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- Q15240458 subject Q7163793.
- Q15240458 subject Q7288439.
- Q15240458 abstract "The Semail Ophiolite of the Hajar Mountains of Oman and the United Arab Emirates is a large slab of oceanic crust that is made of volcanic rocks and ultramafic rocks from the Earth's upper mantle that was overthrust onto continental crust as an ophiolite. It is located on the eastern corner of the Arabian Peninsula and covers an area of approximately 100,000 km2. Based on uranium-lead dating techniques, the Semail Ophiolite formed in the Late Cretaceous. It is primarily made of silicate rocks with (SiO2) content ranging from 45-77 wt%. The Semail Ophiolite is important because it is rich in copper and chromite ore bodies also provides valuable information about the ocean floor and the upper mantle on land. Geologists have studied the area attempting to find the best model explaining the formation of the Semail Ophiolite.".
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- Q15240458 wikiPageWikiLink Q605396.
- Q15240458 wikiPageWikiLink Q7163793.
- Q15240458 wikiPageWikiLink Q7288439.
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- Q15240458 wikiPageWikiLink Q858571.
- Q15240458 wikiPageWikiLink Q878.
- Q15240458 wikiPageWikiLink Q917402.
- Q15240458 comment "The Semail Ophiolite of the Hajar Mountains of Oman and the United Arab Emirates is a large slab of oceanic crust that is made of volcanic rocks and ultramafic rocks from the Earth's upper mantle that was overthrust onto continental crust as an ophiolite. It is located on the eastern corner of the Arabian Peninsula and covers an area of approximately 100,000 km2. Based on uranium-lead dating techniques, the Semail Ophiolite formed in the Late Cretaceous.".
- Q15240458 label "Semail Ophiolite".