![Quantification of risks associated with seabed instability at Ormen Lange [An article from: Marine and Petroleum Geology]](https://www.ebooknetworking.net/books/B00/0RR/bigB000RR3RRY.jpg)
Quantification of risks associated with seabed instability at Ormen Lange [An article from: Marine and Petroleum Geology]
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Book Details
Author(s)
F. Nadim, T.J. Kvalstad, T. Guttormsen
Publisher
Elsevier
ISBN / ASIN
B000RR3RRY
ISBN-13
978B000RR3RR3
Marketplace
France 🇫🇷
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Description
This digital document is a journal article from Marine and Petroleum Geology, published by Elsevier in 2005. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.
Description:
The Ormen Lange gas field is located within the slide scar of the enormous Storegga Slide that took place about 8200 years ago. There are strong indications that the Storegga slide generated a tsunami wave hitting the coastlines of Norway, Scotland and the Faeroes. The headwalls of the Storegga slide are steep and their safety factor against sliding could be low. An extensive study was therefore performed to evaluate the probability for new submarine slides and their potential consequences. Results of the study showed that the 1st party and 3rd part risks associated with potential slide activity in the Ormen Lange area are negligible.
Description:
The Ormen Lange gas field is located within the slide scar of the enormous Storegga Slide that took place about 8200 years ago. There are strong indications that the Storegga slide generated a tsunami wave hitting the coastlines of Norway, Scotland and the Faeroes. The headwalls of the Storegga slide are steep and their safety factor against sliding could be low. An extensive study was therefore performed to evaluate the probability for new submarine slides and their potential consequences. Results of the study showed that the 1st party and 3rd part risks associated with potential slide activity in the Ormen Lange area are negligible.
