The root zone dynamics under the continent collision zone. The role of crustal melting at extremely high pressure and high temperature conditions.

大陆碰撞带下的根区动力学。

基本信息

  • 批准号:
    14403013
  • 负责人:
  • 金额:
    $ 8.51万
  • 依托单位:
  • 依托单位国家:
    日本
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
  • 财政年份:
    2002
  • 资助国家:
    日本
  • 起止时间:
    2002 至 2004
  • 项目状态:
    已结题

项目摘要

Co-operative field survey in the Bohemia massif Czech Republic, has been carried out three times as the joint project between Kyoto University and Charles University from 2002 to 2004, and the field relationships of the representative root zone materials, such as peridotite, acidic-intermediate granulite, pelitic gneiss and various type xenoliths mainly hosted by granulite, have been revealed.In-door work for more than 600kg rock specimens collected by the field survey mentioned above revealed following facts and following 5 topics of them were shown in the annual meeting of Japanese Geological Society at Shizuoka University in 2003 : 1)Re-evaluation of Peak pressure conditions for granulite by Hirajima et al., 2)Finding of UHF eclogite from Nave Dvory peridotite body by Nakamura et al., which issue has been published in Journal of metamorphic Petrology in 2004, 3)Metamorphic history of garnet peridotite at Plesovice quarry by Naemura et al., 4)A significance of un-symmetric diffusion … More texture observed in acidic granulite by Usuld et al., and 5)Transformation of Al2SiO5 phases enhanced by shear stress and its significance by Hiroi. et al. Further In-door work done in 2004 revealed following facts ; 6)Petrological aspect of kinzigite and migmatite at Ktis by Kobayashi, 7)P-T history of calc-silicate nodule at Horny Bory and the finding of fluid inclusion by Hisashima, and 8)P-T history of Mohelno Grt-peridotite by Kamei et al.. Hirajima showed a paper on the P-T history of Grt peridotite at IGC32 held in Florence and discuss the exhumation mechanism of the root zone materials.Fluid inclusion study using the heating stage system purchased by this financial support revealed 9)Multi-stage fluid activities took place in the P-T history of Horny Bory calc-silicate nodule and 10)Quartz eclogite derived from crustal materials in the Sanbagawa belt contains H2O-rich fluid. The tuning of H2O-rich fluid activity have been constrained by the combination of detailed petrological study by Ohtsuka and Hirajima Steering meeting was held in March 2004 including Martin Svojtka at Kyoto and determined the active plan in summer of 2004. Summarizing meeting was held in March 2005 at Kyoto and discussed future plan. Less
波西米亚地块捷克共和国的合作现场调查是在2002年至2004年的京都大学查尔斯大学之间的联合项目中进行的,并且代表了根部区域材料,例如橄榄岩,橄榄岩,橄榄石,野生矿石经过以下事实所述的现场调查收集的花岗岩,鞘岩和各种K标本,并在2003年在Shizuoka University的日本地质学会的年度肉类肉类肉类上进行了5个主题:1)重新评估Hirajima颗粒的峰值压力条件的重新评估等等。 usuld等人,以及5)Al2SIO5阶段的转化是通过hiroi及其在Kobayashi的kinzigite和Migmatite方面增强的。 8)Kamei等人的p-Thelno grt-卵石。在角质Bory的P-T历史上计算硅酸盐结节10)源自Sanbagawa Belt中的地壳的石英纤维岩含有富含H2O的液体的含量。 2004年3月在京都举行的包括马丁·斯沃伊特卡(Martin Svojtka),并确定2004年夏季的积极计划在2005年3月在京都举行,并讨论了未来的计划

项目成果

期刊论文数量(54)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Yoshida, D., Hirajima, T., Ishiwatari, A.: "Pressure-Temperature Path Recorded in the Yangkou lherzolite, in Su-Lu Ultrahigh-pressure Metamorphic Belt, Eastern China"Journal of Petrology. 45(In press). (2004)
吉田,D.,平岛,T.,石渡,A.:“中国东部苏鲁超高压变质带仰口二辉橄榄岩中记录的压力-温度路径”岩石学杂志。
  • DOI:
  • 发表时间:
  • 期刊:
  • 影响因子:
    0
  • 作者:
  • 通讯作者:
Hirajima, T., Nakamura: "The Dabie Shan-Sulu orogen"In Ultrahigh pressure Metamorphism, European Mineralogical Union Notes in Mineralogy. 5. 105-144 (2003)
Hirajima, T.,Nakamura:“大别山-苏鲁造山带”,超高压变质作用,欧洲矿物学联盟矿物学笔记。
  • DOI:
  • 发表时间:
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    0
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Diatexite and metatexite from the Higo metamorpchi rocks, west-central Kyushu, Japan.
日本九州中西部肥后变质岩中的硅藻土和变质岩。
Very high-pressure (> 4 GPa) eclogite associated with the Moldanubian garnet peridotite (Nove Dvory, Czech Republic).
与摩尔达努比亚石榴石橄榄岩(捷克共和国新德沃里)相关的极高压(> 4 GPa)榴辉岩。
  • DOI:
  • 发表时间:
    2004
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Nakamura;D.;Svojtka;M.;Naemura;K.;Hirajima;T.
  • 通讯作者:
    T.
Brun, M., Compagnoni, R., Hirajima, T., Rubbo, M., (2002): "Jadeite with the Ca-Eskola molecule from an ultra-high pressure metagranodiorite, Dora-Maira Massif, Western Alps"Contributions to Mineralogy and Petrology,. 142. 515-519 (2002)
Brun, M.、Compagnoni, R.、Hirajima, T.、Rubbo, M., (2002):“来自西阿尔卑斯山 Dora-Maira 地块的超高压变花岗闪长岩中含有 Ca-Eskola 分子的硬玉”
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  • 影响因子:
    0
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HIRAJIMA Takao其他文献

A new occurrence of okhotskite in the Kurosegawa belt, Kyushu, Japan: the okhotskite + Mn–lawsonite assemblage as a potential high–pressure indicator
日本九州黑濑川带中新发现的鄂霍次石矿:鄂霍次石+锰-硬铝石矿组合作为潜在的高压指标
Single Crystal Elasticity by Inelastic X-ray Scattering udner extreme conditions
极端条件下非弹性 X 射线散射的单晶弹性
  • DOI:
  • 发表时间:
    2022
  • 期刊:
  • 影响因子:
    0
  • 作者:
    YABUTA Wataru;HIRAJIMA Takao;Hiroshi FUKUI
  • 通讯作者:
    Hiroshi FUKUI
Non-barometric behaviour of Na pyroxenes in blueschist(BS)-facies metamorphic rocks
蓝片岩(BS)相变质岩中钠辉石的非气压行为
  • DOI:
  • 发表时间:
    2021
  • 期刊:
  • 影响因子:
    0
  • 作者:
    YABUTA Wataru;HIRAJIMA Takao
  • 通讯作者:
    HIRAJIMA Takao
Multiple origins of UHP eclogites in a garnet peridotite block (Nové Dvory, Czech Republic) and short duration of heating
石榴石橄榄岩块(捷克共和国新德沃里)中超高压榴辉岩的多重起源和加热持续时间短
Mineralogical heterogeneity of UH<i>P</i> garnet peridotite in the Moldanubian Zone of the Bohemian Massif (Nové Dvory, Czech Republic)
波希米亚地块摩尔达努比亚带 UH<i>P</i>石榴石橄榄岩的矿物学异质性(捷克共和国新德沃里)

HIRAJIMA Takao的其他文献

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{{ truncateString('HIRAJIMA Takao', 18)}}的其他基金

Investigation of deep fluid using maluti-solid-phase inclusions
利用马鲁蒂固相包裹体研究深层流体
  • 批准号:
    22244067
  • 财政年份:
    2010
  • 资助金额:
    $ 8.51万
  • 项目类别:
    Grant-in-Aid for Scientific Research (A)
The root zone dynamics under the continent collision zone. The elucidation of the fluid activity at extremely high pressure and high temperature conditions
大陆碰撞带下的根区动力学。
  • 批准号:
    17204047
  • 财政年份:
    2005
  • 资助金额:
    $ 8.51万
  • 项目类别:
    Grant-in-Aid for Scientific Research (A)
Exhumation path of metamorphic rocks and the development of the orogenic belt
变质岩折返路径与造山带的发育
  • 批准号:
    11640477
  • 财政年份:
    1999
  • 资助金额:
    $ 8.51万
  • 项目类别:
    Grant-in-Aid for Scientific Research (C)
Development of the continental crust deruced from deep subducted crustal materials
深俯冲地壳物质推导出的大陆地壳的发育
  • 批准号:
    08454156
  • 财政年份:
    1996
  • 资助金额:
    $ 8.51万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
Modeling for the development of the crust
地壳发育建模
  • 批准号:
    06302031
  • 财政年份:
    1994
  • 资助金额:
    $ 8.51万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
Development of the crust continental in the colision zone
碰撞带地壳大陆的发育
  • 批准号:
    05640530
  • 财政年份:
    1993
  • 资助金额:
    $ 8.51万
  • 项目类别:
    Grant-in-Aid for General Scientific Research (C)

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    2023
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    42302057
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    青年科学基金项目
崆岭地体古元古代麻粒岩相变质作用与深熔作用研究
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伊朗东部锡斯坦缝合带:大洋高压/低温岩石的折返历史和推测的麻粒岩相混杂岩的地质意义。
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    2015
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克拉通麻粒岩、辉石岩和榴辉岩捕虏体:大陆地壳演化和陆地微量元素循环档案
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