Constraints on the formation of geochemically variable plagiogranite intrusions in the Troodos Ophiolite, Cyprus.

Freund, Sarah, Haase, Karsten, Keith, Manuel, Beier, Christoph and Garbe-Schönberg, Dieter (2014) Constraints on the formation of geochemically variable plagiogranite intrusions in the Troodos Ophiolite, Cyprus. Contributions to Mineralogy and Petrology, 167 (2). DOI 10.1007/s00410-014-0978-6.

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Supplementary data:


The geochemistry and petrology of tonalitic to trondhjemitic samples (n = 85) from eight different plagiogranite intrusions at the gabbro/sheeted dyke transition of the Troodos Ophiolite were studied in order to determine their petrogenetic relationship to the mafic plutonic section and the lava pile. The plagiogranitic rocks have higher SiO2 contents than the majority of the glasses of the Troodos lava pile, but lie on a continuation of the chemical trends defined by the extrusive rocks, indicating that the shallow intrusions generally represent crystallised magmas. We define three different groups of plagiogranites in the Troodos Ophiolite based on different incompatible element contents and ratios. The first and most common plagiogranite group has geochemical similarities to the tholeiitic lavas forming the lavas and sheeted dyke complex in the Troodos crust, implying that these magmas formed at a spreading axis. The second plagiogranite group occurs in one intrusion that is chemically related to late-stage and off-axis boninitic lavas and dykes. One intrusion next to the Arakapas fault zone consists of incompatible elementenriched plagiogranites which are unrelated to any known mafic crustal rocks. The similarities of incompatible element ratios between plagiogranites, lavas and mafic plutonic rocks, the continuous chemical trends defined by plagiogranites and mafic rocks, as well as incompatible element modelling results, all suggest that shallow fractional crystallisation is the dominant process responsible for formation of the felsic magmas.

Document Type: Article
Additional Information: Times Cited: 0 Beier, Christoph/F-5604-2012 0
Keywords: Magma evolution Tonalite Trondhjemite Crust formation Fractional crystallisation
Research affiliation: Kiel University
OceanRep > The Future Ocean - Cluster of Excellence
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1007/s00410-014-0978-6
ISSN: 0010-7999
Projects: Future Ocean
Date Deposited: 30 Mar 2015 12:15
Last Modified: 24 Sep 2019 00:16

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