The Cornell Oman Project provides geophysical data focused on the Semail Ophiolite, considered the Earth's best type-example of an ophiolite complex. It was created by SCIOPS using diversified geophysical and seismologic databases to map the shallow and deep crustal structure of the Oman Mountains. The project specifically aimed to define the geometry of the basement, the Moho, and the subsurface geometry of the ophiolite.
Use Cases
- Modeling subsurface crustal geometry based on geophysical mapping techniques mentioned in the description
- Analyzing the relationship between surface geology and deep structure in an ophiolite setting
- Studying the tectonic setting of the Oman Mountains using integrated geophysical data
Strengths
- Focuses on the Semail Ophiolite, described as the Earth's best type-example of an ophiolite complex.
- Integrates multiple geophysical and seismologic databases and techniques for mapping.
Limitations
- Column-level documentation is absent; field semantics must be inferred after download.
- Row count is unknown, which may limit suitability assessment.
- Last update date is unknown; freshness unverified.
Provenance
- Source
- SCIOPS
- Collection Method
- Used diversified geophysical and seismologic databases and techniques.
- Time Range
- unknown
- Freshness
- Last update date is unknown; freshness unverified.
- Geography
- Oman Mountains