Structural evolution, metamorphism and restoration of the Arabian continental margin, Saih Hatat region, Oman Mountains
170 m.y. of relatively stable passive margin sedimentation along the northern continental margin of Arabia was abruptly terminated during the Cenomanian-Turonian (∼95 Ma) when the Oman continental margin collapsed and subsided rapidly (Aruma basin) to accommodate obduction of the Semail ophiolite co...
| Main Authors: | , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2004
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