Resource estimation regions (0)
| Mura-Zala Basin |
| Bekes Basin |
| Backa |
| Somogy Region |
| Drava Basin |
| Zagreb Basin |
| Sava Basin |
| East-Slavonia |
| Vojvodina |
| Mako Trough |
| Battonya High |
Country_boundaries_crop (2)
Country_boundaries (3)
DARLINGe_pilot_area (4)
DARLINGe_project_area (5)
Ca15000 (7)
DH_infra (8)
GeoDH (9)
crossSections (11)
| Section 1 |
| Section 2 |
| Section 3 |
| Section 4 |
| Section 5 |
BM_top_0807.grd (12)
| < - -8 500 |
| -8 499 - -8 000 |
| -7 999 - -7 500 |
| -7 499 - -7 000 |
| -6 999 - -6 500 |
| -6 499 - -6 000 |
| -5 999 - -5 500 |
| -5 499 - -5 000 |
| -4 999 - -4 500 |
| -4 499 - -4 250 |
| -4 249 - -4 000 |
| -3 999 - -3 750 |
| -3 749 - -3 500 |
| -3 499 - -3 250 |
| -3 249 - -3 000 |
| -2 999 - -2 750 |
| -2 749 - -2 500 |
| -2 499 - -2 250 |
| -2 249 - -2 000 |
| -1 999 - -1 750 |
| -1 749 - -1 500 |
| -1 499 - -1 250 |
| -1 249 - -1 000 |
| -999 - -750 |
| -749 - -500 |
| -499 - -250 |
| -249 - 0 |
| 1 - 250 |
| 251 - 500 |
| 501 - 650 |
Top surface of the BF30-50 reservoir [m a.s.l.] (14)
| < -1 000 |
| -1 000 - -900 |
| -900 - -800 |
| -800 - -700 |
| -700 - -600 |
| -600 - -500 |
| -500 - -400 |
| -400 - -300 |
| -300 - -200 |
Bottom surface of the BF30-50 reservoir [m a.s.l.] (15)
|
| < -1 100 |
| -1 100 - -1 000 |
|
| -1 000 - -900 |
|
| -900 - -800 |
|
| -800 - -700 |
|
| -700 - -600 |
|
| -600 - -500 |
|
| -500 - -400 |
|
| -400 < |
Top surface of the BF50-75 reservoir [m a.s.l.] (16)
| < -1 300 |
| -1 300 - -1 200 |
| -1 200 - -1 100 |
| -1 100 - -1 000 |
| -1 000 - -900 |
| -900 - -800 |
| -800 - -650 |
|
| -650 < |
Bottom surface of the BF50-75 reservoir [m a.s.l.] (17)
| < -1 500 |
|
| -1 500 - -1 400 |
| -1 400 - -1 300 |
|
| -1 300 - -1 200 |
|
| -1 200 - -1 100 |
|
| -1 100 - -1 000 |
|
| -1 000 - -900 |
|
| -900 - -800 |
|
| -800 - -650 |
|
| -650 < |
Top surface of the BF75-100 reservoir [m a.s.l.] (18)
| < -1 600 |
| -1 600 - -1 500 |
| -1 500 - -1 400 |
| -1 400 - -1 300 |
| -1 300 - -1 200 |
| -1 200 - -1 100 |
| -1 100 - -1 050 |
|
| -1 050 < |
Bottom surface of the BF75-100 reservoir [m a.s.l.] (19)
| < -2 000 |
| -2 000 - -1 900 |
| -1 900 - -1 800 |
| -1 800 - -1 700 |
|
| -1 700 - -1 600 |
|
| -1 600 - -1 500 |
|
| -1 500 - -1 400 |
|
| -1 400 - -1 300 |
|
| -1 300 - -1 200 |
|
| -1 200 - -1 090 |
|
| -1 090 < |
Top surface of the BF100-125 reservoir [m a.s.l.] (20)
| < -2 100 |
| -2 100 - -2 000 |
| -2 000 - -1 900 |
| -1 900 - -1 800 |
| -1 800 - -1 700 |
| -1 700 - -1 600 |
| -1 600 - -1 500 |
|
| -1 500 < |
Bottom surface of the BF100-125 reservoir [m a.s.l.] (21)
| < -2 600 |
| -2 600 - -2 500 |
| -2 500 - -2 400 |
| -2 400 - -2 300 |
| -2 300 - -2 200 |
|
| -2 200 - -2 100 |
|
| -2 100 - -2 000 |
|
| -2 000 - -1 900 |
|
| -1 900 - -1 800 |
|
| -1 800 - -1 700 |
|
| -1 700 - -1 600 |
|
| -1 600 - -1 500 |
|
| -1 500 < |
Top surface of the BF125-150 reservoir [m a.s.l.] (22)
| High : 0 - Low : -2656.15 |
Bottom surface of the BF125-150 reservoir [m a.s.l.] (23)
|
| High : 0 - Low : -2947.88 |
BF reservoir -- H50C difference between and measured and estimated value (estimated by the conductive model) (25)
| < Mean - 2 x st.dev |
| Mean - (1--2) x st.dev |
| Mean (-1 - +1) x st.dev |
| Mean +(1--2) x st.dev |
| > Mean -+2 x st.dev |
Calculated 30 °C isotherm surface in the Neogene sediments [m a.s.l.] (26)
| < -600 |
| -600 - -575 |
| -575 - -550 |
| -550 - -525 |
| -525 - -500 |
| -500 - -475 |
| -475 - -450 |
| -450 - -425 |
| -425 - -400 |
| -400 - -375 |
| -375 - -350 |
| -350 - -325 |
| -325 - -300 |
| -300 < |
Calculated 50 °C isotherm surface in the Neogene sediments [m a.s.l.] (27)
|
| < -1 150 |
| -1 150 - -1 100 |
| -1 100 - -1 050 |
| -1 050 - -1 000 |
| -1 000 - -950 |
| -950 - -900 |
| -900 - -850 |
| -850 - -800 |
| -800 - -750 |
| -750 - -700 |
| -700 - -650 |
|
| -650 < |
Calculated 75 °C isotherm surface in the Neogene sediments [m a.s.l.] (28)
| < -1 900 |
| -1 900 - -1 850 |
| -1 850 - -1 800 |
| -1 800 - -1 750 |
| -1 750 - -1 700 |
| -1 700 - -1 650 |
| -1 650 - -1 600 |
| -1 600 - -1 550 |
| -1 550 - -1 500 |
| -1 500 - -1 450 |
| -1 450 - -1 400 |
| -1 400 - -1 350 |
|
| -1 300 < |
Calculated 100 °C isotherm surface in the Neogene sediments [m a.s.l.] (29)
|
| < -2 350 |
| -2 350 - -2 300 |
| -2 300 - -2 250 |
| -2 250 - -2 200 |
| -2 200 - -2 150 |
|
| -2 150 - -2 100 |
| -2 100 - -2 050 |
| -2 050 - -2 000 |
| -2 000 - -1 950 |
| -1 950 - -1 900 |
|
| -1 900 < |
Calculated 125 °C isotherm surface in the Neogene sediments [m a.s.l.] (30)
|
| < -3 000 |
|
| -3 000 - -2 950 |
|
| -2 950 - -2 900 |
|
| -2 900 - -2 850 |
|
| -2 850 - -2 800 |
|
| -2 800 - -2 750 |
|
| -2 750 - -2 700 |
|
| -2 700 - -2 650 |
|
| -2 650 - -2 600 |
|
| -2 600 - -2 550 |
|
| -2 550 - -2 500 |
|
| -2 500 - -2 450 |
|
| -2 450 < |
Calculated 150 °C isotherm surface in the Neogene sediments [m a.s.l.] (31)
|
| < -3 600 |
|
| -3 600 - -3 550 |
|
| -3 550 - -3 500 |
|
| -3 500 - -3 450 |
|
| -3 450 - -3 400 |
|
| -3 400 - -3 350 |
|
| -3 350 - -3 300 |
|
| -3 300 - -3 250 |
|
| -3 250 - -3 200 |
|
| -3 200 - -3 150 |
|
| -3 150 - -3 100 |
|
| -3 100 - -3 050 |
|
| -3 050 - -3 000 |
|
| -3 000 < |
Top of fine grained alluvial sediments [m a.s.l.] (33)
| -3000 - -2 800 |
| -2 800 - -2 600 |
| -2 600 - -2 400 |
| -2 400 - -2 200 |
| -2 200 - -2 000 |
| -2 000 - -1 800 |
| -1 800 - -1 600 |
| -1 600 - -1 400 |
| -1 400 - -1 200 |
| -1 200 - -1 100 |
| -1 100 - -1 000 |
| -1 000 - -900 |
| -900 - -800 |
| -800 - -700 |
| -700 - -600 |
| -600 - -500 |
| -500 - -400 |
| -400 - -300 |
| -300 - -200 |
| -200 - -100 |
| -100 - 0 |
| 0 - 100 |
| 100 < |
Base of shallow lacustrine sandy sediments [m a.s.l.] (34)
|
| -3000 - -2 800 |
|
| -2 800 - -2 600 |
|
| -2 600 - -2 400 |
|
| -2 400 - -2 200 |
|
| -2 200 - -2 000 |
|
| -2 000 - -1 800 |
|
| -1 800 - -1 600 |
|
| -1 600 - -1 400 |
|
| -1 400 - -1 200 |
|
| -1 200 - -1 100 |
|
| -1 100 - -1 000 |
|
| -1 000 - -900 |
|
| -900 - -800 |
|
| -800 - -700 |
|
| -700 - -600 |
|
| -600 - -500 |
|
| -500 - -400 |
|
| -400 - -300 |
|
| -300 - -200 |
|
| -200 - -100 |
|
| -100 - 0 |
|
| 0 - 100 |
|
| 100 < |
Top of pre-cenozoic basement [m a.s.l.] (35)
|
| < - -8 500 |
|
| -8 499 - -8 000 |
|
| -7 999 - -7 500 |
|
| -7 499 - -7 000 |
|
| -6 999 - -6 500 |
|
| -6 499 - -6 000 |
|
| -5 999 - -5 500 |
|
| -5 499 - -5 000 |
|
| -4 999 - -4 500 |
|
| -4 499 - -4 250 |
|
| -4 249 - -4 000 |
|
| -3 999 - -3 750 |
|
| -3 749 - -3 500 |
|
| -3 499 - -3 250 |
|
| -3 249 - -3 000 |
|
| -2 999 - -2 750 |
|
| -2 749 - -2 500 |
|
| -2 499 - -2 250 |
|
| -2 249 - -2 000 |
|
| -1 999 - -1 750 |
|
| -1 749 - -1 500 |
|
| -1 499 - -1 250 |
|
| -1 249 - -1 000 |
|
| -999 - -750 |
|
| -749 - -500 |
|
| -499 - -250 |
|
| -249 - 0 |
|
| 1 - 250 |
|
| 251 - 500 |
|
| 501 < |
|
