Petrology and geochemistry of the Cyclops ophiolites (Irian Jaya, East Indonesia): Consequences for the Cenozoic evolution of the north Australian ... View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1999-03

AUTHORS

C. Monnier, J. Girardeau, M. Pubellier, M. Polvé, H. Permana, H. Bellon

ABSTRACT

The Cyclops massif (Irian Jaya - Western Indonesia) displays all components of an ophiolitic sequence including residual mantle peridotites (harzburgites and dunites), cumulate gabbros, dolerites, normal mid-oceanic ridge basalts (N-MORB) and minor amounts of boninitic lavas. This ophiolitic series tectonically overlies high temperature (HT)-high pressure (HP) mafic rocks metamorphosed during the Miocene. Mineral chemistry and bulk rock rare-earth element (REE) abundances of the peridotites are characteristic of highly residual mantle rocks. The high Cr# [Cr#=100*Cr/(Cr+Al)] of spinel (up to 60) and very low heavy rare-earth element (HREE) concentrations of peridotites (< 0.1 time the chondritic values) are in agreement with residues of 25 to 35% melting as expected for peridotites from supra-subduction zone environments. Ti-enrichments in spinels and secondary clinopyroxenes (up to 1%, and 0.5%, respectively) are likely a consequence of reaction between mantle-derived melts and the host peridotites. High light rare-earth element (LREE) concentrations reaching up to chondritic values and high field strength element (HFSE) anomalies suggest that the initial composition of the residual peridotites has been previously modified by the passage of boninitic melt(s). The associated basalts and related cumulate rocks display major and trace element contents with Nb-negative anomalies typical of back-arc magmas. New40K/40Ar isotopic ages obtained from the back-arc basin basalts (BABB - 29 Ma) and boninites (43 Ma) combined with the geochemical signatures of the rocks studied here, indicate that the Cyclops Mountains may have formed in a single suprasubduction environment. This implies southward plunging subduction of the Australian oceanic lithosphere beneath the northern part of the Australian margin. The ultramafic rocks and related lavas (boninites) likely formed during the Eocene in a forearc environment, before their southward obduction onto the island arc crustal welt during the early Miocene. The Pliocene back-thrusting event has led to the slicing of the backarc basin series onto the arc and fore-arc sequences. More... »

PAGES

1-28

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/bf01161574

DOI

http://dx.doi.org/10.1007/bf01161574

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1048874200


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