Chronostratigraphic relations of Neogene formations of the Great Hungarian Plain based on interpretation of seismic and paleomagnetic data
- Geofizikai, Budapest (Hungary)
- Magyar Allami Foeldtani Intezet, Budapest (Hungary)
- Geological Survey, Reston, VA (USA)
- Geological Survey, Flagstaff, AZ (USA)
This cooperative study by Hungarian and American geologists and geophysicists, demonstrates the power of the combination of modern paleomagnetic techniques and seismic profiling in working out the stratigraphy of a basin, with only limited paleontologic and isotopic control. Indirect evidence suggests that lake levels in the Pannonian inland sea (a remnant of the Paratethys), although isolated from the world's oceans, were affected by eustatic sea-level changes. Four hiatuses identified by seismic profiles near the northern margin of the Pannonian Basin and inferred to represent non-deposition between 11.5 and 10.5, 7.9 and 7.6, 6.8 and 5.7, 5.4 and 4.6 million years ago. Comparing these hiatuses with the eustatic sea level change curves the accordance is close and systematic. This indicates that the sea level of the Pannonian Inland Sea that became gradually isolated from the world oceans fluctuated in the same phase as global sea level. The hiatus between 6.8 and 5.7 Ma is tentatively correlated with the Messinian global stage during which time evaporite deposition in the Mediterranean was widespread--the so-called Messinian salinity crisis.
- OSTI ID:
- 6250491
- Journal Information:
- International Geology Review; (USA), Vol. 32:5; ISSN 0020-6814
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
HUNGARY
SEDIMENTARY BASINS
STRATIGRAPHY
AGE ESTIMATION
CORRELATIONS
DEPOSITION
DEPTH
GEOLOGIC HISTORY
GROUND SUBSIDENCE
ISOTOPE RATIO
PALEOMAGNETISM
PALEONTOLOGY
SEA LEVEL
SEDIMENTS
SEISMIC SURVEYS
SURFACE WATERS
DEVELOPING COUNTRIES
DIMENSIONS
EASTERN EUROPE
EUROPE
GEOLOGIC STRUCTURES
GEOLOGY
GEOPHYSICAL SURVEYS
LEVELS
MAGNETISM
SURVEYS
580000* - Geosciences