Abstract
The Al-Amar fault, one of the most important geological features of the E corner of the Arabian Shield, separates a dominantly metavolcanic sequence overlying gneissis granodiorite of the basement to the E, from an essentially metasedimentary sequence to the W. Intrusive rocks of the region include: grabbro, diorite, granodiorite, and alkalic granite. The Al-Amar- Idsas region, evaluated in the light of the plate tectonic theory, appears to represent a continental volcanic arc and a contiguous back-arc basin. -Author
| Original language | English |
|---|---|
| Title of host publication | Evolution and mineralization of the Arabian-Nubian Shield. Proc. symposium, Vol 2 |
| Editors | S.A. Tahoun |
| Publisher | Pergamon Press for King Abdulaziz University, Jeddah, Institute of Applied Geology; I.A.G. Bulletin 3 |
| Pages | 29-40 |
| Number of pages | 12 |
| State | Published - 1979 |
ASJC Scopus subject areas
- General Earth and Planetary Sciences
- General Environmental Science
Fingerprint
Dive into the research topics of 'Geology of the Al-Amar-Idsas region of the Arabian Shield.'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver