DigitalCommons@USU
metadata only
Sedimentation and Paleogeography of an Eocene to Oligocene Rift Zone, Idaho and Montana
Examination of sedimentary basins in east-central Idaho and analysis of previous work in western Montana indicate that late middle Eocene to Oligocene extension north of the eastern Snake River Plain was confined to a north- to north-northwest-trending rift zone, 100 ±25 km wide. In east-central Ida
Conceptio Open Archive
Analyze & explore related research in Conceptio
Connect this record directly into your research workflow or AI agent. Explore citations across open repositories, query full text, and export structured proof bundles.
This document is indexed with metadata only: full text is not available in the archive for this record. Open the official source ↗
Related documents
- Long-Distance Longitudinal Transport of Gravel Across the Cordilleran Thrust Belt of Montana and Idaho#1089354
- Rapid Extension in an Eocene Volcanic Arc: Structure and Paleogeography of an Intra-Arc Half Graben in Central Idaho#1141214
- Upper Cretaceous strata in the Powder River Basin—Formation tops database, structure and thickness contour maps, and associated well data#435467
- Paleogeographic and Paleotectonic Setting of Laramide Sedimentary Basins in the Central Rocky Mountain Region#1089352
- Controls on Sediment Transport and Storage in the Little Snake, Yampa, and Green Rivers in the Vicinities of Dinosaur National Monument and Ouray National Wildlife Refuge, Colorado and Utah, with Implications for Fish Habitat in the Middle#621764
Record · ID 1089359
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Bring this data into your agent: Connect via MCP or API · 20 free credits to start · no card required
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive