Palaeomagnetic evidence for Tertiary counterclockwise rotation of Adria

E. Márton, K. Drobne, V. Ćosović, A. Moro

Research output: Contribution to journalArticle

59 Citations (Scopus)

Abstract

With the aim of obtaining Tertiary palaeomagnetic directions for the Adriatic Foreland of the Dinaric nappe system, we carried out a palaeomagnetic study on platform carbonates from stable Istria, from the northwestern and the Central Dalmatia segment of imbricated Adria. Despite the weak to very weak natural remanences of these rocks, we obtained tectonically useful palaeomagnetic directions for 25 sites from 20 localities. All exhibit westerly declinations, both before and after tilt correction. Concerning the age of the magnetizations, we conclude that five subhorizontal and magnetite bearing Eocene localities from stable Istria are likely to carry primary remanence, whereas three tilted and hematite-bearing ones were remagnetized. In the northwestern segment of imbricated Adria the cluster of the mean directions improved after tectonic correction indicating pre-tilting magnetization. In contrast, Maastrichtian-Eocene platform carbonates from Central Dalmatian were remagnetized in connection with the late Eocene-Oligocene deformation or Miocene hydrocarbon migration. Based on the appropriate site/locality means, we calculate mean palaeomagnetic directions for the above three areas and suggest an alternative interpretation of the data of Kissel et al. [J. Geophys. Res. 100 (1995) 14999] for the flysch of Central Dalmatia. The four area mean direction define a regional palaeomagnetic direction of Dec=336°, Inc=+52°, k =107, α95=9°. From these data we conclude that stable Istria, in close coordination with imbricated Adria, must have rotated by 30° counterclockwise in the Tertiary, relative to Africa and stable Europe. We suggest that the latest Miocene-early Pliocene counterclockwise rotations observed in northwestern Croatia and northeastern Slovenia were driven by that of the Adriatic Foreland, i.e. the rotation of the latter took place between 6 and 4 Ma.

Original languageEnglish
Pages (from-to)143-156
Number of pages14
JournalTectonophysics
Volume377
Issue number1-2
DOIs
Publication statusPublished - Dec 18 2003

Fingerprint

Eocene
carbonate platform
magnetization
Miocene
hydrocarbon migration
flysch
remanence
Maastrichtian
tilt
westerly
nappe
hematite
Oligocene
magnetite
carbonates
Pliocene
platforms
Croatia
folds (geology)
tectonics

Keywords

  • Adria
  • Istria
  • Palaeomagnetism
  • Rotation
  • Tertiary

ASJC Scopus subject areas

  • Earth-Surface Processes
  • Geophysics

Cite this

Palaeomagnetic evidence for Tertiary counterclockwise rotation of Adria. / Márton, E.; Drobne, K.; Ćosović, V.; Moro, A.

In: Tectonophysics, Vol. 377, No. 1-2, 18.12.2003, p. 143-156.

Research output: Contribution to journalArticle

Márton, E. ; Drobne, K. ; Ćosović, V. ; Moro, A. / Palaeomagnetic evidence for Tertiary counterclockwise rotation of Adria. In: Tectonophysics. 2003 ; Vol. 377, No. 1-2. pp. 143-156.
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