LSU Digital Commons
metadata only
The Case for Ice Rises at Ross Bank since the Middle Miocene
Many tens of ice rises exist at the marine margins of the Antarctic Ice Sheet. Isle-type ice rises in particular are those where an ice shelf is pinned to an underlying submarine bank. Recent and ongoing studies show that Ross Bank, on the middle continental shelf of central Ross Sea, was the former
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
- The under-ice habitat constitutes a critical survival hub for zooplankton in the Central Arctic Ocean#4952
- Documenting Arctic Sea Ice Dynamics with Global Fiducials Program Imagery#621626
- Compression and expansion index and void ratio of samples from Lomonosov Ridge and Yermak Plateau#1121166
- ICESat-2 land ice products resolve Greenland and Antarctic ice-sheet height changes on seasonal to multiyear time scales.#420933
- Biogeochemical investigation of Basiluzzo CO2 vents (Panarea, Italy) during ECO2 cruises from 2011-2013#1121187
Record · ID 823306
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