Sr, Nd, and Pb isotope geochemistry of ODP Hole 104-642E, supplement to: Taylor, Paul N; Morton, Andrew C (1989): Sr, Nd, and Pb isotope geochemistry of the upper and lower volcanic series at Site 642. In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 429-435

ODP Leg 104 recovered 914 m of volcanics at Site 642 on the Vøring Plateau in the Norwegian Sea. The upper series of these volcanics correlates with seaward-dipping seismic reflectors (DRS), and is tholeiitic in character. The lower series underlies the DRS and is broadly andesitic in character. Rb-...

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Bibliographic Details
Main Authors: Taylor, Paul N, Morton, Andrew C
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 1989
Subjects:
Drilling/drill rig
Leg104
Joides Resolution
Ocean Drilling Program ODP
Morton
Norwegian Sea
Vøring Plateau
Online Access:https://dx.doi.org/10.1594/pangaea.737407
https://doi.pangaea.de/10.1594/PANGAEA.737407
Description
Summary:ODP Leg 104 recovered 914 m of volcanics at Site 642 on the Vøring Plateau in the Norwegian Sea. The upper series of these volcanics correlates with seaward-dipping seismic reflectors (DRS), and is tholeiitic in character. The lower series underlies the DRS and is broadly andesitic in character. Rb-Sr, Sm-Nd, and Pb isotopic analyses show that upper series samples have isotopic features characteristic of MORB, except for one dike sample that has a Pb isotopic composition that may indicate interaction of its parent magma with older continental crust. The five most silicic samples from the lower series, which occur high up in the sequence, define a 63 ± 19 Ma Rb-Sr whole-rock isochron age, and have an initial 87Sr/86Sr of 0.7116 ± 0.0004. Other lower series samples have lower initial 87Sr/86Sr, but all are greater than any upper series rock. The combined evidence of initial 87Sr/86Sr, initial epsilon-Nd values, Sm-Nd model ages, Pb isotopic compositions, and petrographic features clearly indicate that lower series rocks were derived, at least in part, from continental crustal source materials. That the DRS is underlain by rocks of continental character is an important observation, constraining models for the development of DRS-type passive continental margins.

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