Core Description

Major and Minor Characteristics and Degree of Formation Consolidation

Major Characteristics

Major characteristics might include the fact that the rock is laminated (Figure 1) or shaly, as well as the minerals present (quartz, feldspar [Figure 1], clays, etc.).

rock laminations quartz and feldspar
Figure 1: From left to right: rock laminations, quartz and feldspar

Minor Characteristics

Minor characteristics might indicate a minor percentage of accessory minerals such as mica, pyrite or glauconite (Figure 2). Other important sedimentary characteristics and structures, such as the presence of stylolites (serrated surfaces within a rock mass from which mineral material has been removed by pressure dissolution in a process that decreases the total volume of rock) (Figure 3), should be recorded when present.

mica muscovite, pyrite and glauconite
Figure 2: From left to right: mica (muscovite), pyrite and glauconite
Stylolite
Figure 3: Stylolite

Although a hardness scale exists for pure minerals, it is not generally used for core descriptions. Instead, the degree of consolidation or unconsolidation, and whether it is friable or well cemented (Figure 4 ), are the characteristics that are noted in describing a core.

friable core section left and well cemented core section right
Figure 4: Friable core section (left) and well-cemented core section (right)

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