Tertiary surface combustion of Cretaceous bituminous sediments in Isra
el produced high-T, low-P metamorphic assemblages, which were dated by
conventional K-Ar and Ar-40/Ar-39 techniques. Meaningful ages were ob
tained from samples of high metamorphic grade and K content higher tha
n 0.8%, containing sanidine, anorthite, gehlenite and zeolites. In the
se minerals the K-Ar system has been reset, and equilibrated with atmo
spheric Ar, yielding a mean age of 3 +/- 1 Ma. Ar-40/Ar-39 plateau and
isochron ages for four whole-rock samples range between 2.3 and 4.0 M
a. One gehlenite rock yielded an Ar-40/Ar-39 age of 16 +/- 0.2 Ma (1 s
igma). These results indicate a major combustion metamorphic event aro
und 3 Ma, probably preceded by an event around 16 Ma. The early event
took place upon initial exposure of the protolith in the Miocene, wher
eas the second followed the removal of Neogene sediments and re-exposu
re of the bituminous rocks.