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Robert E. Fellows

Publications and source records attributed to Robert E. Fellows.

3 recordsLinked to original sources

Flowage and recrystallization in paleozoic quartzites

The lower limit of visible traces of penetrative movement in quartz‐rich rocks can be defined by studies of orientations and mutual relations of grains. Intensity of deformation in the central Appalachians decreases gradually from the crystalline Piedmont toward the north, northwest, and west perpendicular to the regional trend. The author has attempted to determine the limits of visible deformation geographically and stratigraphically.

Eos, Transactions, American Geophysical Union

The influence of grain‐selection on the meaning of quartz‐diagrams

The most important factor which would reduce confusion in fabric analyses is the expanded use of partial diagrams. The purpose of this paper is to stress the significance of partial diagrams in a consideration of some confusing aspects of petrofabrics. Any statistical study results in the accumulation of a mass of detail. In quartz‐fabric analyses the detail consists of the measuring and plotting of thousands of quartz‐axes; in an analysis of joints it consists of the measuring and plotting of thousands of joint‐attitudes. In each case limiting factors are required to give meaning to the accumulated data. The study of joints, to be significant, must be confined to an area with well‐integrated structural features. In quartz‐fabric studies discrimination between grain‐types is essential to the development of interpretable diagrams.

Eos, Transactions, American Geophysical Union