Putting some time on the orogeny periods/episodes:
Yavapai orogeny 1710–1680 Mya
Mazatzal orogeny at 1650–1600 Mya
Picuris orogeny at 1450–1300 Mya
https://en.wikipedia.org/wiki/Picuris_orogeny (at least a couple of typos on dates in this article)
Cites:
https://pubs.geoscienceworld.org/gs...nic-model-for-the-Proterozoic-growth-of-North
Grenville orogeny at 1300–950 Mya
https://en.wikipedia.org/wiki/Grenville_orogeny (or 1250–980 Ma)
Sveconorwegian orogeny 1140 to 960 million years ago
https://en.wikipedia.org/wiki/Sveconorwegian_orogeny
Ostensibly, whatever 'mountains' formed eroded relatively quickly. I wonder what the climate/weather was like during those periods and how it varied between summer and winter.
Bear in mind that what became the continents today were probably thousands of miles away from present positions. According to some simulations, there was very little, if any, dry land in the norther hemisphere, and as I recall, oceans/seas were relatively shallow.
Plate tectonic evolution from 1 Billion years ago to the present.
from -
https://singularityhub.com/2021/02/...illion-year-dance-of-Earth's-tectonic-plates/
Andrew S. Merdith, Simon E.Williams, Alan S.Collins, Michael G.Tetley, Jacob A.Mulder, Morgan L. Blades, Alexander Young, Sheree E. Armistead, John Cannon, Sabin Zahirovic, R. Dietmar Müller, "Extending full-plate tectonic models into deep time: Linking the Neoproterozoic and the Phanerozoic," Earth-Science Reviews Volume 214, March 2021, 103477
https://www.sciencedirect.com/science/article/pii/S0012825220305237
Animation of plate tectonics 540 Ma to present
https://www.earth.northwestern.edu/our-people/affiliated-faculty/scotese-christopher.html
Consider -
https://www.sciencedirect.com/science/article/pii/S0024493720305259
R. Tamblyn, D. Brown, M. Hand, L. Morrissey, C. Clark, R. Anczkiewicz
"The 2 Ga eclogites of Central Tanzania: Directly linking age and metamorphism," Lithos
Volumes 380–381, January 2021, 105890
https://en.wikipedia.org/wiki/Eclogite
Also, note that geological situation in what is now Gabon, Africa about 1.7 billion years ago (sandstone over granite).
https://en.wikipedia.org/wiki/Natural_nuclear_fission_reactor
A key factor that made the reaction possible was that, at the time the reactor went
critical 1.7 billion years ago, the fissile isotope
235U made up about 3.1% of the natural uranium, which is comparable to the amount used in some of today's reactors. (The remaining 96.9% was non-fissile
238U.) Because
235U has a shorter half-life than
238U, and thus decays more rapidly, the current abundance of
235U in natural uranium is about 0.70–0.72%.
Note that europium is a fission product (more so from fast fission) as well as a transmutation (n-capture) of samarium (also a fission product). About 800 million years ago, the enrichment of natural U would have been reduced to something like 1.4 to 1.5% from about 3.1% (it might have been 3.3-3.4% at 1.7 billion years).
I'd be interested to learn the origin of the zircon specimens. In another paper, it mention zircons from Tibet.