DataCite
metadata only
Method of interpreting seismic reflection data in the Vilyui Syncline
The interpretation of observations obtained from geophysical prospecting is complicated in permafrost regions by the low ground temperatures and high ice contents causing higher seismic velocities and electrical resistivities than in thawed strata. This paper deals with seismic surveying in the Vily
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
- (Table 1) Petrographic properties of studied volcanogenic sediments of Unit VI, DSDP Site 89-585#320033
- Apport de la datation absolue aux processus tectoniques et sédimentaires : une approche multi-proxy appliquée aux réservoirs en contextes compressifs et extensifs#301147
- Deciphering the stratigraphic record of rifting and dynamic topography#378107
- The role of seamounts, fluids, and normal faults in slow slip regions: seismological insights from the northern Hikurangi margin#1135819
- Stratigraphic record of an extreme hydro-sedimentary event in steep mountainous environments: a case study in the Roya Valley#68394
Record · ID 1353369
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