Geochemical Evidence for Diachronous Uplift and Synchronous Collapse of the High Elevation Variscan Hinterland

Ian W. Hillenbrand, Michael L. Williams

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DOI: 10.1029/2022gl100435
Published: 2022-11-07
Container: Geophysical Research Letters
Publisher: American Geophysical Union (AGU)
Open access: unknown

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Cite this work

BibTeX

@article{allodium:10.1029/2022gl100435,
  title = {Geochemical Evidence for Diachronous Uplift and Synchronous Collapse of the High Elevation Variscan Hinterland},
  author = {Ian W. Hillenbrand and Michael L. Williams},
  year = {2022},
  journal = {Geophysical Research Letters},
  doi = {10.1029/2022gl100435},
  url = {https://doi.org/10.1029/2022gl100435}
}

RIS

TY  - JOUR
TI  - Geochemical Evidence for Diachronous Uplift and Synchronous Collapse of the High Elevation Variscan Hinterland
AU  - Ian W. Hillenbrand
AU  - Michael L. Williams
PY  - 2022
JO  - Geophysical Research Letters
DO  - 10.1029/2022gl100435
UR  - https://doi.org/10.1029/2022gl100435
ER  -

APA

Hillenbrand, I. W., & Williams, M. L. (2022). Geochemical Evidence for Diachronous Uplift and Synchronous Collapse of the High Elevation Variscan Hinterland. Geophysical Research Letters. https://doi.org/10.1029/2022gl100435

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crossref · retrieved 2026-09-26T10:51:31.281Z