About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The AAPG/Datapages Combined Publications Database
Journal of Petroleum Geology
Abstract
Journal of Petroleum Geology, vol.
INTERACTIONS BETWEEN TECTONIC ACTIVITY
AND EUSTATIC SEA-LEVEL CHANGES IN THE
PINDOS AND MESOHELLENIC BASINS, NW GREECE:
BASIN EVOLUTION AND HYDROCARBON POTENTIAL
P. Avramidis*, A. Zelilidis* +, I. Vakalas* and N. Kontopoulos*
* University of Patras, Department of Geology, 26500 Patras, Greece.
+ author for correspondence: [email protected]
This paper investigates the sedimentological response of the Tertiary Pindos and
Mesohellenic Basins to localized tectonic and eustatic sea-level changes in a submarine
setting dominated by turbidite deposition. Five composite stratigraphic cross
-
sections
were compiled from field data, three in the Pindos Basin and two in the Mesohellenic
Basin; 45 samples were dated by means of nannofossil biostratigraphy. On the basis of
these field studies, we relate observed changes in depositional environment to eustatic
sea-level changes and to activity on local thrusts. Between the early Eocene and the late
Miocene, tectonically-driven subsidence in both basins was generally more significant
than eustatic variations in controlling depositional patterns. However, depositional
conditions can be related to eustatic changes at four specific times:
(i) late Eocene submarine fans and deltaic or fan-delta deposits in the Mesohellenic
Basin can be related to a sea-level rise (NP17) and subsequent fall (NP18-19),
respectively;
(ii) the development of submarine fans in both basins during the early to middle
Oligocene (NP22-23) can be related to a sea-level rise;
(iii) a late Oligocene (NP24-25) sea-level fall can be related to more restricted
depositional conditions, accompanied by intra-basinal thrusting in the Pindos Basin
and the presence of two indentors in the Mesohellenic Basin;
(iv) a change from deep-water (submarine fan) to shallow-marine deposition during
the late Miocene in the Mesohellenic Basin can be related to a eustatic fall in sea-level.
Standard organic geochemical analyses were carried out on 93 samples from both basins, including Rock-Eval pyrolysis and column and gas chromatography. Preliminary results indicate that the sedimentary sequences in both the Pindos and Mesohellenic Basins may have the potential to generate natural gas.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
Watermarked PDF Document: $14 | |
Open PDF Document: $24 |