Pregled bibliografske jedinice broj: 185084
Dinarides, still unexplored opportunities
Dinarides, still unexplored opportunities // AAPG European Region Conference with GSA / AAPG (ur.).
Prag: AAPG European Region Conference with GSA, 2004. str. 1-5 (poster, međunarodna recenzija, sažetak, znanstveni)
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Naslov
Dinarides, still unexplored opportunities
Autori
Hrvatović, Hazim ; Tari, Vlasta
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
AAPG European Region Conference with GSA
/ AAPG - Prag : AAPG European Region Conference with GSA, 2004, 1-5
Skup
AAPG European Region Conference with GSA
Mjesto i datum
Prag, Češka Republika, 10.10.2004. - 13.10.2004
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Dinarides; petroleum exploration; coastal Croatia; source potential
Sažetak
Petroleum exploration in the Dinarides has been carried out from 60’ to 80’ of the last century, encouraged by widespread occurrence of oil seeps and bituminous rocks. Despite 22 drilled wells no discoveries have yet been made, mostly because of structural complexity and lithological uniformity (carbonates) which limit seismic quality. Source potential (TOC, pyrolysis and kerogen type analysis) exists in Upper Permian (20% TOC, Type II oil-prone kerogen, post-mature), Middle Triassic (Type II oil-prone kerogen, late-mature), Upper Jurassic (about 10% TOC Type I/II oil-prone kerogen early-mature) and Upper Cretaceous (Type I oil-prone kerogen, low-mature to immature). The maturity studies have shown that Permian to Late Jurassic source rocks attained their maximum burial conditions/migration prior to Eocene main compression phase and Miocene relaxation. The originally trapped hydrocarbons escaped either by faulting or tilting of the structures. There is a little chance to locate original traps with negligible spillage. However, the perception of migration and entrapment history combined with play concepts (reservoirs and seals) leads to designation of two most prospective exploration zones in the Dinarides: a) imbricated thrust series in “ shallow” external zone (coastal Croatia), which are stacked at their tops and merging with the sole fault at the bases and b) subthrust structures, as footwall anticlines and duplexes, of interior part of the External Dinarides thrust (south-western Bosnia and Hercegovina).
Izvorni jezik
Engleski
Znanstvena područja
Geologija