The Lyngen Gabbro: the lower crust of an Ordovician Incipient-Arc.

Kvassnes, Astri J. S., Strand, Anita H., Moen-Eikeland, Heidi and Pedersen, Rolf Birger (2004) The Lyngen Gabbro: the lower crust of an Ordovician Incipient-Arc. Mineralogy and Petrology, 148 (3). pp. 358-379. DOI 10.1007/s00410-004-0609-8.

[img] Text
549_Strand_2004_TheLyngenGabbroTheLower_Artzeit_pubid11603.pdf - Reprinted Version
Restricted to Registered users only

Download (1133Kb) | Contact

Supplementary data:

Abstract

We present evidence for the origin of the Lyngen Gabbro of the Ordovician Lyngen Magmatic Complex in Troms, Northern Norway. The two magmatic suites of the Lyngen Gabbro strike parallel NNE-SSW, and have distinct magmatic signatures. We define these signatures by using major and trace-element analyses together with selected major- and trace-element mineral analyses and 143Nd/144Nd-isotope whole-rock analyses of gabbroic to tonalitic plutonic rocks from seven detailed cross-sections from this large gabbro-complex. The Western suite of the Lyngen Gabbro precipitated from magma that may have been derived from the same system as the associated volcanic rocks. The gabbros have high An-content (An>90) of their plagioclases relative to co-existing mafic minerals. Together with somewhat high ɛNd(t) values (+6), this implies that the parental magmas were hydrous tholeiites similar to those found in back arc basins today. The Eastern suite, on the other hand, consist of cumulates that were precipitated from melts resembling those of ultra-depleted high-Ca boninitic magmas found in fore-arcs. Extremely high-An plagioclases (An>95) co-exist with evolved mafic minerals and oxides, and the ɛNd(t) values are lower (+4) than in the Western suite. The Eastern suite has no volcanic counterpart, but dikes intersecting the suites have compositions that possibly represent its parental magma. The oceanic Rypdalen Shear Zone generally separates the two suites in the north, but several non-tectonic transitions from boninitic to tholeiitic signatures southwards advocate that the magmatism happened concurrently. The magmatic proximity between the suites, the hydrous magmatism and the absence of a silicic or calc-alkaline mature arc section, suggests that the Lyngen Gabbro formed in the Iapetus Ocean under conditions presently found in incipient arcs later emplaced as outer arc highs.

Document Type: Article
Keywords: Lyngen Gabbro, Ordovician, Incipient Arc
Research affiliation: OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-MUHS Magmatic and Hydrothermal Systems
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1007/s00410-004-0609-8
ISSN: 0930-0708
Date Deposited: 24 Feb 2009 10:50
Last Modified: 20 Mar 2017 13:20
URI: http://oceanrep.geomar.de/id/eprint/1260

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...