Journal of Petroleum Geology, Vol.7,
No.4, pp.365-380, 1984
©Copyright 2000 Scientific Press,
Ltd.
FISSION TRACK DATING OF AN
APATITE CRYSTAL
FROM HORMUZ ISLAND, IRAN
A. J. Hurford*, H. R. Grunau** and J.
Stöcklin***
*Abteilungfur Isotopengeologie der
Universität Bern, Erlachstrasse 9a, 3012 Bern, Switzerland.
**Petroconsultants S.A., 8-10, Rue
Muzy, 1211 Geneve 6, Switzerland.
***Erdbuhlstrasse 4, 8472 Seuzach,
Switzerland.
Abstract
Geological evidence points to a Late
PreCambrian origin for the Hormuz apatites associated with the
red iron oxides, salt and other sedimentary and igneous rocks of
the Hormuz Complex. Fission track dating of an apatite crystal
from Hormuz Island gives an age of 55.4 ± 2.6 MM* years for a
cooling temperature of approximately 100°C corresponding to the
Paleocene-Eocene boundary. This result is interpreted in the
light of the burial and temperature history of the apatite
associated with the Hormuz salt. It is concluded that the apatite
clock registers the time elapsed since the temperature decreased
to 100°C at the Paleocene-Eocene boundary. Steady cooling took
place thereafter due to the continuing upward movement of the
salt plug until Quaternary times. The stratigraphic position
which the salt diapir (with the associated apatite) had reached
55 MM years ago corresponds to a level somewhere within the
Triassic sequence. This would have been the zone of oil
generation in Paleocene-Eocene time, assuming that a source rock
was present. Interpretational uncertainties are due to in
sufficient knowledge of the paleotemperature regime and of the
stratigraphy and sedimentary thicknesses of the complete sequence
down to the PreCambrian. In addition, it is not possible to draw
far-reaching conclusions based on the dating of only one sample.