Geochemical correlation studies of seven oils and source rocks from th
e onshore Tempoku basin of northern Hokkaido were carried out. Low sul
fur, high wax and high pristane/phytane ratios of the oils suggest tha
t they were generated mainly from nonmarine source rocks. Source rock
evaluation and hydrous pyrolysis data show that coals and coaly shales
in the Paleogene Haboro Formation and Cretaceous Hakobuchi Group have
oil-generating potential. These nonmarine source rocks are correlated
as the major source of the Tempoku oils, using sterane and triterpane
distributions and carbon isotope compositions. Correlation studies al
so suggest a minor contribution from marine source rocks of the Neogen
e Onishibetsu or Paleogene Magaribuchi Formations to the oils of the Y
uchi and Wakkanai fields located in the western part of the basin. Cop
yright (C) 1996 Elsevier Science Ltd