Constraints on the timing and duration of orogenic events by combined Lu–Hf and Sm–Nd geochronology: An example from the Grenville orogeny

Author:

Johnson Thomas A.,Vervoort Jeffrey D.ORCID,Ramsey Molly J.,Aleinikoff John N.,Southworth Scott

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference68 articles.

1. U–Pb geochronology of zircon and monazite from Mesoproterozoic granitic gneisses of the northern Blue Ridge, Virginia and Maryland, USA;Aleinikoff;Precambrian Res.,2000

2. SHRIMP U–Pb ages of zircon and monazite, and garnet Lu–Hf ages in anorthosite of the Marcy massif, Adirondack Highlands, NY: recognizing inherited, igneous, and metamorphic components;Aleinikoff;Abstr. Program – Geol. Soc. Am.,2018

3. Hotspots, polar wander, Mesozoic convection and the geoid;Anderson;Nature,1982

4. Slow cooling of deep crustal granulites and Pb-loss in zircon;Ashwal;Geochim. Cosmochim. Acta,1999

5. Sr and Nd isotope geochronology, geologic history, and origin of the Adirondack Anorthosite;Ashwal;Geochim. Cosmochim. Acta,1983

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