Szekessy Vilmos (szerk.): A Magyar Természettudományi Múzeum évkönyve 41. (Budapest 1948)

Szurovy, G.: Geological structure of the Southern part of the Great Hungarian Plain

//// gasoline odour. The Schlumberger log showed 10—15 Q resistance and 20—45 mV porosity. (Fig. 27.) The well showed during an eruption of 20 minutes approximately 63 barrel oil-water emulsion, and then nothing. After having been shut down for 12 hours, the fluid level increased to 1312.3 ft, and approximately 1/5 to 1/7 of the fluid column consisted of oil. After 12 days of bailing tests, it was obvious that the well was on the oil-water contact. During the bailing tests, approximately 140 barrels of oil were recovered. The well was cemented off between 5971.28—5797.39 ft, with 25 sacks of cement, The 6—5/8" casing was cut and pulled out at 3916.44 ft. (o) Körösszegapáti 4. Drilling time: 28 April 1944 to 10 July 1944. The well was drilled without incident^. There was no need for production tests. The well was staked out higher on the structure than No. 3. and reached the depth of 4429.3 ft, without incidents, where the 9—5/8" casing w

ras cemented. The well was left behind all ready for operation when political incidents intervened. The workshop and storerooms in Tótkomlós, Berekböszörmény and Pocsaj, as well as the drilling outfits WIAG # 6, WIAG # 11 and ELWERATH S 55 were left behind in good condition, as their transfer could always be delayed for one reason or another. Looting or destruction was only done by the native population and the retreating German SS troops. (p) Körösszegapáti 5. VII. The Gas of the Deep Tests. 1. Tótkomlós'!. Composition of the Gases: Crude Test: CO= 48.6% Airless test: CO= 51.4% CH. 44.9% O* 1.2% Ns 4.3% C>H. 1.0% CH« 47.5% O* — % N* — % C.H« 1.1% 100.0% 100.0%