Szekessy Vilmos (szerk.): A Magyar Természettudományi Múzeum évkönyve 41. (Budapest 1948)
Szurovy, G.: Geological structure of the Southern part of the Great Hungarian Plain
//// Moreni 1* Tótkomlós 1 Moreni 1 Tótkomlós 1 Salt Content Relatíve to 100% Salt g/l g/l % % Cl' 103,311 9,890 61.28 54.34 Br' 0,526 0.31 — — J' 0,016 0.01 SO*" Sp. 0,005 — — HCOs' 0,127 0,995 0.07 5.47 K' 0,385 [ 0.23 Na' 53,640 6,997 31.82 38.44 NHs, 0,109 0,020 0.065 0.11 CA8,635 0,124 5.13 0.68 Mg1,719 0,031 1.02 0.17 Fe0,045 Sp. 0.03 — — SiOaHa 0,058 SiOa 0,145 SÍO3H2 0.035 SiO= 0.79 168,571 18,207 100.000 100.00 The water of the well Körösszegapáti 3. is worthy of attention. The results of the analyses were no longer furnished. VIII. Summary. The southern part of the Plain is not a uniform big basin. The line Solt—Kiskunhalas—Zenta —Magyarpadé, seemingly the continuation of the Valer fault, divides this part of the Plain into two halves (Fig. 28). The part of the territory southwest of this line lies considerably higher than the really low territory NE of this line. The demarcation line of the big deep territory in the south may be given by the line Aradi—Lázárfölde—Nagybecskerek—Boka, as lias been also shown by the geophysical measurements made in the Bánság. The basement rock lies again higher south of this line. The less sunken „foreground" is characterized by mountain chains descending into the Plain mostly in the striking trend of the rim mountains. In the Kiskunság this trend is SW — NE. In the Bácska the trend is more W—E. In the southern Bánság the mountains have partly S —E and partly SE — NW trend. Extensive mountain chains descend from the Transylvanian intermediate chain of mountains * G. Macovei: Les gisements de Pétrole, Paris 1938, page 66.
