This weathering may result in a slightly increasing trend in 87 Sr/ 86 Sr ratios from the Late Miocene to Pliocene.
← all excerpts
A seven-million-year hornblende mineral record from the central Chinese Loess Plateau.
1
—
—
This weathering may result in a slightly increasing trend in 87 Sr/ 86 Sr ratios from the Late Miocene to Pliocene.