|
|
|
|||||||||||||||||
| Journal of the Geological Society | ![]() |
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
Article |
1 Department of Geology, The University, Southampton SO9 5NH, UK
2 Department of Geology, University College, PO BOX 78, Cardiff CF1 1XL, UK
The geology of the Rhodope region of northern Greece consists of crystalline basement rocks of the Rhodope Massif in which Tertiary extensional basins and granitic intrusions of Oligocene age occur widely.
Geophysical modelling has highlighted the close spatial relationship of the Tertiary sedimentary basins and post-tectonic granites of closely similar age. Geochemical data for selected granites are used to support the suggestion that there is a close genetic relationship between the episode of granite intrusion and the tectonic development of extensional basins.
This article has been cited by other articles:
![]() |
D. Kondopoulou, A. Atzemoglou, and S. Pavlides Palaeomagnetism as a tool for testing geodynamic models in the North Aegean: convergences, controversies and a further hypothesis Geological Society, London, Special Publications, January 1, 1996; 105(1): 277 - 288. [Abstract] [PDF] |
||||
![]() |
I. KOUKOUVELAS and G. PE-PIPER The Oligocene Xanthi pluton, northern Greece: a granodiorite emplaced during regional extension Journal of the Geological Society, August 1, 1991; 148(4): 749 - 758. [Abstract] [PDF] |
||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |