Geochemical Study of Collision Volcanism at the Plate Boundary in Turkey -Comparison With Subduction Volcanism in Japan-
土耳其板块边界碰撞火山作用的地球化学研究-与日本俯冲火山作用的比较-
基本信息
- 批准号:63041085
- 负责人:
- 金额:$ 6.4万
- 依托单位:
- 依托单位国家:日本
- 项目类别:Grant-in-Aid for Overseas Scientific Survey.
- 财政年份:1988
- 资助国家:日本
- 起止时间:1988 至 1989
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
All these geochemical data show that there are inhomogeneity in the upper mantle structure related with the plate tectonics in Turkey. In the eastern part, Sr isotopic rations of Karacadag are low, suggesting the less contribution of magma-crust interaction. Sr isotopes for the volcanoes in the lake Van area vary locally. The Sr rations of Nemurut have a correlation with SiO_2 contents, indicating the crustal contamination. He isotopes in this area is higher than that of air, and suggest the presence of mantle He. The value of mantle He is the same as that in the subduction area, suggesting that the He isotopes are the same in both subduction and collision area. In the central part of Turkey, Sr isotopes of Erciyes and Hasan are 0.7038-0.7058 which are in the range of the subduction area. He isotopes show the higher degree of crustal contamination than that in the eastern Turkey. In the western Turkey, the radiogenic ^4He was observed in all over the geothermal area in the Aegean coast. However, the high high ^3He/^4He ratios and low carbon isotopes are obtained in Kula, where Sr isotopes are also very low (0.7030-0.7035). Kula seem to be very special if it is on the extension of Aegean island arc. It should be necessary to examine the Aegean arc in future in comparison with this study.
所有这些地球化学数据表明,与土耳其板块构造有关的上地幔结构存在不均质性。东部卡拉卡达格的锶同位素配分较低,表明岩浆-地壳相互作用的贡献较小。凡湖地区火山的锶同位素在当地有所不同。Nemurut的锶比值与SiO_2含量呈正相关,反映了地壳混染。该区的氦同位素高于空气中的氦同位素,反映了地幔氦的存在。地幔氦的值与俯冲区的值一致,表明俯冲区和碰撞区的氦同位素是相同的。土耳其中部Erciyes和Hasan的锶同位素为0.7038-0.7058,均在俯冲区范围内。氦同位素显示,与土耳其东部相比,地壳污染程度更高。在土耳其西部,爱琴海沿岸地热区的所有地方都观测到了放射性成因的~4He。但库拉具有高的高~3He/~4He比值和低碳同位素,锶同位素也很低(0.7030~0.7035)。如果是在爱琴海岛弧的延伸处,库拉似乎很特别。今后应该有必要对照这项研究来研究爱琴海弧线。
项目成果
期刊论文数量(2)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
J.Matsuda,K.Matsubara,H.Yajima,K.Yamamoto: "Anomalous Ne enrichment in obsidians and Darwin glass;Diffusion of noble gases in silica-rich glasses" Geochim.Cosmochim.Acta. 53. 3025-3033 (1989)
J.Matsuda、K.Matsubara、H.Yajima、K.Yamamoto:“黑曜石和达尔文玻璃中的异常氖富集;富含二氧化硅的玻璃中稀有气体的扩散”Geochim.Cosmochim.Acta。
- DOI:
- 发表时间:
- 期刊:
- 影响因子:0
- 作者:
- 通讯作者:
Jun-ichi Matsuda: "Geochemical study of collision volcanism at the plateboundary in Turkey -Comparison with subduction volcanism in Japan-" DELP News. 24. 11-15 (1988)
Jun-ichi Matsuda:“土耳其板块边界碰撞火山作用的地球化学研究 - 与日本俯冲火山作用的比较 -”DELP 新闻。
- DOI:
- 发表时间:
- 期刊:
- 影响因子:0
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MATSUDA Jun-ichi其他文献
MATSUDA Jun-ichi的其他文献
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{{ truncateString('MATSUDA Jun-ichi', 18)}}的其他基金
The origin of the main component of noble gases in meteorite and its cosmogenic/ geochemical implications
陨石中稀有气体主要成分的起源及其宇宙成因/地球化学意义
- 批准号:
18104010 - 财政年份:2006
- 资助金额:
$ 6.4万 - 项目类别:
Grant-in-Aid for Scientific Research (S)
Behavior of volatile elements at the early stage of our solar system - Exploration of Q, the main host phase of noble gases in meteorite -
太阳系早期挥发性元素的行为 - 陨石中稀有气体的主要宿主相 Q 的探索 -
- 批准号:
14204056 - 财政年份:2002
- 资助金额:
$ 6.4万 - 项目类别:
Grant-in-Aid for Scientific Research (A)
Study of noble gas carrier "Q" in meteorites
陨石中稀有气体载体“Q”的研究
- 批准号:
10440162 - 财政年份:1998
- 资助金额:
$ 6.4万 - 项目类别:
Grant-in-Aid for Scientific Research (B).
Experimental study of elemental process of the earth's core formation-Noble gas geosientific approach-
地核形成元素过程的实验研究-稀有气体地球科学方法-
- 批准号:
06403002 - 财政年份:1994
- 资助金额:
$ 6.4万 - 项目类别:
Grant-in-Aid for Scientific Research (A)
K-Ar dating of volcanic rocks younger than 0.1 m.y.
小于 0.1 m.y 的火山岩的 K-Ar 测年
- 批准号:
60840021 - 财政年份:1985
- 资助金额:
$ 6.4万 - 项目类别:
Grant-in-Aid for Developmental Scientific Research
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