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Organic geochemical signatures of the Upper Miocene (Tortonian—Messinian) sedimentary succession onshore Crete Island, Greece: implications for hydrocarbon prospectivity

Maravelis Angelos, Kontakiotis, George, Bellas Spyridon, Antonarakou, Assimina, Botziolis Chrysanthos, Janjuhah Hammad Tariq, Makri Panayota, Moissette, Pierre, Cornée, Jean-Jacques, Pasadakis Nikos, Manoutsoglou Emmanouil, Zelilidis, Avraam, Karakitsios, Vassilis, 19..-

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URIhttp://purl.tuc.gr/dl/dias/C92F43F0-1CED-4EFB-9F54-9AB298B14D88-
Αναγνωριστικόhttps://doi.org/10.3390/jmse10091323-
Αναγνωριστικόhttps://www.mdpi.com/2077-1312/10/9/1323-
Γλώσσαen-
Μέγεθος16 pagesen
ΤίτλοςOrganic geochemical signatures of the Upper Miocene (Tortonian—Messinian) sedimentary succession onshore Crete Island, Greece: implications for hydrocarbon prospectivityen
ΔημιουργόςMaravelis Angelosen
ΔημιουργόςKontakiotis, Georgeen
ΔημιουργόςBellas Spyridonen
ΔημιουργόςΜπελλας Σπυριδωνel
ΔημιουργόςAntonarakou, Assiminaen
ΔημιουργόςBotziolis Chrysanthosen
ΔημιουργόςJanjuhah Hammad Tariqen
ΔημιουργόςMakri Panayotaen
ΔημιουργόςMoissette, Pierreen
ΔημιουργόςCornée, Jean-Jacquesen
ΔημιουργόςPasadakis Nikosen
ΔημιουργόςΠασαδακης Νικοςel
ΔημιουργόςManoutsoglou Emmanouilen
ΔημιουργόςΜανουτσογλου Εμμανουηλel
ΔημιουργόςZelilidis, Avraamen
ΔημιουργόςKarakitsios, Vassilis, 19..-en
ΕκδότηςMDPIen
ΠερίληψηThe definition of pre-Messinian source rocks in the eastern Mediterranean is of paramount importance for hydrocarbon exploration because of the ability of salt to act as a high-quality seal rock. This research evaluates the organic geochemical features of the Upper Miocene (Tortonian—Messinian) sedimentary succession onshore Crete Island, Greece. The study employs original (Messinian, Agios Myron Fm) and published (Tortonian, Viannos Fm, Skinias Fm, Moulia Fm, and Messinian Ploutis section) results from organic geochemical analyses of mudstone samples. One hundred and one samples were examined using standard organic geochemistry methodology (Rock-Eval II and VI-TOC) to define the origin, type, and degree of organic matter maturity. The data indicate that the studied samples have poor to fair gas-prone source rock potential. These possible source rock units have not experienced great temperatures during burial, and, thus, their organic matter is thermally immature. The sub-salt (Tortonian—Messinian) source rock units are likely to be of higher thermal maturity in the western and eastern south Cretan trenches because of tectonic subsidence and a thicker sedimentary overburden. Several traps can grow in these regions, associated with normal faults, rotated blocks and unconformities (both below and above the unconformities). This research provides a basis for the further evaluation of the hydrocarbon potential in Crete Island. It is an area that shares geological similarities with the surrounding regions that contain proven reserves and is of crucial economic and strategic importance.en
ΤύποςPeer-Reviewed Journal Publicationen
ΤύποςΔημοσίευση σε Περιοδικό με Κριτέςel
Άδεια Χρήσηςhttp://creativecommons.org/licenses/by/4.0/en
Ημερομηνία2023-10-12-
Ημερομηνία Δημοσίευσης2022-
Θεματική ΚατηγορίαRock Eval analysisen
Θεματική ΚατηγορίαPre-evaporitic source rocksen
Θεματική ΚατηγορίαHydrocarbon potentialen
Θεματική ΚατηγορίαSedimentary basin dynamicsen
Θεματική ΚατηγορίαThermal maturityen
Θεματική ΚατηγορίαKerogen typeen
Θεματική ΚατηγορίαHydrocarbon explorationen
Θεματική ΚατηγορίαEvaporites sealing qualityen
Θεματική ΚατηγορίαMessinian salinity crisisen
Θεματική ΚατηγορίαEastern Mediterraneanen
Βιβλιογραφική ΑναφοράA. G. Maravelis, G. Kontakiotis, S. Bellas, A. Antonarakou, C. Botziolis, H. T. Janjuhah, P. Makri, P. Moissette, J.-J. Cornée, N. Pasadakis, E. Manoutsoglou, A. Zelilidis and V. Karakitsios, “Organic geochemical signatures of the Upper Miocene (Tortonian—Messinian) sedimentary succession onshore Crete Island, Greece: implications for hydrocarbon prospectivity,” J. Mar. Sci. Eng., vol. 10, no. 9, Sep. 2022, doi: 10.3390/jmse10091323.en

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