Effects of ridge subduction on Early Cretaceous magmatism in Kitakami Mountains, Japan
Effects of ridge subduction on Early Cretaceous magmatism in Kitakami Mountains, Japan
批准号:
06640574
负责人:
TSUCHIYA Nobutaka
金额:
$1.15万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
1994
资助国家:
日本
项目状态:
已结题
起止时间:
1994 至 1996
中文摘要
点击翻译按钮获取中文摘要
英文摘要
The Cretaceous igneous rocks in the Kitakami Mountains consist mainly of plutonic rocks with minor amounts of volcanic rocks and dike rocks. The radiometric ages of plutonic rocks are concentrated around 120 Ma, and these plutonic rocks give contact metamorphisms on some volcanic and dike rocks. The petrochemical signatures of plutonic rocks are similar to those of volcanic rocks, but are different from those of dike rocks. From this, Cretaceous igneous rocks in the Kitakami Mountains are divided into main series (plutonic rocks and volcanic rocks) and early dyke series. The main series rocks are composed mainly of calcalkine (rarely tholeiitic) rocks, adakitic pluton distributed along eastern margin of the Kitakami Mountains, and sporadic shoshonitic rocks. Petrochemical evidence indicates that the adakitic plutonic rocks can be derived by direct partial melting of subducted slab. The presence of adakitic magmas of slab melting origin indicates the subduction of young and hot oceanic crust. Detailed investigation of incompatible trace elements suggests that calcalkaline to shoshonitic rocks of the main series derived from various degrees of partial melting of a mantle wedge. The early dyke series contain high-Nb basalts with petrochemical characteristics of intraplate alkali basalts and Sr-rich andesitic rocks similar to "bajaites". Alkaline magmatism would be produced by small degrees of decompressive partial melting of mantle materials rising adiabatically through the slab window upon ridge subduction. Bajaite has the common nature of petrochemistry to adakite except high content of Mg, Cr, and Ni. This suggests that bajaitic magmas were formed by reactions between ascending adakitic melt and a mantle peridotite.The occurrence of these rocks suggests ridge subduction, which would promote passive upwelling of asthenosphere (slab window) and produce alkali basalt, and subsequent subduction of young and hot oceanic slab appropriate for slab melting.
期刊论文(20)
专著(0)
科研奖励(0)
会议论文
登录
查看更多内容
土谷信高: "東北日本白亜紀火成活動と海嶺沈み込み." 「月刊地球」. 16・8. 490-494 (1994)
Nobutaka Tsuchiya:“日本东北部的白垩纪火成岩活动和洋脊俯冲。”地球月刊 16/8(1994 年)。
DOI:
--
发表时间:
期刊:
影响因子:
--
作者:
[]
通讯作者:
土谷信高: "北上山地姫神深成岩類におけるK_2O含有量の多様性とその成因." 岩手大学教育学部研究年報. 56・1. 83-112 (1996)
土屋信隆:“北上山姬神深成岩中 K_2O 含量的多样性及其起源”,岩手大学教育学院年度报告 56・1(1996 年)。
DOI:
--
发表时间:
期刊:
影响因子:
--
作者:
[]
通讯作者:
土谷信高: "Rh 管球を用いた蛍光X線分析法による岩石試料中の主成分および微量成分の定量分析." 岩手大学教育学部研究年報. 55・1. 89-110 (1995)
Nobutaka Tsuchiya:“使用Rh管对岩石样品中的主要成分和痕量成分进行定量分析”岩手大学教育学院研究年度报告55・1(1995年)。
DOI:
--
发表时间:
期刊:
影响因子:
--
作者:
[]
通讯作者:
Miyashita,S.: "Petrology of the Okushiri Ridge Basalts in the Japan Sea Basin:Arc-and Plume-type magma series" Mem.Geol.Soc.Japan. 44. 1-21 (1995)
Miyashita,S.:“日本海盆奥尻脊玄武岩的岩石学:弧型和羽状岩浆系列”Mem.Geol.Soc.Japan。
DOI:
--
发表时间:
期刊:
影响因子:
--
作者:
[]
通讯作者:
Tsuchiya, N.and Kanisawa, S.: "Early Cretaceous Sr-rich silicic magmatism by slab melting in the Kitakami Mountains, Northeast Japan." J.Geophys.Res.99-B11. 22205-22220 (1994)
Tsuchiya, N. 和 Kanisawa, S.:“日本东北部北上山脉的早白垩世富锶硅质岩浆作用,由板片熔化引起。”
DOI:
--
发表时间:
期刊:
影响因子:
--
作者:
[]
通讯作者:
共 14 条
海外基金