3D-JewelSuite-Model2.wrl.zip
URL: https://gdr.openei.org/files/793/3D-JewelSuite-Model2.wrl.zip
3D model of the INL site. Model 2 shows the same system of calderas shifted to the south, beyond the boundaries of the GRRA. Here we assume that the boundary between volcanics and Paleozoic rocks is defined by a flexural surface that was formed in response to the emplacement of a dense mid-crustal sill beneath the ESRP. This model is supported by the attitudes of ancient fold hinges within the mountains north of the plain. Fold hinges near the boundary of the plain plunge towards the plain at around 30 degrees. North of the plain, the plunge angles decrease in a more or less uniform manner. Thus, in this model, the base of the volcanic system is defined by a planar feature dipping 30 degrees to the south.
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Additional Information
| Field | Value |
|---|---|
| Data last updated | August 8, 2022 |
| Metadata last updated | November 20, 2025 |
| Created | August 8, 2022 |
| Format | ZIP |
| License | Creative Commons Attribution |
| Datastore active | False |
| Has views | False |
| Id | 284e6bb6-f1e9-4071-b40c-fdf933495edb |
| Mimetype | application/zip |
| Package id | 112bc980-5814-4bbd-a020-6ffc09f0918e |
| Position | 34 |
| State | active |