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Viktória Ünnep 1, Ágnes Török 1 és Attila Balázs 2

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Presentation on theme: "Viktória Ünnep 1, Ágnes Török 1 és Attila Balázs 2"— Presentation transcript:

1 Viktória Ünnep 1, Ágnes Török 1 és Attila Balázs 2
Complex sedimentological and geophysical study of the Kápolna-hegy „spring-cone” (Buda Hills, Hungary) Viktória Ünnep 1, Ágnes Török 1 és Attila Balázs 2 (ELTE TTK - Geology Msc1 and Geophysics Msc. 2) 1

2 Presentation outline Freshwater limestone grouping Springcones
Facies of freshwater limestones Springcones The outcrop of Kápolna-hegy Location Previous studies Field work and laboratory results Reconstruction model Geophysical interpretation Conclusion 2

3 Freshwater limestone grouping (after Pentecost 2005)
Termogen Meteogen Tetaratas, Yellowstone National Park Calcareous tufa, Szalajka patak 3

4 Facies of freshwater limestone
Pamukkale Tetaratas in Pamukkale (Turkey) Spring ridge, Terme San Giovanni (Toscana, Italia) 4 Springcone with lake, Ruzsbachfürdő (Slovakia) Springcone, Szántó (Slovakia)

5 Springcones Types of springcones (Scheuer and Schweitzer 1985) 5

6 Deposit of Kápolna-hegy
Location of Kápolna-hegy Travertine Tamás Tóth 2003 6

7 Deposit of Kápolna-hegy
Previous studies: Schréter (1951) suggested that limestone layers dip outward concentric, forming a mound Scheuer (1996) described the deposit as a springcone Kele (2009) measured Middle-Pleistocene age for the limestone by U/Th method. Schematic representation of springcone by Scheuer (1996) 7

8 Deposit of Kápolna-hegy
Field works Onkoids Schematic represetation of the mine 8

9 Deposit of Kápolna-hegy
2 cm Field works “Orifice (Feeder channel)” 9

10 Field works Deposit of Kápolna-hegy One of caves on the north wall
(Fotó: Virág M.) One of caves on the north wall 10

11 Field works - Laboratory
XRF – yellow siltyclay The yellow powder 90% carbonate abudant amount of quartz Clay minerals: Muskovite/illite Kaolinite Smectite Goethite 11

12 Deposit of Kápolna-hegy
Field works Reed stems 12 “bough”

13 Field works Deposit of Kápolna-hegy 2 cm
Microbial „shrub” exposed bay the south wall Lamination of south wall, tetarata (?) 13

14 Deposit of Kápolna-hegy
Measurement of layer dips The location of vertical section - Dip direction are oriented outward from the possible feed channel Schematic representation of the mine with the dip values 14

15 Location of vertical section
Deposit of Kápolna-hegy Location of vertical section The panorama picture of north wall with the location of samples 15

16 A kápolna-hegyi előfordulás
Szelvény 4 Oncoids Oocardium-like algal Plant fragments Reeds Thin- laminated beds 16

17 Deposit of Kápolna-hegy
The location of profile A N B The satelite picture of the mine with the location of profile ( 17

18 Deposit of Kápolna-hegy
The profile 18

19 Deposit of Kápolna-hegy
Recontruction of sedimentary enviroments Asymmetric cone with lake. The triangle shows the water table of the lake 19

20 Geophysical interpretation
Multielectrode geoelectric profiling clay limestone Vertical elevation (mBf) Distance on the profile (m) 20

21 } Conclusions distal  We separated four different litology types
laminated proximal thick-bed/ oncoids thick-bed/algal fragments thick-bed/ reed stems } distal  The available data suggest that the generation of the cone is related to faults.  We tried to find explanation to the anomalous feature by thin sections and laboratory invetigations (yellow silty clay, „feeder channel”) 21

22 The combination of a springcone and a lake
We elaborated a model to reconstruct the sedimentary enviroment  We verified the sedimentary model by geoelectrical measurement  We have improved Scheuer’s model by suggesting that the travertine of Kápolna-hegy is not simply springcone but: The combination of a springcone and a lake 22

23 Thank you for your attention!
Yellowstone (from internet) 23

24 Thanks to Andrea Mindszenty Sándor Kele Zoltán Hámori András Varga
Orsolya Győri László Lovas Ildikó Cora Ferenc Horváth Zsolt Bendő Tamás Vladár 24 Orange springcone, Yellowstone (from internet)


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