CLASSIFICATION OF REFOLD STRUCTURES

dc.contributor.author	Grasemann B.
dc.contributor.author	Wiesmayr G.
dc.contributor.author	Draganits E.
dc.contributor.author	Fusseis F.
dc.date.accessioned	2022-09-24T04:26:15Z
dc.date.available	2022-09-24T04:26:15Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=7896625
dc.identifier.citation	Journal of Geology, 2004, 112, 1, 119
dc.identifier.issn	0022-1376
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38741
dc.description.abstract	Structural geology textbooks distinguish among four end members of three-dimensional refold structures established from their two-dimensional interference patterns. Here it is shown that six different end members of three-dimensional refold structures exist. These end members can be described by a reduced direction cosines matrix L. The classical types 1-3 are extended to have three new counterparts types 0!sub 1!-0!sub 3!, which are derived by 90(o) rotation of the superposed fold around its fold axis. The matrix L can be used to characterize the angles between the two fold generations in a simple triangle plot illustrating the six end members and even any intermediate refold structure. [PUBLICATION ABSTRACT]
dc.subject	GEOLOGY
dc.title	CLASSIFICATION OF REFOLD STRUCTURES
dc.type	Статья

Files in this item

Name: Gras_04.pdf

Size: 436.3Kb

Format: PDF