1-7 OF 7 RESULTS FOR

Pangaion-Pirin Complex

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 July 2017
The Canadian Mineralogist (2017) 55 (4): 535–560.
... in the hanging wall. The footwall Pangaion-Pirin Complex consists of marbles and acid gneisses of a Mesozoic carbonate platform on pre-Mesozoic continental basement. In this paper, a range of petrographic and geochemical techniques were used to determine (1) any similarities and differences to other mafic...
FIGURES | View All (13)
Journal Article
Published: 01 March 2010
European Journal of Mineralogy (2010) 22 (2): 189–198.
.... High- and ultrahigh-pressure metamorphic conditions are preserved in an intensely strained mélange zone which is sandwiched between upper-greenschist to lower-amphibolite-facies rocks in the footwall (Pangaion-Pirin Complex) and upper-amphibolite-facies rocks in the hanging wall (Rhodope Terrane...
FIGURES | View All (5)
Image
Geological map of the study area. The mélange zone and the entire <span class="search-highlight">Pangaion</span>...
Published: 01 March 2010
Fig. 2. Geological map of the study area. The mélange zone and the entire Pangaion-Pirin Complex shown on this map are affected by the Nestos Shear Zone. UTM-Coordinates (WGS84) are given in units of metres.
Journal Article
Published: 29 October 2019
Geological Magazine (2019) 156 (12): 2117–2124.
..., 2018 ). The Kerdilion unit is considered as a gneissic complex similar to the Rhodope Massif and representing its integral crustal component (Burg et al . 1995 ; Kydonakis et al . 2015 ). In order to date the marble deposition in the Pirin unit, we have analysed detrital zircons of the two...
FIGURES | View All (5)
Journal Article
Published: 01 September 1992
Journal of the Geological Society (1992) 149 (5): 855–857.
.... 1) with the older SW-vergent Meso-Rhodopean overthrust ( Dimadis & Zachos 1989 ) of the Central Rhodope (Sidironero) unit over the Pirin-Pangaion unit ( Papanikolaou & Panagopoulos 1981 ; Zagorèev 1981 , 1989 ). This overthrust is probably of a Mid-Cretaceous age similarly to the Strimon...
Journal Article
Published: 01 December 2016
European Journal of Mineralogy (2016) 28 (6): 1187–1202.
...Hans-Joachim Massonne Abstract A garnet-bearing schist, rich in white mica, was sampled from the southern Pirin Mountains, western margin of the Rhodope Metamorphic Complex, near the Popovi-Livadi pass and investigated with the electron microprobe. Garnet grains of mm-size commonly display...
FIGURES | View All (11)
Journal Article
Published: 01 April 1994
Journal of the Geological Society (1994) 151 (2): 413–415.
... plutons) are cross-cutting the folded Rhodopian metamorphic rocks in the Pirin -Pangaion structural zone, in the footwall of the pretended detachment. (5) Radiometric results. Many authors working in northern Greece make far-gone conclusions from the scarce data obtained in the Rhodope massif by isotopic...