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Middle Tertiary near-trench volcanism from ridge-trench collisions along west-central California: Implications from Nd, Sr-isotopic and REE data

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:6137539
;  [1]
  1. Univ. of Rochester, NY (United States). Dept. of Geological Sciences
Early Miocene near-trench bimodal volcanism in the Santa Maria Province (SMP) of west-central California occurred when segments of the East Pacific Rise collided with a subduction zone along western North America. These ridge-trench interactions resulted in the transition from subduction to transform tectonic regimes along the California continental margin. The Nd, Sr-isotopic and trace element geochemical data for the SMP volcanic rocks indicate a depleted mantle (mid-ocean ridge basalt/MORB) source of magma. The basalts are mildly enriched in light rare earth elements (LREE) with La/Ce (n) = 0.9 to 1.2 and Ce/Yb (n) = 1.8 to 2.6. Basaltic andesites show moderate LREE enrichment with La/Ce (n) = 1.0 to 1.4 and Ce/Yb (n) = 2.2 to 3.4, and rhyolites/dacites exhibit strong LREE enrichment of La/Ce (n) = 1.1 to 1.3 and Ce/Yb (n) = 3.8 to 7.1. These data for the SMP volcanic rocks are analogous to MORB isotopic signatures from modern and young oceanic spreading ridges, including the East Pacific Rise, and indicate a MORB source of magma. This magma erupted to form basalts and also assimilated and partially melted local Jurassic-Cretaceous sedimentary and metasedimentary basement rocks to form rhyolites and dacites. The data indicates that SMP volcanism occurred when a depleted mantle reservoir of MORB was juxtaposed beneath the continental margin with the approach of the East Pacific Rise and was rapidly erupted during a phase of crustal extension/transtension and basin development. The results of this study clearly document that mid-ocean ridge and trench interactions can provide a unique tectonomagmatic setting for plate margin volcanism.
OSTI ID:
6137539
Report Number(s):
CONF-921058--
Conference Information:
Journal Name: Geological Society of America, Abstracts with Programs; (United States) Journal Volume: 24:7
Country of Publication:
United States
Language:
English

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