Incremental Growth of Plains-Type (Compactional) Folds in a Cratonic Environment as Revealed by the Sedimentary Sequence

The enigma of the origin and development of plains-type folds, as they were christened in the early 20th Century, essentially has been solved. The folds, a considerable distance from the tectonic disturbance, were formed by draping of sediments over differentially displaced Precambrian basement faul...

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Veröffentlicht in:	Natural resources research (New York, N.Y.) N.Y.), 2003-03, Vol.12 (1), p.27-40
1. Verfasser:	Merriam, Daniel F
Format:	Artikel
Sprache:	eng
Schlagworte:	Anticlines Basements Columnar structure Compaction Constraint modelling Depth perception Estimates Precambrian Sediments Segments Stratigraphy Tectonics Well data
Online-Zugang:	Volltext
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