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西秦岭造山带郎木寺火山岩锆石U-Pb定年及岩石成因

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对西秦岭造山带郎木寺火山岩进行了岩相学、锆石 U-Pb年代学、主量元素和微量元素地球化学研究.郎木寺火山岩主要由安山岩组成,锆石 LA-ICP-MS的 U-Pb定年,获得郎木寺火山岩的结晶年龄为 217±4 Ma.郎木寺火山岩亲石元素(LILE)富集,高场强元素(HFSE)相对亏损,ΣREE总量为 195.9~418 ppm,(La/Yb)N=12.16~13.93,δEu =0.72~0.81,表明郎木寺火山岩的岩浆源区主要来源于陆壳物质,由幔源岩浆底侵作用引起的下地壳部分熔融形成,岩浆产生机制可能为在碰撞后构造伸展阶段的岩石圈拆沉作用.
Zircon U-Pb Dating and Petrogenesis of the Langmusi Volcanic Rock in West Qinling Orogenic Belt
An integrated study of petrology,zircon U-Pb dating and geochemistry for the Langmusi volcanic rock in the middle part of the west Qinling were carried out.The Langmusi volcanic rocks consist of andecite and trachyandecite.Results show that the zir-con LA-ICP-MS U-Pb age of the Langmusi volcanic rocks is 217±4 Ma.The Langmusi volcanic rocks are characterized by enrich-ments of LILE(e.g.Rb,Ba,U,Th,Pb)and HFSE(e.g.Ta,Nb)depletion,with ΣREE=195.9~418 ppm,(La/Yb)N= 12.16~13.93,δEu= 0.72~0.81,which show the magma of the volcanic rocks was dominantly derived from crustal materials.The Langmusi volcanic rocks were generated by partial melting of lower crust,granodiorite and volcanic rock resulted from lithospheric delamination in post-collisional setting.

Langmusi volcanic rockzircon U-Pb datingpetrogenesis

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辽宁省有色地质一〇五队有限责任公司,辽宁 葫芦岛 125000

郎木寺火山岩 锆石U-Pb年代学 岩石成因

2024

有色矿冶
辽宁省有色金属学会

有色矿冶

影响因子:0.251
ISSN:1007-967X
年,卷(期):2024.40(1)
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