Abstract
IN a previous paper in the Geological Magazine (1) the hypothesis was suggested that mountains might result from the dragging together of sediments and other rocks by a convection current inthe material below the crust. It may be useful to review the present position as to how far this idea has offered an adequate explanation of mountain and other earth structures.
Publisher
Cambridge University Press (CUP)
Cited by
2 articles.
订阅此论文施引文献
订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Terrestrial Heat and Earth Movements;Proceedings of the Geologists' Association;1947-01
2. The compression of a sheet;Proceedings of the Geologists' Association;1943-01