Late Jurassic magmatism in the Ligurian-Piedmont Ocean constrained by zircon ages of mafic and felsic meta-intrusives

被引：3

作者：

de Togni, Marcello ^{[1
]}

Balestro, Gianni ^{[1
]}

Rubatto, Daniela ^{[2
]}

Castelli, Daniele ^{[1
]}

Gattiglio, Marco ^{[1
]}

Festa, Andrea ^{[1
,3
]}

机构：

[1] Univ Turin, Dept Earth Sci, Via Valperga Caluso 35, I-10125 Turin, Italy

[2] Univ Bern, Inst Geol Sci, Bern, Switzerland

[3] CNR, Inst Geosci & Earth Resources, Turin, Italy

来源：

TERRA NOVA | 2024年 / 36卷 / 05期

关键词：

Fe-Ti metagabbro; Ligurian-Piedmont Ocean; metaplagiogranite; U-Pb zircon dating; Western Alpine Ophiolites; NORTHERN APENNINE OPHIOLITES; WESTERN ALPS; U-PB; TECTONIC EVOLUTION; ALPINE; SUBDUCTION; TETHYS; MONVISO; CRUST; EXHUMATION;

D O I：

10.1111/ter.12723

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

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 (similar to 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.

引用

页码：403 / 413

页数：11