Danelian, Taniel, Robertson, Alastair H. F., Dimitriadis, Sarantis (1996) Age and significance of radiolarian sediments within basic extrusives of the marginal basin Guevgueli Ophiolite (northern Greece) Geological Magazine, 133 (2) 127-136 doi:10.1017/s0016756800008645
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Age and significance of radiolarian sediments within basic extrusives of the marginal basin Guevgueli Ophiolite (northern Greece) | ||
| Journal | Geological Magazine | ||
| Authors | Danelian, Taniel | Author | |
| Robertson, Alastair H. F. | Author | ||
| Dimitriadis, Sarantis | Author | ||
| Year | 1996 (March) | Volume | 133 |
| Page(s) | 127-136 | Issue | 2 |
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/s0016756800008645Search in ResearchGate | ||
| Mindat Ref. ID | 256882 | Long-form Identifier | mindat:1:5:256882:3 |
| GUID | 62baa619-4abc-4927-a298-2c2f5ccd6254 | ||
| Full Reference | Danelian, Taniel, Robertson, Alastair H. F., Dimitriadis, Sarantis (1996) Age and significance of radiolarian sediments within basic extrusives of the marginal basin Guevgueli Ophiolite (northern Greece) Geological Magazine, 133 (2) 127-136 doi:10.1017/s0016756800008645 | ||
| Plain Text | Danelian, Taniel, Robertson, Alastair H. F., Dimitriadis, Sarantis (1996) Age and significance of radiolarian sediments within basic extrusives of the marginal basin Guevgueli Ophiolite (northern Greece) Geological Magazine, 133 (2) 127-136 doi:10.1017/s0016756800008645 | ||
| In | (1996, March) Geological Magazine Vol. 133 (2) Cambridge University Press (CUP) | ||
| Abstract/Notes | AbstractWell-preserved Radiolaria have been discovered in calcareous silt turbidites and mudstones intercalated with basic extrusives of the Guevgueli Ophiolite, northern Greece. The mudstones contain terrigenous silt, probably derived from adjacent continental basement of the Serbo-Macedonian and/or Paikon units. Volcanic quartz and rare volcanic glass were probably derived from an active continental margin arc (Paikon volcanic arc) to the west. The radiolarian sediments were deposited within fault-controlled hollows in the ophiolitic extrusives, and then covered by massive and pillowed extrusives. The radiolarian assemblage is indicative of an early Late Jurassic (Oxfordian) age, which therefore dates the genesis of the Guevgueli Ophiolite. Our data are consistent with the age of the intrusive Late Jurassic Fanos Granite, believed to be contemporaneous with the Guevgueli Ophiolite. In general, the Guevgueli and related ophiolites of northern Greece are thought to have formed within a transtensional intra-continental marginal basin, generated in response to oblique eastward subduction of older Tethyan oceanic crust (Almopias ocean). | ||
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| Not Yet Imported: Bulletin de la Société Géologique de France - journal-article : 10.2113/gssgfbull.S7-XIX.4.927 If you would like this item imported into the Digital Library, please contact us quoting Journal ID 10845 | |
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