STRUCTURE OF THE INTRAPLATE EASTERN PALMYRIDE FOLD BELT, SYRIA
The Palmyride Fold Belt is an aulacogen within the Arabian plate linked to the Levantine continental margin, which contains >10km of Phanerozoic sediments. Recent field mapping shows that almost all the structures have resulted from a phase of northwest-southwest compression followed by major...
| Päätekijä: | |
|---|---|
| Aineistotyyppi: | Journal article |
| Kieli: | English |
| Julkaistu: |
1994
|