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We used Berea sandstone and Sarukawa sandstone as homogeneous and heterogeneous rock in this study.
In particular, the distinctive IP property of the massive sulfide rock in this study (Fig. 3c) is similar to that observed in terrestrial massive kuroko ore samples of volcanogenic massive sulfide deposits by Yoshikawa and Yoshikawa (1978), who performed time-domain IP measurements and found that the interfaces behave as a kind of Warburg impedance.
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Most of the PhP isomers and 2,2′-BiN were detected in all rocks in this study.
Table 1 Bulk properties and selected geochemical parameters for oils and rocks in this study Sample no.
However, we treat basements rocks in the two belts and those beneath the Joban basin as 'pre-Cretaceous basement rocks' in this study.
The conglomeratic rocks in this study are parts of thick synorogenic molasses sequence of upper Pliocene to Pleistocene age, the Bakhtiari and Hezardareh Formations.
It should be noted that properties of the rock were identical in the entire rock block in this study.
The mineral assemblages of this rock in the study area are orthopyroxene + quartz + K-feldspars + biotite ± garnet.
Two contrasting types of mineral assemblage are present in the two dykes of rodingitized granitic rock investigated in this study.
Transmission electron microscopy or synchrotron-based x-ray methods represent useful follow-up methods to characterize the rock varnish in this study [12, 22, 23].
It seems reasonable that biological mediation must play some significant role in Mn oxidation, if in tandem with abiological processes, in the development of rock varnishes in this study.
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