foliation

This is called a local transversal section of the foliation.

It is aligned more or less parallel with the regional foliation.

The result is a feature referred to as foliation fanning.

Forty or fifty miles beyond this mass of foliation, they came to another that was even more extensive.

Foliation is usually formed by the preferred orientation of minerals within a rock.

Foliation is separated into two groups: primary and secondary.

There is a global foliation theory, because topological constraints exist.

Light descending in floods dissolved the separate foliation into one green mound.

Let be a submanifold that is a leaf of a foliation.

The technical statement is that the tori make a foliation of the moduli space.

Some authors chose to use cleavage when describing any form of secondary foliation.

Technically, these stripes are called plaques of the foliation.

The doorways to the hall have densely carved figures and foliation.

For example, an F fold should have an S axial foliation.

The existence of a taut foliation implies various useful properties about a closed 3-manifold.

The notion of leaves allows for a more intuitive way of thinking about a foliation.

They suggest that structures such as pervasive foliation are a result of load compaction.

The space between planes of parting or foliation are consistent which makes it uniform in thickness.

It is closely related to the concept of Reebless foliation.

Cleavage is a type of secondary foliation associated with fine grained rocks.

Essentially, these distinctions correspond to the dimensions of the leaves of the foliation.

The foliation is commonly crinkled or wavy in appearance.

Due to this orientation, foliation took place.

Shear zones accommodate compressive stress by movement on foliation planes.

Depending on the intensity of heat during recrystallization, the foliation will either be strengthened or weakened.