Variations within individual cratons, as well as across different cratons, are readily apparent at the Earth's surface, providing indirect insight into the processes governing the formation …
Mid‐lithosphere discontinuities are seismic interfaces likely located within the lithospheric mantle of stable cratons, which typically represent velocities decreasing with depth. The …
Lower crustal xenoliths from the Missouri Breaks diatremes and Bearpaw Mountains volcanic field in Montana record a multi-billion-year geologic history lasting from the …
C Heckel, AB Woodland, J Linckens… - Journal of …, 2022 - academic.oup.com
Sheared peridotites from the Kaapvaal craton may be broadly divided into two types:(1) high T and refertilized and (2) low T and highly depleted, which equilibrated at conditions lying …
We present constraints on the hydration state and rheology of the lithospheric mantle beneath the North Anatolian fault zone (NAFZ). Peridotite xenoliths from the Biyikali and …
CT Lee, EJ Chin - Earth and Planetary Science Letters, 2023 - Elsevier
The mid-Archean to mid-Proterozoic appears to have favored the formation of cratons, stable crustal shields underlain by unusually thick and cold mantle roots. Most of these cratons and …
New zircon and titanite U-Pb and trace-element data from minette-and kimberlite-hosted lower crustal xenoliths from near the northern margin of the Wyoming craton document …
Y Shao, C Liu, R Gao, S Li, T Zhao - Tectonics, 2025 - Wiley Online Library
The large‐volume lithospheric mantle xenoliths around the Damaping area provides valuable insights into the detailed destruction progression of the North China Craton (NCC) …
Abstract Knowledge of the water capacity of the deep lithosphere is crucial for validating models of craton growth and for constraining solid earth volatile cycles over geologic time …