The
location of the area is shown on the general
map of the Kuldiga structure.
The
Kuldiga
oil discovery (in Cambrian sandstone) is located within the licence area, discovered in 1963,
it is the very first oil
discovery within the Cambrian succession of the Baltic Region. It is
associated with the Kuldiga High, and is an asymmetrical north-northeast
trending anticlinal structure. The size of this fold is about 45 km2
with a vertical closure of 60 m, its eastern flank is steep and fault
controlled. Based on the drilling data, the identified oil occurs within
a 7 m (based on seismic data -15? m) thick sandstone layer of the
Deimena Formation, which is 55 m thick there. The sandstone is poorly
cemented, and the porosity exceeds 20%, permeability might exceed 1D.
The oil-bearing bed is sealed by 8-11 m of Early Ordovician mudstone.
The Kuldiga oil-water contact is horizontal at depth of 962 (961?) m.
The area of the oil deposit within that contour does not
exceed 1 km2; its size approximately 1.5 x 0.5 km.
The driving mechanism in the structure is predominantly by water;
reservoir temperature is 22ºC and initial pressure was 102
atmospheres.
In
the well Kuldiga R-2 (Kuldiga-2) the oil flow reached 3.3 m3 per day on
test.
Besides,
oil was observed in the Ordovician
deposits as well. Small oil flows were obtained from several wells from the
U. Ordovician calcarenite and L. Ordovician sandstone.
AVAILABLE
GEOPHYSICAL AND GEOLOGICAL DATA
Small-scale
CDP seismic investigations were carried out in the area of the Kuldiga
oil deposit; several wells were drilled.
Well
and seismic data as well as maps are available to the oil industry for purchase and
inspection: