Jurassic Igneous Rocks of the Central Sanandaj–Sirjan Zone (Iran) Mark a Propagating Continental Rift, Not a Magmatic Arc
dc.contributor.ORCID | 0000-0002-8083-4632 (Stern, RJ) | |
dc.contributor.VIAF | 284885305 (Stern, RJ) | |
dc.contributor.author | Azizi, H. | |
dc.contributor.author | Stern, Robert J. | |
dc.contributor.utdAuthor | Stern, Robert J. | |
dc.date.accessioned | 2020-04-11T21:58:22Z | |
dc.date.available | 2020-04-11T21:58:22Z | |
dc.date.issued | 2019-04-29 | |
dc.description | Due to copyright restrictions and/or publisher's policy full text access from Treasures at UT Dallas is limited to current UTD affiliates (use the provided Link to Article). | |
dc.description | Supplementary material is available on publisher's website. Use the DOI link below. | |
dc.description.abstract | Jurassic igneous bodies of the Sanandaj–Sirjan zone (SaSZ) in SW Iran are generally considered as a magmatic arc but critical evaluation of modern geochronology, geochemistry and radiogenic isotopes challenges this conclusion. There is no evidence for sustained igneous activity along the ~1,200 km long SaSZ, as expected for a convergent plate margin; instead activity was brief at most sites and propagated NW at ~20 mm/a. Jurassic igneous rocks define a bimodal suite of gabbro-diorite and granite. Chemical and isotopic compositions of mafic rocks indicate subcontinental lithospheric mantle sources that mostly lacked subduction-related modifications. The arc-like features of S-type granites reflect massive involvement of Cadomian crust and younger sediments to generate felsic melts in response to mafic intrusions. We conclude that Jurassic SaSZ igneous activity occurred in a continental rift, not an arc. SaSZ igneous rocks do not indicate that subduction along the SW margin of Eurasia began in Jurassic time. © 2019 John Wiley & Sons Ltd | |
dc.description.department | School of Natural Sciences and Mathematics | |
dc.identifier.bibliographicCitation | Azizi, H., and R. J. Stern. 2019. "Jurassic igneous rocks of the central Sanandaj–Sirjan zone (Iran) mark a propagating continental rift, not a magmatic arc." Terra Nova 31(5): 415-423, doi: 10.1111/ter.12404 | |
dc.identifier.issn | 0954-4879 | |
dc.identifier.issue | 5 | |
dc.identifier.uri | http://dx.doi.org/10.1111/ter.12404 | |
dc.identifier.uri | https://hdl.handle.net/10735.1/7932 | |
dc.identifier.volume | 31 | |
dc.language.iso | en | |
dc.publisher | Blackwell Publishing Ltd | |
dc.rights | ©2019 John Wiley & Sons Ltd | |
dc.source.journal | Terra Nova | |
dc.subject | Sanandaj (Iran) | |
dc.subject | Sīrjān (Kirmān, Iran) | |
dc.subject | Geology, Stratigraphic—Jurassic | |
dc.subject | Magmatism | |
dc.subject | Igneous rocks | |
dc.title | Jurassic Igneous Rocks of the Central Sanandaj–Sirjan Zone (Iran) Mark a Propagating Continental Rift, Not a Magmatic Arc | |
dc.type.genre | article |
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