Abstract
The Tarr albitite complex of SE Sinai is structurally controlled by two large shear zones and is spatially associated with a tectonically emplaced ophiolitic suite consisting of hornblendite, gabbro, talc-serpentinite and carbonate. Based on un- or partially metasomatized remnants of protoliths throughout albitite bodies, gradational contacts, ghost structures, and other features, the albitite is shown to have originated by Na-metasomatism.-from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 7-22 |
| Number of pages | 16 |
| Journal | Ofioliti |
| Volume | 12 |
| Issue number | 1 |
| State | Published - 1 Jan 1987 |
| Externally published | Yes |
ASJC Scopus subject areas
- Geology