ORCID Profile
0000-0002-1138-4527
Current Organisation
Washington State University
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Publisher: Elsevier BV
Date: 08-2020
Publisher: Elsevier BV
Date: 2020
Publisher: Elsevier BV
Date: 2023
Publisher: Geological Society of America
Date: 25-02-2022
DOI: 10.1130/GES02430.1
Abstract: Combined Hf-O isotopic analyses of zircons from tuffs and lavas within the Sierra Madre Occidental (SMO) silicic large igneous province are probes of petrogenetic processes in the lower and upper crust. Existing petrogenetic and tectonomagmatic models erge, having either emphasized significant crustal reworking of hydrated continental lithosphere in an arc above the retreating Farallon slab or significant input of juvenile mantle melts through a slab window into an actively stretching continental lithosphere. New isotopic data are remarkably uniform within and between erupted units across the spatial and temporal extent of the SMO, consistent with homogeneous melt production and evolution. Isotopic values are consistent with enriched mantle magmas (80%) that assimilated Proterozoic paragneisses (~20%) from the lower crust. δ18Ozircon values are consistent with fractionation of mafic magma and not with assimilation of hydrothermally altered upper crust, suggesting that the silicic magmas evolved at depth. Isotopic data agree with previous interpretations where voluminous juvenile melts entered the lithosphere during the transition from a continental arc experiencing slab rollback (Late Eocene) to the arrival of a subducting slab window (Oligocene and Early Miocene) and failure of the upper plate leading to the opening of the Gulf of California (Late Miocene). An anomalously large heat flux and extension of the upper plate allow for the sustained fractionation of the voluminous SMO magmas and assimilation of the lower crust.
Publisher: Elsevier BV
Date: 10-2021
Publisher: American Geophysical Union (AGU)
Date: 12-2017
DOI: 10.1002/2017TC004728
Publisher: Elsevier BV
Date: 04-2018
No related grants have been discovered for Jeff Vervoort.