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Naxos Island

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Journal Article
Published: 28 April 2021
Journal of the Geological Society (2021) jgs2020-217.
... in the passive margin sequence of the Cycladic Blueschist Unit on Naxos Island, Greece, separates amphibolite facies, non-high-pressure rocks (Koronos Unit) below the shear zone from Eocene high-pressure rocks (Zas Unit) above the shear zone. We review existing pressure–temperature data from the Koronos Unit...
FIGURES | View All (9)
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP321.9
EISBN: 9781862395695
... and are discussed taking into account the tectonic history of Naxos Island based on published structural and metamorphic data. This discussion will also reassess previously published thermal and tectonic models accounting for thermochronometric data obtained previously. The previous geochronological data sets...
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Series: GSA Special Papers
Published: 01 January 2004
DOI: 10.1130/0-8137-2378-7.51
... An interdisciplinary study has been carried out on Naxos Island, located in the southern Aegean Sea (Greece), which shows Miocene geodynamic and environmental changes in a classic example of a collapsing orogen. Early to mid-Miocene siliciclastic deposits on Naxos have been shed from...
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Geological map of <b>Naxos</b> <b>Island</b> and two cross-sections, one E–W and the othe...
Published: 02 April 2019
Fig. 9. Geological map of Naxos Island and two cross-sections, one E–W and the other N–S, showing simplified geometry of the metamorphic core complex (after Lamont et al. 2019 ). Note upright folds in the kyanite- and sillimanite-grade core unit truncated by the overlying Koronos Shear Zone
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Panorama and cross-section across Mount Koronos area, <b>Naxos</b> <b>Island</b>, showing...
Published: 02 April 2019
Fig. 10. Panorama and cross-section across Mount Koronos area, Naxos Island, showing the geometry of the folds, ductile shear zones and faults. (a) Infolded kyanite gneisses (green) and marbles (blue) of the Koronos Unit structurally overlying deepest-level kyanite- and sillimanite-migmatites
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Geological map of <b>Naxos</b> <b>Island</b> (modified from Koukouvelas &amp;amp; Kokkalas,  ...
Published: 29 August 2012
Figure 5. Geological map of Naxos Island (modified from Koukouvelas & Kokkalas, 2003 ) with fault-slip data from the major faults. NF – Naxos Fault, SF – Stellida Fault, GF – Glinadon Fault. (a) The Stellida area in more detail showing the NE-striking main
Journal Article
Published: 01 December 1998
European Journal of Mineralogy (1998) 10 (6): 1309–1319.
...Dov Avigad Abstract The island of Naxos, in the centre of the Aegean Sea, is a Cordillera-type metamorphic core complex formed by the collapse of the Alpine orogenic belt of the Hellenides. The island is dominated by Early-Miocene (M2) Barrovian metamorphic assemblages that overprinted Eocene (M1...
Journal Article
Journal: GSA Bulletin
Published: 04 June 2019
GSA Bulletin (2020) 132 (1-2): 149–197.
...Thomas N. Lamont; Michael P. Searle; David J. Waters; Nick M.W. Roberts; Richard M. Palin; Andrew Smye; Brendan Dyck; Phillip Gopon; Owen M. Weller; Marc R. St-Onge Abstract The island of Naxos, Greece, has been previously considered to represent a Cordilleran-style metamorphic core complex...
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Journal Article
Published: 01 July 2000
European Journal of Mineralogy (2000) 12 (4): 859–875.
...Georgia PE-PIPER Abstract The island of Naxos in the Cyclades preserves a core complex developed by Miocene detachment faulting associated with extension of continental crust inboard of the Hellenic subduction zone. The extension has unroofed Miocene hornblende-biotite granite and leucogranite...
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Journal Article
Journal: Geology
Published: 01 October 1998
Geology (1998) 26 (10): 935–938.
... of key localities on the Aegean island of Naxos (Greece) in which we combined textural observations with micro-scale trace element and stable isotope analysis to test the assumptions upon which modeling of metamorphic fluid flow is based, and to identify fluid transport mechanisms. Integration of ion...
Journal Article
Journal: GSA Bulletin
Published: 01 January 2017
GSA Bulletin (2017) 129 (1-2): 93–117.
... and Pliocene sedimentary rocks ( Kuhlemann et al., 2004 ), which form a synform between the Naxos metamorphic core complex and the Naxos Granite. Figure 2. (A) Geological map of the Naxos metamorphic core complex in the Cyclades Islands, Greece, showing lithologies, metamorphic isograds, and faults...
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Journal Article
Published: 01 February 1991
Journal of the Geological Society (1991) 148 (1): 93–103.
.... In some cases however, granitic plutonism on other islands is roughly coeval with the M2, event on Naxos (e.g. Tinos, Ikaria; Altherr et al. 1982). Wijbrans & McDougall (1988) suggest that such an intrusion may have provided the heat source for the M2, event itself. The chemistry and distribution...
Journal Article
Published: 01 January 2003
Geological Magazine (2003) 140 (1): 45–61.
... and crops out over the eastern part of the island of Naxos (Fig. 1b ); (c) the Chora unit consisting of orthogneisses, and paragneisses of Hercynian age, which is exposed in the inner core of Naxos ( Pe-Piper, Kotopouli & Piper, 1997 ; Keay, Lister & Buick, 2001 ); (d) the Late Triassic to Late...
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Journal Article
Published: 01 January 2002
European Journal of Mineralogy (2002) 14 (1): 37–47.
... on the island of Naxos in the Cycladic Archipelago, Greece, where detailed petrological analysis of high-grade siliceous dolomite assemblages in the Miocene (M2) metamorphic complex ( Fig. 1 ) revealed two distinct periods of mineral growth. The first period of mineral growth occurred during prograde M2...
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Sm&#x2F;Nd isotopic compositions of the plutonic rocks of the <b>island</b> of <b>Naxos</b>.
Published: 01 July 2000
Table 2. Sm/Nd isotopic compositions of the plutonic rocks of the island of Naxos.
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP291.2
EISBN: 9781862395398
... Cretaceous age was assigned to the metamorphic event that affected the entire sequence of the Upper Unit ( Katzir et al. 1996 ). Late Cretaceous ages were also determined for Upper Unit gneisses and amphibolites on several other islands in the Cyclades ( Reinecke et al. 1982 ; Maluski et al. 1987...
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Journal Article
Journal: Geology
Published: 01 February 2002
Geology (2002) 30 (2): 119–122.
...A. Feenstra; B. Wunder Abstract The diasporite-corundite rock transformation, which releases 6–8 wt% H 2 O in an average metabauxite, was studied experimentally. The results are compared with petrological observations on the island of Naxos (Greece), where the transformation occurred in metakarst...
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Journal Article
Published: 03 February 2011
Geological Magazine (2011) 148 (4): 511–528.
...- and/or tectonostratigraphic relationships across the Cycladic islands, and as a proxy for the time of sediment formation. For this purpose, we have studied metamorphic carbonate rocks from the islands of Tinos, Andros, Syros, Sifnos and Naxos. Identical 87 Sr/ 86 Sr values for certain marble horizons occurring on Tinos...
Journal Article
Journal: Geology
Published: 01 April 1984
Geology (1984) 12 (4): 221–225.
...Gordon S. Lister; Greetje Banga; Anne Feenstra Abstract The islands of Ios and Naxos in the Cycladic archipelago, Greece, contain elongate domes over which a pervasive north- to north-northeast–stretching lineation is warped. These islands may be metamorphic core complexes of Cordilleran type...
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP291.3
EISBN: 9781862395398
.... The islands of Tinos and Andros are part of the numerous metamorphic core complexes exhumed in the Aegean domain. They illustrate two steps of a gradient of finite extension along a transect between Mt. Olympos and Naxos. This study confirms the main role of boudinage as an initial localizing factor...
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