An examination of inclusion assemblages in Hadean zircons from Jack Hills (Western Australia) is presented, which constrain the magmatic formation conditions to about 700 °C and 7 kbars. This result implies a near-surface heat flow about 3–5 times lower than estimates of global Hadean heat flow. As the only site of magmatism on modern Earth that is characterized by heat flow of about one-quarter of the global average is above subduction zones, it is suggested that the magmas from which the Jack Hills Hadean zircons crystallized were formed largely in an underthrust environment, perhaps similar to modern convergent margins.
- Michelle Hopkins
- T. Mark Harrison
- Craig E. Manning