Abstract
Volcano-sedimentary successions, of the Lower and Upper Hovin and Horg Groups (Ordovician to ?Lower Silurian), unconformably overlie a variable substrate which includes fragmented oceanic crust and ensimatic immature arc assemblages initially deformed and metamorphosed in earliest Ordovician times. A compromise model involving an elongate microcontinental plate within the Iapetus is invoked. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 233-244 |
| Number of pages | 12 |
| Journal | Unknown Journal |
| Publication status | Published - 1984 |
| Externally published | Yes |