用户名: 密码: 验证码:
纳米比亚欢乐谷地区斑状花岗岩地球化学特征及成因
详细信息    查看官网全文
摘要
<正>达马拉造山带(Damara Orogen)属于泛非造山带的一部分。在纳米比亚,达马拉造山带分为南北向海岸分支和北东向内陆分支,是Congo,Kalahari和Rio de Plata克拉通碰撞的产物(Stanistreet et al.1991;Prave 1996)。达马拉造山带北东向的内陆分支根据断层,航磁解译的线性构造带等线性构造可以划分为不同的带。达马拉造山带陆内分支中央带岩浆活动强烈,形成了大面积的花岗岩类(Miller,1983)。Marlow(1983)将中央带的花岗岩划分为
引文
付建明,马昌前,谢才富,等.2005.湖南金鸡岭铝制A型花岗岩的厘定及其构造分析.地球化学,34(3):7~215-226.
    Brandt R.1985.Preliminary report on the Stratigraphy of the Damara sequence and the geology and gochemistry of Damaran granites in an area between Walvis Bay and Karibib.Communications of the Geological Survey of Namibia 1.31~43.
    Jacob R E.1978.Granite genesis and associated mineralisation in part of the Central Damara Belt.In:Verwoerd,W.J.(Ed.),Mineralisation in Metamorphic Terranes[M].Geological Society of South Africa Special Publication,vol.4,pp.417~432.
    Marlow A G 1983.Geology and Rb-Sr geochronology of mineralised and radioactive granites and alaskites,Namibia.In:Miller,R.McG,ed.,Evolution of the Damara Orogen of South West Africa/Namibia.Geological Society of South Africa,Special Publication 11,pp.289~298.
    Miller R.McG 1983.The Pan-African Damara Orogen of South West Africa/Namibia.In:Miller,R.McG(ed.),Evolution of the Damara Orogen of South West Africa/Namibia[M].Geological Society of South Africa,Special Publications,11:431~515.
    Miller R.McG 2008.The Geology of Namibia,Vols.I and II.Geological Survey of Namibia Special Publication.
    Patino Douce A E and Johnson A D.1991.Phase equilibria and melting productivity in the politic system:Implication for the origin of peraluminous granitoids and aluminous guanulites.Contributions to Mineralogy and petrology,107:20~218
    Prave A R.1996.Tale of three cratons:tectonostratigraphic anatomy of the Damara orogen in northwestern Namibia and the assembly of Gondwanaland.Geology,24,1115~1118.
    Smith D A M.1965.The geology of the area around the Khan and Swakop rivers in South West Africa.Mem geol Surv S Afr,SW Afr Ser 3:113.
    Stanistreet I G,Kukla P A,Henry G 1991.Sedimentary basinal responses to a Late Precambrian Wilson cycle:the Damara orogen and Nama foreland Namibia.Journal of African Earth Sciences,13,141~156.
    Sylvester P J.1998.Post-collisional strongly peraluminous granites.Lithos,45:29~44.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700