Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4735144 | Proceedings of the Geologists' Association | 2009 | 6 Pages |
Abstract
Sediment mass-transport layers of submarine origin on the northern and southern flanks of the Troodos ophiolitic massif are dated biostratigraphically as early Miocene and late Miocene, respectively and therefore represent different seismogenic events in the uplift and erosional history of the Troodos terrane. Analysis of such events has potential for documenting Miocene seismic and uplift events regionally in the context of changing stress field directions and plate vectors through time.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Alan R. Lord, Richard W. Harrison, Marcelle BouDagher-Fadel, Byron D. Stone, Osman Varol,