These are magnetite deposits associated with volcanic rocks of dioritic affinity (i.e., igneous rocks intermediate in composition between granites and gabbros).
Table 6 Aggravation factor F A according to earthquake origin, soil type, and slope Earthquake source Type of soil F A Slope < 10% Slope > = 10% Near Rock +0.5 +1.0 Intermediate 0 +0.5 Soft −0.25 +0.25 Far Rock 0 +0.5 Intermediate +0.5 +1.0 Soft +1.0 +1.0.
ROCK phosphorylates intermediate filament proteins, specifically at the cleavage furrow during cytokinesis.
Andesine, less common, occurs in many granular and volcanic rocks with intermediate silica content, as in Marmato, Colom., and Bodenmais, Bavaria, Ger.
SEES surfactant also showed improved wettability alteration property, changing the nature of oil-aged rock from intermediate-wet to water-wet.
Epidote is a hydroxylated Ca-Al-silicate commonly observed in a variety of high-pressure rocks, from basaltic eclogites, to metagabbros and rodingites of the metamorphosed oceanic crust, then to intermediate rock compositions representative of slices of the continental crust involved in high-pressure processes at subduction zones.
Felsic rocks are commonly oversaturated and contain free quartz (SiO2), intermediate rocks contain little or no quartz or feldspathoids (undersaturated minerals), and mafic rocks may contain abundant feldspathoids.
The shear strength of the thrust fault may be relatively insensitive to rock types at intermediate depths (15 to 35 km in depth).
On the other hand, non-uniform crusts, which do not entirely cover the host rock, represent an intermediate condition: storage of airborne carbonaceous particles and surface accumulation of metallic pollutants are enhanced because of a relatively high porosity, given by a mix of disaggregated host rock and uneven, incomplete and scarcely adhering crystallization of newly formed phases.
In contrast to the deep thrust zone, the shear strength of siliceous sedimentary rocks in the intermediate zone (segment b-c in Figure6a) is almost the same as that of basic rocks.
