GASTIME

GAS SEEPS AND SUBMARINE SLIDES IN THE EASTERN MEDITERRANEAN: TOWARD COMPREHENSIVE GEOHAZARD PREVENTION

 Coordinatore UNIVERSITY OF HAIFA 

 Organization address address: "Mount Carmel, Abba Khoushi Blvd."
city: HAIFA
postcode: 31905

contact info
Titolo: Mrs.
Nome: Iris
Cognome: Levi
Email: send email
Telefono: +972 4 8288485

 Nazionalità Coordinatore Israel [IL]
 Totale costo 100˙000 €
 EC contributo 100˙000 €
 Programma FP7-PEOPLE
Specific programme "People" implementing the Seventh Framework Programme of the European Community for research, technological development and demonstration activities (2007 to 2013)
 Code Call FP7-PEOPLE-2011-CIG
 Funding Scheme MC-CIG
 Anno di inizio 2012
 Periodo (anno-mese-giorno) 2012-05-01   -   2016-04-30

 Partecipanti

# participant  country  role  EC contrib. [€] 
1    UNIVERSITY OF HAIFA

 Organization address address: "Mount Carmel, Abba Khoushi Blvd."
city: HAIFA
postcode: 31905

contact info
Titolo: Mrs.
Nome: Iris
Cognome: Levi
Email: send email
Telefono: +972 4 8288485

IL (HAIFA) coordinator 100˙000.00

Mappa


 Word cloud

Esplora la "nuvola delle parole (Word Cloud) per avere un'idea di massima del progetto.

reservoirs    seepage    mechanisms    salt    hydrocarbon    recovery    boreholes    basins    mass    shaping    fluid    slope    hazard    stability    prone    messinian    eastern    geological    basin    mediterranean    gas    sedimentary    levantine    depths   

 Obiettivo del progetto (Objective)

'The objectives of this proposal are to study the shaping mechanisms behind gas seepage and slope stability in the Levantine basin (eastern Mediterranean), and to understand the geological forces shaping and controlling sedimentary basins under similar conditions. Fluid escape features and mass transport deposits are common in hydrocarbon-prone basins. Thus, studying the relationship between these features in the Levantine basin is crucial for hazard assessment and risk mitigation for safe hydrocarbon recovery. Massive hydrocarbon reservoirs have recently been discovered in the, up to now, under-explored Levantine basin. Wells and boreholes show high quality gas trapped in lower Miocene sandstones at water depths over 1500 m. The estimated amount of gas in place for these fields is world class: with 25 trillion cubic feet. These giant sub-Messinian salt gas discoveries in the Levantine basin were considered, at the time of their finding, the largest of the last decade, thus bringing the eastern Mediterranean into the limelight. Israel’s energy sector is set to undergo significant changes that could transform the country into an exporter of natural gas. Increasing numbers of offshore constructions including undersea pipelines and oil rigs in relation to the development of these hydrocarbon reservoirs, require detailed hazard assessments. Gaining reliable data about frequency, causes and consequences of mass movements and their interplay with gas seepage is imperative prior to successful recovery and development of these fields. The presence of fluid flow signatures piercing deep Messinian salt layers and reaching shallower depths requires the implementation of a comprehensive geological study of the Levantine basin based on the interpretation of 2D and 3D surveys, coupled by information retrieved from boreholes and sedimentary cores. This exercise serves as a solid basis to understand the mechanisms controlling slope stability in hydrocarbon-prone sedimentary basins.'

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