Journal of Petrology Advance Access published online on October 7, 2008
Journal of Petrology, doi:10.1093/petrology/egn046
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Age and Geochemistry of the Central American Forearc Basement (DSDP Leg 67 and 84): Insights into Mesozoic Arc Volcanism and Seamount Accretion on the Fringe of the Caribbean LIP
1Dynamics of the Ocean Floor, Ifm-Geomar Leibniz-Institut Für Meereswissenschaften, Wischhofstr. 1–3, d-24148 Kiel, Germany
2Fachbereich Geowissenschaften, University of Bremen, Postfach 33 04 40, D-28334 Bremen, Germany
Received February 5, 2008; Revised typescript accepted September 2, 2008
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The igneous forearc basement along the Pacific coast of northern Central America (between southern Mexico and Costa Rica) comprises a highly tectonized accretionary assemblage of igneous and ultramafic rocks. Volcanic and gabbroic rocks with primitive arc geochemical signatures formed between
100 and
180 Ma and are interpreted to have originated by arc magmatism resulting from subduction of the Pacific–Farallon plate. Geochemically enriched ocean island basalt (OIB)-like units are interpreted as accreted seamounts and islands of a hotspot track, which was active between
220 and 100 Ma and originated from a hotspot located in the central Pacific. Based on their combined Pb, Nd and Hf isotopic compositions an affiliation of these rocks with the Caribbean Large Igneous Province or the present-day Galápagos hotspot appears unlikely. Rocks of similar age and geochemistry are exposed on the Santa Elena Peninsula in Costa Rica, suggesting that a similar forearc basement is accreted to the continental Chortis Block from southern Mexico to Costa Rica.
KEY WORDS: Central America; Chortis Block; DSDP; forearc; Pacific margin
*Corresponding author. Present address: IODP, Texas A&M University, 1000 Discovery Drive, College Station, TX 77840, USA. Telephone: +1-979-845-0506. Fax: +1-979-845-0876. E-mail: geldmacher{at}iodp.tamu.edu