OCEANIC ARC; TONALITE; HIGH PRESSURE EXPERIMENT; PARTIAL MELTING; LOW CRUST; TANZAWA; IZU-BONIN-MARIANA (IBM) ARC; 花こう岩マグマ; 高温・高圧実験; 伊豆-ボニン-マリアナ弧

In order to evaluate granitic magma generation and crustal growth in the oceanic island arc system, a series of hydrous partial melting experiments on low-K basalt compositions were done together with petrological and geochemical studies on the Miocene Tanzawa plutonic complex. Melt compositions in the high pressure melting experiments show low-K calc-alkalic trends, and are classified as metaluminous or peraluminous tonalite. These features are similar to the felsic rocks in the Izu-Bonin-Mariana (IBM) arc, e.g., Tanzawa plutonic rocks. The anatectic origin of Tanzawa tonalites is consistent with geochemical modeling, which demonstrate that the REE characteristics of Tanzawa plutonic rocks (which represents the middle crust of the IBM arc) can be generated by partial melting of amphibolite in the lower crust (-50% melting at 1050ﾟC and below 1.2GPa). The Tanzawa plutonic complex is interpreted to be exposed middle crust of the IBM arc, which was uplifted during the collision. Partial melting of hydrated mafic lower crust might play an important role in felsic middle crust formation in the IBM arc.

为了评估海洋岛弧系统中的花岗岩岩浆产生和地壳生长，对低k玄武岩组成的一系列静水熔化实验以及对中新世塔济该底川普鲁氏络合物的岩石学和地球化学研究进行了进行。高压熔化实验中的熔体成分显示出低k骨的趋势，并被归类为金属或毛状的音调。这些特征类似于Izu-Bonin-Mariana（IBM）弧中的长英质岩石，例如Tanzawa Plutonic Rocks。 Tanzawa Tonalites的解剖学起源与地球化学建模一致，这表明Tanzawa Plutonic Rocks的REE特征（代表IBM ARC的中间地壳）可以通过在下层壳中部分融化在低甲虫中的部分融化（在1050％C.-50％旋转）中（-50％C）和以下1.2GPA）产生。 Tanzawa Plutonic综合体被解释为IBM弧的中间地壳，在碰撞期间被抬高。水合健康下层外壳的部分融化可能在IBM ARC中长石中部地壳形成中起重要作用。

项目成果

Nakajima,K & Arima,M: "Melting experiments on hydrous Low-K-Tholeiite:Implications for the genesis of tonalitic rust in the IBM arc" The Island Arc. (印刷中). (1998)

Nakajima,K 和 Arima,M：“含水低 K 拉斑铁矿的熔化实验：对 IBM 弧中英闪长铁锈成因的影响”The Island Arc（1998 年出版）。

有馬 眞: "岩波書店,地球惑星科学,13巻" 火成作用の変遷と大陸地殻の進化, 259-302 (1998)

有马诚：《岩波书店，地球与行星科学，第 13 卷》岩浆作用的变化和大陆地壳的演化，259-302 (1998)

Shaw, R.K., and Arima, M.: "Mineral Chemistry, reaction textures, thermobarometry and P-T path deduced from pyroxene granulites of Rayagada, Eastern Ghats, India" J.Southeast Asian Earth Sciences. 14. 175-184 (1996)

Shaw, R.K. 和 Arima, M.：“从印度东高止山脉 Rayagada 的辉石麻粒岩推导出来的矿物化学、反应结构、温压和 P-T 路径”J.东南亚地球科学。

Shaw,R.K. & Arima,M.: "High temperature metamorphic imprinton calcusilicate granulites of Rayagada,Eastern Ghats,Indiai implication for the isoboric cooling path" Contribntios to Mineralosy and Petrology. 126. 169-180 (1996)

肖，R.K.

Shaw, R.K.& Arima, M.: "Protegozoic evants in the Eastern Ghats GranuliteBelt,India,edidence from Rb-Sr,Sw-Nd on d SHRIMO dating." J.of Geology. 105. 645-656 (1997)

肖，R.K.