Age and provenance of Grenville supergroup rocks, Trans-Adirondack Basin, constrained by detrital zircons
Author:
Publisher
Geological Society of America
Subject
Geology
Link
http://pubs.geoscienceworld.org/geology/article-pdf/43/2/183/3548080/183.pdf
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2. SHRIMP study of zircons from Early Archean rocks in the Minnesota River Valley: Implications for the tectonic history of the Superior Province;Bickford;Geological Society of America Bulletin,2006
3. Revision of Grenville stratigraphy and structure in the Balmat-Edwards District, northwest Adirondacks, New York;Brown;Geological Society of America Bulletin,1956
4. Shawinigan arc magmatism in the Adirondack Lowlands as a consequence of closure of the Trans-Adirondack backarc basin;Chiarenzelli;Geosphere,2010
5. Tectonic implications of the discovery of a Shawinigan ophiolite (Pyrites Complex) in the Adirondack Lowlands;Chiarenzelli;Geosphere,2011
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1. Provenance and depositional age of metasedimentary rocks in the Frontenac terrane (Grenville Province, Ontario);Canadian Journal of Earth Sciences;2024-04-25
2. Zircon U-Pb-Hf isotope evidence for juvenile Penokean sources (ca. 1.9 Ga) in the SW Grenville Province;Lithos;2023-12
3. Xenocrystic zircon in Central New York State Kimberlites record Neoproterozoic disturbance of Grenville Basement rocks;Lithos;2023-11
4. Varicolored Marble in the Central Metasedimentary Belt, Grenville Supergroup. I. Circumstantial Evidence of Melting;The Canadian Journal of Mineralogy and Petrology;2023-07-01
5. Neodymium isotope mapping a polygenetic TTG batholith: failed back-arc rifting in the Central Metasedimentary Belt, southwestern Grenville Province;Canadian Journal of Earth Sciences;2022-02
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