Rates of tectonic uplift in the Corinth and Megara Basins, central Greece

Tectonics

Volumn 11, Issue 6, 1992, Pages 1159-1167

  Collier, R E L ^a   Leeder, M R ^a   Rowe, P J ^a   Atkinson, T C ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

NEOTECTONICS; QUATERNARY; SEA LEVEL VARIATION; UPLIFT; URANIUM SENSES DATING;

GREECE, CORINTH BASIN; GREECE, MEGARA BASIN;

EID: 0027046646     PISSN: 02787407     EISSN: 19449194     Source Type: Journal    
DOI: 10.1029/92TC01565     Document Type: Article

References (41)

1. Uranium‐series evidence on diagenesis and hydrology in Pleistocene carbonates of Barbados, West Indies
2. Uranium‐234 anomalies in corals older than 150,000 years
3. Ratio of ionium to uranium in coral limestone
4. Uranium‐series dating of the Pleistocene reef tracts of Barbados, West Indies
5. Tectono‐sedimentary development of an extensional basin: the Neogene Megara Basin, Greece
6. Geodetic determination of tectonic deformation in central Greece from 1900 to 1988
7. A preliminary evaluation of uranium series inequilibrium as a tool for absolute age measurement on marine carbonates.
8. 238U, 234U and 232Th in seawater
9. Eustatic and tectonic controls upon Quaternary coastal sedimentation in the Corinth Basin, Greece
10. Neogene to Quaternary rifting, sedimentation and uplift in the Corinth Basin, Greece
11. Transverse and linear dunes in an Upper Pleistocene marine sequence, Corinth Basin, Greece
12. Transgressions and regressions: a model for the influence of tectonic subsidence, deposition and eustacy, with application to Quaternary and Carboniferous examples
13. Observations sur l'histoire géologique pliocène et quaternaire du golfe et de l'isthme de Corinthe
14. Listric faulting, sedimentation, and Quaternary eastern Corinth rift, Greece: First stages of continental rifting
15. 238U‐234U‐230Th‐232Th systematics and the precise measurement of time over the past 500,000 years
16. Application of the 227Th/230Th method to dating Pleistocene carbonates and comparison with other dating methods
17. 234U/238U mass spectrometry of corals: How accurate is the U/Th age of the last interglacial period?
18. The Hellenic subduction beneath the Peloponnesus: First results of a microearthquake study
19. Zur jungpleistozanen und Holozanen Kustenmorphologie zwischen Korinth und sud‐Attica
20. The orbital theory of Pleistocene climate: support from a revised chronology of the marine d18O record
21. The geometrical evolution of normal fault systems
22. Rates of active deformation in the Aegean Sea and surrounding areas
23. Seismicity, normal faulting, and the geomorphological development of the Gulf of Corinth (Greece): the Corinth earthquakes of February and March 1981
24. The neotectonics of the Aegean: an alternative view
25. A synoptic view on the neotectonic development of the Peloponnesian coastal regions
26. Le Plio‐Pléistocène marin et oligohalin en Grèce: Stratigraphie et paléogéographie
27. The terraces of Corinth (Greece) ‐ a detailed record of eustatic sea‐level variations during the last 500,000 years
28. The Tertiary geodynamical evolution of the Aegean arc: a palaeomagnetic reconstruction
29. Palaeomagnetic evidence for Neogene rotational deformations in the Aegean domain
30. U‐series dating of last interglacial high sea stands: Barbados revisited
31. Sedimentation and tectonic geomorphology adjacent to major active and inactive normal faults, southern Greece
32. The Aegean Sea
33. Active tectonics of the Alpine‐Himalayan belt: the Aegean Sea and surrounding regions
34. A block model of distributed deformation by faulting
35. Marine geological research at the eastern Corinthiakos Gulf
36. Oxygen isotopes, ice volume and sea level
37. The Hellenic subduction zone: a tomographic image and its geodynamic implications
38. The seismicity, geomorphology and structural evolution of the Corinth area of Greece