--> --> Exploring in Structurally Complex Thrust Belt: Southwest Albania Case, by Ballauri, Z. Bega1, P. Meehan, R. Gambini, and W. Klammer, #30011 (2003).

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Exploring in Structurally Complex Thrust Belt: Southwest Albania Case*

By

  1. Ballauri1, Z. Bega1, P. Meehan1, R. Gambini2, and W. Klammer2

 Search and Discovery Article #30011 (2003)

 *Adapted from an extended abstract of presentation at AAPG Hedberg Conference, “Deformation History, Fluid Flow Reconstruction and Reservoir Appraisal in Foreland Fold and Thrust Belts,” May 14-18, 2002, Palermo – Mondello (Sicily, Italy)

1OMV Albanien

2OMV AG

Introduction

Fold and thrust belts are characterized by complex trap geometry; a complex burial and thermal history; a narrow time line between the onset of petroleum generation, migration, and trap development; and a complex history of fill and spill. Most of the time, the available data support several “non-unique solutions.” These different solutions may imply radically different geological models that have different geological risks. 

To unravel the complex structural setting of the Vlora-Corfu sector of the Albanides thrust belt (Southwest Onshore Albania) we have adopted a workflow based on a multidisciplinary approach. The proposed geological model is based on fieldwork regional reconstruction, satellite images, MT data, gravity and magnetic data, and seismic acquisition methodology and parameters which were continuously improved to optimise reflectivity response. The resulting structural model has been further validated using geometrical modelling (3D visualization and cross section balancing techniques), 2D gravity modelling, and the kinematics analysis of the structure using the HCA numerical modelling (Salvini et al., 2002). 

The results represented here are part of the ongoing Southern Albanian program. Exploration in Albania has been limited in the past to the valleys where access and costs were lower than this renewed effort over rougher, higher altitude terrain (Figure 1). OMV Albanien and Hellenic Petroleum are thanked for permission to present data from their recent efforts.

 

 

uIntroduction

uFigure captions

uPaleogeography & structural setting

tVlora Elbasan accommodation zone

tApulian platform buttress

uAcknowledgment

uReferences

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

uIntroduction

uFigure captions

uPaleogeography & structural setting

tVlora Elbasan accommodation zone

tApulian platform buttress

uAcknowledgment

uReferences

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

uIntroduction

uFigure captions

uPaleogeography & structural setting

tVlora Elbasan accommodation zone

tApulian platform buttress

uAcknowledgment

uReferences

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

uIntroduction

uFigure captions

uPaleogeography & structural setting

tVlora Elbasan accommodation zone

tApulian platform buttress

uAcknowledgment

uReferences

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Figure Captions

Figure 1. Main structural elements, SW Albania.

 

Figure 2. Simplified geological cross section across Fterra-Nemercka area, based on seismic lines, S Albania.

Figure 3. Simplified geological cross section across Llogora-Golimbasi area, based on seismic liens, SW Albania.

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Overall Paleogeographic and Structural Setting

The overall structural setting of SW Albania is dominated by the Vlora Elbasan Accommodation Zone and the buttressing effect of the thick and rigid Apulian Platform colliding against the thin and relatively brittle Ionian Sequence.

·        Vlora Elbasan Accommodation Zone (VEAZ) - This outstanding NNE-SSW tectonic feature is accommodating the change in the tectonic setting between the northern and southern areas (Roure et al., 1995; Bakiaj et al. 1992).  The northern area, west of the Kruja platform, is characterized by no thrusting of the carbonate sequence while in the southern zone the carbonates are heavily overthrusted, up to tens of kilometres per thrust (Velaj et al., 1999; Moorkens et al., 1994). This accommodation zone consists of several lateral ramps, more or less connected to form an apparent strike slip zone. This lineation may reflect a paleogeograhic change such as the edge of the thick Triassic evaporitic basin and/or a pre-existing deeply rooted basement fault (Roure et al., 2000).

·        Apulian Platform Buttress – The effect of the Apulian platform buttress can be seen in the western sector of the onshore Albania, south of the VEAZ (Gambini et al., 1996). There, the structural setting of the Ionian sequence reflects the shape of the Apulian platform margin. In this area the paleogeographic reconstruction shows three different sectors of the platform edge. In offshore Albania it runs more or less E-W, turning NNW-SSE from Sazan Island to Himara Town, and finally it connects to a NW-SE oriented intra-platform basin (Himara basin).  The main platform edge and the connected Himara intra-platform basin form a sort of platform embayment where the Corfu thrust could develop relatively undisturbed. These three different sectors of the Apulian platform edge caused three different structural areas. 

·        North and West of Sazan Island (north of VEAZ) the Apulian platform and Ionian basin are relatively undisturbed simply forming the substratum of the Tertiary foredeep (Peri-Adriatic depression).

·        Between Sazan Island and Himara town the Apulian platform collided heavily with the Ionian sequence. In this sector the thick Apulian platform stopped the foreland forward thrusting sequence of the Ionian sediments, promoting out-of-sequence thrusting (Tragjasi Unit).

·        In the southern sector, in the Himara basin the Ionian thrust units are not constrained by the Apulian platform, and they could develop relatively undisturbed.

The structural complexity of the area and lack of a detailed tectono-stratigraphic study prevent detailed reconstruction of the kinematics evolution of the area. However, based on the regional knowledge, two main phases of thrusting can be recognized:

1.      The first phase (Miocene in age) mainly involved the Ionian basinal sediments. It was characterized by a foreland forward thrusting sequence, with structural trends oriented NNW-SSE.

2.      The second phase  (Pliocene in age) involved the Ionian and the Apulian platform. During this phase the Apulian platform acted as a rigid buttress promoting out-of-sequence thrusting. The main axes of the structural trends produced during this phase are oriented NW-SE.

Most of the structures in the study area have been affected by both phases. The outcropping Tragjasi structure shows a multiphase evolution; the northern part of it still shows the older NNW-SSE orientation, while the southern part has been refolded and shows mainly the younger NW-SE trend. The two structural trends are accommodated along the Lapardha zone, a deeply eroded valley oriented NE-SW.

The structural setting generated during the first phase is well illustrated by the Fterra-Nemercka regional seismic line (Figure 2). This line has been acquired on the highly deformed Ionian basinal sediment, but in front of the Corfu Apulian platform embayment (Himara intra-platform basin), in a zone only marginally affected by the Apulian platform buttress. This line shows few well-developed fault-bend folds with few tens of kilometers of displacement along each thrust fault.

The buttressing effect and the development of the major out-of-sequence thrusting is well illustrated south of Vlora town along the Llogora-Golimbasi regional line (Figure 3). The western portion of this line illustrates the rigid Apulian platform acting as buttress, the fault bend folds generated during the previous phase and the development of the Tragjasi out-of-sequence thrust (OOST) disconnecting this unit from the more internal Golimbasi trend.  

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Acknowledgment

This work is part of an ongoing exploration program that OMV Albanien, as operator, and Hellenic Petroleum have undertaken recently in S. Albania. We thank OMV Albanien and Hellenic Petroleum management for allowing us to publish some of the data. We would like to acknowledge the contribution of Dr. P. Seifert of OMV AG for his cooperation and fruitful discussions on this subject.

 

References

Bakiaj H. and Bega Z., 1992,    Lushnje-Elbasan transversal fault as an important feature of the external Albanides – an interpretation, 4th EAPG Conf. and Tech. Exhibition, Paris.

Moorkens T. and Döhler M., 1994, Albania. in Kulke H., ed., Regional Petroleum Geology of the World, v. I: Gebruder Borntraeger, Berlin, p. 325-342.

Gambini R, and Tozzi M., 1996, Tertiary geodynamic evolution of the Southern Adria microplate; Terra Nova, v. 8, p. 593-602.

Roure F., and Prenjasi E., Xhafa Z., 1995 Trip #7, Albania: Petroleum geology of the Albanian thrust belt. AAPG International Conference, Nice.

Roure F., et al., 2000, Kinematic evolution and petroleum systems: an appraisal of the Outer Albanides (in press): AAPG Special Publication (Proceedings of the Thrust Tectonics 99 Meeting/London, ed. K. MacKlay).

Salvini F., and Storti F, Gambini R., Ballauri A., 2002, The contribution of HCA numerical modelling to cross-section validation and balancing: application to Vlora Region (S.Albania).

Velaj T., Davison I., Serjani A., and Alsop I., 1999, Thrust tectonics and the role of evaporites in the Ionian zone of the Albanides, AAPG Bulletin, v. 83, no. 9, p. 1408-1425.

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