GSA Annual Meeting, November 5-8, 2001

Paper No. 0
Presentation Time: 4:15 PM

PROVENANCE OF SUBDUCTED OCEANIC SEDIMENTS IN THE UHP TERRAINS OF THE WESTERN ALPS


MAHLEN, Nancy J., Department of Geology and Geophysics, Univ of Wisconsin, Weeks Hall, 1215 W. Dayton Street, Madison, WI 53706-1692 and JOHNSON, Clark M., Department of Geology and Geophysics, Univ of Wisconsin, Madison, WI 53706, mahlen@geology.wisc.edu

Rare Earth Element (REE) concentrations and Nd-isotope compositions are used to constrain pre-collision Tethys paleogeography in the Alpine orogen. The metasedimentary protoliths are manganese-rich, pelagic deep-sea sediments that were deposited during Jurassic/Early Tertiary divergence of the neoTethys ocean and subsequently underwent ultra-high-pressure metamorphism during Eocene subduction. The relative immobility of REEs and resistance of Sm-Nd fractionation during erosion, re-deposition, or metamorphism make the Nd-isotope system well-suited for provenance determination in high-grade metasedimentary rocks. Isotopic and REE data can be broken into three provenance groups: 1) An old upper continental crust source is suggested for the first set (Group 1) based on overall REE patterns, including flat but depleted HREE trends, Eu/Eu*=0.65, and (Sm/Nd)N=0.57. Group 1 samples yield TCHUR of 1.16 to 1.38 Ga and present-day epsilon Nd of -12.5 to -14.8. 2) Mixed provenance of old upper continental crust including recycled crust and juvenile mafic material is indicated for a second suite (Group 2). These samples have lower concentrations of LREE and HREE than Group 1, Eu/Eu* from 0.57 to 0.73, and (Sm/Nd)N varying from 0.61 to 0.66. Group 2 samples have TCHUR of 0.82 to 1.01 Ga and present-day epsilon Nd varying from -7.8 to -8.8. 3) An oceanic crustal source is suggested for the third set (Group 3), based on REE patterns that are similar to MORB, including depleted LREE and enriched HREE relative to LREE, Eu/Eu*=0.95, and (Sm/Nd)N=0.9988. Nd isotope data provide no TCHUR age solutions due to the high present-day epsilon Nd of +8.1. Source terrains during neoTethys divergence included European crust and African/Adriatic crust. These crustal sources are represented as various nappes in the Western Alps and are currently being studied as controls for provenance determination.