analisi dei parametri ipocentrali del terremoto del friuli del 6 maggio 1976

Clicks: 190
ID: 150469
2010
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This article has not been analysed, so there is no overall score — reader engagement is measured and shown alongside.
AI Quality Assessment
Not analyzed
Readership in this journal
Steady

Ranked #83 of 205 articles by views in desalination

Most read Least read

Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 205 in total.

Mint this article as an NFT
Not yet minted

Create a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.

5 SUSD one-off · no wallet required
Abstract
The hypocentral parameters to t0, φ0, λ0, h0, for the main shock occurred in Friuli on May 6th 1976 and itsfore shock were determined by the first arrival method. The computation was tried employing travel-time curves for different crustal models. The results show a very low influence of the travel-time curves on epicentral coordinates, whose error is essentially dependent on the precision of station data. The focal depth, on the contrary, is a parameter directly connected to the model used in the computation, so, if the model is not accurately known, the indetermination can be of the same order of magnitude as the crust thickness, even using very precise recorded data.
Reference Key
gasparini2010annalsanalisi Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;Calvino Gasparini;Rodolfo Console
Journal desalination
Year 2010
DOI
10.4401/ag-4657
URL
Keywords

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

No comments yet. Be the first to comment on this article.