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(1)-0(3), which are derived by 90degrees 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.
Original language | English |
---|---|
Pages (from-to) | 119-125 |
Journal | Journal of Geology |
Volume | 112 |
Issue number | 1 |
DOIs | |
Publication status | Published - 2004 |