Flow direction in triclinic folded rocks

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ID: 303244
1968
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Abstract
Folds that have widely dispersed trends in outcrop of the northern Ruby Mountains, Nevada, show a common sense of overturning that is interpreted to be the flow line of velocity-gradient flow. The flow line thus deduced remains constant over a wide area in which both the major folds and the average parasitic folds vary markedly in orientation, and the fabric symmetry varies from monoclinic to triclinic.
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openalex_W2316585173 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Keith A. Howard
Journal american journal of science
Year 1968
DOI
10.2475/ajs.266.9.758
URL
https://ajs.scholasticahq.com/article/59267.pdf
Keywords Keywords not found

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