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Solea Graben

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Series: GSA Special Papers
Published: 01 January 1995
DOI: 10.1130/SPE296-p81
... Epidosites (epidote- and quartz-rich rock with granoblastic texture) from the Solea graben are believed to form from upflowing hydrothermal fluid that deposited massive sulfide ores at the seawater-sea-floor interface of the Cretaceous age oceanic crust. Epidosite within the graben occurs...
Journal Article
Journal: Geology
Published: 01 November 1992
Geology (1992) 20 (11): 987–990.
...Lori Bettison -Varga; Robert J. Varga; Peter Schiffman Abstract Field relations indicate that high-temperature hydrothermal circulation and accumulation of massive sulfide deposits within the Solea graben of the Troodos ophiolite, Cyprus, followed extreme crustal attenuation. Zones of pervasive...
Journal Article
Published: 01 June 2018
Mineralogical Magazine (2018) 82 (3): 697–724.
... graben, one of three regional graben structures on Cyprus, showing enrichment in Te and Se. Of the three VMS sampled within the Solea graben, Apliki exhibits the most significant enrichment in Se. Samples from the South Apliki Breccia Zone; a zone of hematite-rich breccia containing euhedral pyrite...
FIGURES | View All (16)
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 February 2013
Lithosphere (2013) 5 (1): 109–127.
... transform fault and the N-S–striking Solea graben. Rocks within the inside corner are primarily sheeted dikes and gabbros. The strikes of dikes vary with proximity to the Arakapas fault, changing from NW- to N- to E-striking with increasing proximity to the fault. We report new paleomagnetic results from 24...
FIGURES | View All (13)
Journal Article
Journal: Geology
Published: 01 June 1991
Geology (1991) 19 (6): 637–640.
... graben. A ridge jump boundary separates the old crust, formed at the Solea axis, from the new crust generated at the outside corner of the new ridge with a dextrally slipping continuation of the Southern Troodos transform. The final episode involved extension of the crust generated at the new ridge...
Journal Article
Journal: Geology
Published: 01 July 1987
Geology (1987) 15 (7): 593–597.
...Simon Allerton; F. J. Vine Abstract It has been suggested that grabens on the northern flank of the Troodos ophiolite formed by listric faulting in an oceanic environment and represent axial valleys fossilized by ridge-jumping. This paleomagnetic survey of the Solea graben was carried out...
Image
Outline of Cyprus and the Troodos ophiolite superimposed on the tectonic mo...
Published: 01 September 2001
is considered to have formed as part of an inside corner strip south of the transform. It is possible that the spreading centre north of the Arakapas Fault lay in the Solea Graben which crosses the circular outcrop of mantle rocks in the centre of the northern part of the ophiolite, but the ophiolite west
Image
( a ) Simplified geological map of the late Cretaceous (92 Ma) Troodos ophi...
Published: 01 June 2018
Fig. 1. ( a ) Simplified geological map of the late Cretaceous (92 Ma) Troodos ophiolite, Cyprus. Apliki VMS is located in NW Troodos, W of the Solea graben axis (adapted from Keith et al ., 2016 ). ( b ) Simplified structural cross-section of Troodos. Normal fault rotation leads to inversely
Image
Simplified geologic map for the ridge-transform intersection in the Troodos...
Published: 01 February 2013
Figure 2. Simplified geologic map for the ridge-transform intersection in the Troodos ophiolite. Map details are modified from Bishopp et al. (1959) , Bear and Morel (1960) , Bear and Carr (1960) , Bear (1960) , Pantazis (1967) , and Gass et al. (1994) . Axis of the Solea Graben axis
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Summary of relevant geologic features for interpreting model results of ins...
Published: 01 February 2013
. Insets show paleostress orientations for the east ( Hurst et al., 1994 ) and west ( Varga, 1991 ) sides of the Solea graben. TMV—Troodos mean vector.
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( a ) Location map of the Apliki VMS and structural schematic cross-section...
Published: 01 June 2018
Fig. 5. ( a ) Location map of the Apliki VMS and structural schematic cross-section. Apliki is located in NW Troodos within the Solea graben. The deposit is situated within the Lower Pillow Lava stratigraphy and bound by two axis parallel (N–S) normal faults. At depth faults are inferred
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Geological map of Troodos ophiolite (Cyprus) showing location of study area...
Published: 01 March 2016
Figure 1. Geological map of Troodos ophiolite (Cyprus) showing location of study area and main structural features such as axis and edges of Solea graben (red lines), Southern Troodos transform fault zone (STTFZ), and general orientation of sheeted dikes (short black lines). Region in study area
Journal Article
Published: 01 November 1995
Journal of the Geological Society (1995) 152 (6): 923–932.
.... Tectonic evolution of the Troodos ophiolite within the Tethyan framework Tectonics 1990 9 811 823 Hurst S.D. Moores E.M. Varga R.J. Structural and geophysical expression of the Solea graben, Troodos Ophiolite, Cyprus Tectonics 1994 13 139 156 Karson J.A. Halls...
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Fe/(    Fe   +   Mg    )
versus Si (per formula unit) for chlorites (does n...
Published: 01 January 2002
Figure 5. Fe/( Fe  +  Mg ) versus Si (per formula unit) for chlorites (does not include mixed-layer smectite/chlorite analyses). Field for other sheeted dike sections from Gillis and Robinson ( 1990 ; upper dikes, Akai area) and Schiffman and Smith ( 1988 ; NW Troodos, Solea graben area
Journal Article
Journal: Geology
Published: 01 March 2016
Geology (2016) 44 (3): 199–202.
...Figure 1. Geological map of Troodos ophiolite (Cyprus) showing location of study area and main structural features such as axis and edges of Solea graben (red lines), Southern Troodos transform fault zone (STTFZ), and general orientation of sheeted dikes (short black lines). Region in study area...
FIGURES
Journal Article
Journal: Geology
Published: 01 February 2000
Geology (2000) 28 (2): 151–154.
... deformation in the Solea graben spreading center, Troodos ophiolite, Cyprus : Geology , v. v. 20 pp. 987 ߝ 990 . Bloomer , S.H. , Taylor , B. , MacLeod , C.J. , Stern , R.J. , Fryer , P. , Hawkins , J.W. , and Johnson , L. , 1995 , Early arc volcanism and the ophiolite...
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Journal Article
Published: 01 January 2002
The Journal of Geology (2002) 110 (1): 57–74.
...Figure 5. Fe/( Fe  +  Mg ) versus Si (per formula unit) for chlorites (does not include mixed-layer smectite/chlorite analyses). Field for other sheeted dike sections from Gillis and Robinson ( 1990 ; upper dikes, Akai area) and Schiffman and Smith ( 1988 ; NW Troodos, Solea graben area...
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Journal Article
Published: 01 September 2001
Journal of the Geological Society (2001) 158 (5): 757–767.
... is considered to have formed as part of an inside corner strip south of the transform. It is possible that the spreading centre north of the Arakapas Fault lay in the Solea Graben which crosses the circular outcrop of mantle rocks in the centre of the northern part of the ophiolite, but the ophiolite west...
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Journal Article
Journal: Geology
Published: 01 October 2007
Geology (2007) 35 (10): 935–938.
... . Schiffman , P. , and Smith , B.M. , 1988 , Petrology and oxygen isotope geochemistry of a fossil sea-water hydrothermal system within the Solea graben, northern Troodos ophiolite, Cyprus : Journal of Geophysical Research , v. 93 pp. 4612 - 4624 . Schroeder , T. , and John , B.E...
FIGURES
Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.260.01.15
EISBN: 9781862395084
... ). Spreading took place either by steady-state processes ( Allerton & Vine 1987 ), or by formation of discrete, ephemeral, sea-floor grabens ( Varga & Moores 1985 ). The best documented and most distinctive graben runs through the Solea area to the north of the plutonic complex, above the ‘Kakopetria...
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