A Modification of the Geosyncline and Tectogene Hypothesis
- Creators
- Wyllie, Peter J.
Abstract
Intersections may exist between a zone of chemical discontinuity (basalt—feldspathic periodtite or eclogite—garnet peridotite) and a phase transition zone (basalt—eclogite or feldspathic peridotite to garnet peridotite) at about the depth of the continental M-discon-tinuity. Variations in depth to the chemical discontinuity and in the positions of isogeotherms produce flexibility in erogenic models. Intersections between the two zones at depth could be reflected at the surface by major fault zones separating large structural blocks of different elevations. The effects of such intersections on the conventional hypothesis for the development of tectogenes, geosynclines, and mountains are considered. The intersections could provide a beginning and an end to the more vigorous changes in surface level occurring during an orogenic cycle.
Additional Information
© 1965 Cambridge University Press. I am grateful to R.F. Schmalz for reading the manuscript critically, to R.H. Jahns and B.F. Howell for earlier discussions, and to the National Science Foundation for covering the costs of preparing the manuscript (Grant NSF-GP-1970). This is Contribution No. 63-70 from the College of Mineral Industries, The Pennsylvania State University.Additional details
- Eprint ID
- 63864
- Resolver ID
- CaltechAUTHORS:20160122-075017915
- GP-1970
- NSF
- Created
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2016-01-22Created from EPrint's datestamp field
- Updated
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2021-11-10Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences