锆石年龄对利古里亚-皮埃蒙特洋晚侏罗世岩浆活动的制约

IF 2.2 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Terra Nova Pub Date : 2024-05-18 DOI:10.1111/ter.12723
Marcello de Togni, Gianni Balestro, Daniela Rubatto, Daniele Castelli, Marco Gattiglio, Andrea Festa
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引用次数: 0

摘要

古地理重建显示,利古里亚-皮埃蒙特洋(LPO)是一个相对狭窄的大洋盆地,但大洋岩石圈的实际生成量和岩浆增生的时间仍存在争议。对苏萨和兰佐山谷蛇绿岩(西阿尔卑斯山)的两对铁钛氧化物辉长岩和偏闪长岩中的锆石进行了新的 U-Pb 测定,得出了侏罗纪晚期的岩浆年龄(约 150 Ma),比 LPO 中的大多数岩浆活动年轻 10-15 Ma。本文结合 LPO 的结构构造,讨论了所提供的地质年代数据的潜在意义,并强调所调查的蛇绿岩代表了西阿尔卑斯山增生的最年轻的大洋岩石圈。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Late Jurassic magmatism in the Ligurian‐Piedmont Ocean constrained by zircon ages of mafic and felsic meta‐intrusives
Paleogeographic reconstructions show that the Ligurian‐Piedmont Ocean (LPO) was a relatively narrow oceanic basin but the actual amount of oceanic lithosphere generated and the timing of magmatic accretion are still subjects of debate. New U–Pb dating of zircon from two pairs of FeTi‐oxide metagabbro and metaplagiogranite s.l. of the Susa and Lanzo Valleys Ophiolites (Western Alps) yields Late Jurassic magmatic ages (~150 Ma), 10–15 Ma younger than most of the magmatism in the LPO. The potential significance of the geochronological data presented are discussed in relation to the structural architecture of the LPO, emphasizing that the investigated ophiolites represent the youngest oceanic lithosphere accreted in the Western Alps.
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来源期刊
Terra Nova
Terra Nova 地学-地球科学综合
CiteScore
4.80
自引率
8.30%
发文量
59
审稿时长
2.3 months
期刊介绍: Terra Nova publishes short, innovative and provocative papers of interest to a wide readership and covering the broadest spectrum of the Solid Earth and Planetary Sciences. Terra Nova encompasses geology, geophysics and geochemistry, and extends to the fluid envelopes (atmosphere, ocean, environment) whenever coupling with the Solid Earth is involved.
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