Palaeomagnetic timing of the rotation and translation of Cyprus

Details Palaeomagnetic timing of the rotation and translation of Cyprus Palaeomagnetic timing of the rotation and translation of Cyprus

Feb 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987e%26psl..81..409a&link_type=abstract

Earth and Planetary Science Letters, Volume 81, Issue 4, p. 409-418.

Mathematics

Logic

7

Scientific paper

The geological evolution of the Mesozoic Troodos Ophiolite Complex in Cyprus, and the tectonic nature and timing of the palaeomagnetically indicated anticlockwise rotation of Cyprus of some 80° and ca. 15° northward translation, have been open for debate for some time. New palaeomagnetic data from 18 sites (~ 180 samples) in the post-ophiolite sediments, ranging in age from Upper Cretaceous to Upper Miocene, are presented. Most of the sites are of normal geomagnetic polarity, but indications of reversed polarity have been found in an older group of sediments (the Lefkara Formation of Upper Palaeocene age).
Six sites from the older group of sediments (Upper Cretaceous to Eocene in age) give a site mean direction of the AF cleaned sediments of (D, I) = (323°, 29°) with α95 = 18°, while 5 sites from a younger group of sediments (Oligocene to Miocene in age) give a cleaned site mean direction of (D, I) = (334°, 58°) with α95 = 9°. These and published data suggest that an anticlockwise rotation of Cyprus of ~ 60 +/- 10° occurred early during the post-igneous evolution of the Cyprus oceanic crust between ~ 90 and ~ 50 Ma, leaving only a minor anticlockwise rotation of ~ 20 +/- 10° to occur during the last 50 Ma. It is furthermore concluded that the northward translation of Cyprus of ~ 15° mostly took place during the last ~ 30 Ma.
It thus appears that a fairly rapid rotation of the Cyprus microplate first took place in the Late Cretaceous and Early Tertiary time with an average angular velocity of ~ 1-2°/Ma, during which the northward translation was minor or negligible. In the latter half of the Tertiary, the sense of movement appears to have radically changed, the northward translation now being dominant with an average velocity of ~ 5-6 cm/yr. This temporal evolution is found to be in good agreement with the Mesozoic and Tertiary movements of the African lithospheric plate relative to Europe, as evidenced from the Atlantic sea-floor magnetic anomaly spreading history.

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