30 Myr of Cenozoic magmatism along the Tethyan margin during Arabia–Eurasia accretionary orogenesis (Meghri–Ordubad pluton, southernmost Lesser Caucasus)
Published inLithos, vol. 288-289, p. 108-124
Publication date2017
Abstract
Keywords
- Tethyan orogenic belt
- Arabia-Eurasia collision
- Crustal growth
- Calc-alkaline
- Shoshonitic and adakitic series
- Geochemical modeling
- Lesser Caucasus
Research groups
Funding
- Swiss National Science Foundation - Episodic Mesozoic to Tertiary ore-forming events along the Lesser Caucasus and adjoining tectonic provinces [138130]
- Swiss National Science Foundation - Episodic Mesozoic to Tertiary ore-forming events in successive geodynamic settings in an accretionary orogenic belt: the case of the Tethys orogenic belt [155928]
- Swiss National Science Foundation - Metallogeny of the Lesser Caucasus: From arc construction to post-collision evolution [168996]
- Autre - SCOPES Joint Research Projects IB7620-118901 and IZ73Z0-128324
Citation (ISO format)
REZEAU, Hervé et al. 30 Myr of Cenozoic magmatism along the Tethyan margin during Arabia–Eurasia accretionary orogenesis (Meghri–Ordubad pluton, southernmost Lesser Caucasus). In: Lithos, 2017, vol. 288-289, p. 108–124. doi: 10.1016/j.lithos.2017.07.007
Main files (1)
Article (Published version)
Identifiers
- PID : unige:95796
- DOI : 10.1016/j.lithos.2017.07.007
Additional URL for this publicationhttp://linkinghub.elsevier.com/retrieve/pii/S0024493717302463
Journal ISSN0024-4937