Matches in SemOpenAlex for { <https://semopenalex.org/work/W3013529928> ?p ?o ?g. }
Showing items 1 to 69 of
69
with 100 items per page.
- W3013529928 abstract "The Middle Anatolia Massif is one of the largest igneous and metamorphic complexes in Turkey. The western part of the massif is the subject of the present study. The main purposes of the work are to map the different igneous and metamorphic rocks; to identify their mineralogical, petrographical and geochemical characteristics and by considering their relationships to each other, determine the metamorphic, magmatic and geological evolution of the Ortakoy area. The geological map of the Ortakoy area (Appendix-Ia) shows that the oldest identified rocks are the Seksenusagi Formation of Silurian- Devonian age and the conformably overlying Gobektepe Formation of Upper Palaeozoic age. The Ekecekdagi gabbro comprises hornblende-gabbro and minor banded gabbro and may have been emplaced onto the metamorphic rocks as an allochthonous unit or intruded into the metasediments before the intrusion of the Ortakoy pluton. The metasediments were intruded and hornfelsed by the voluminous Upper Cretaceous - Paleocene Ortakoy pluton containing hornblendite, hornblende diorite, biotite-hornblende granitoid, microgranite and quartz- alkali syenite. The massif is overlain by the Pecenek Formation of Pliocene age composed of rhyolitic tuff; clay and sand with some gravels; and lacustrine limestone. Colluvium and alluvium are the youngest formations in the area. The Ortakoy part of the Middle Anatolia Massif underwent four phases of deformation: D1 during the formation of the metamorphic rock fabric, D2 which produced folds varying from isoclinal to tight while D3 folds have open limbs and developed in approximately an E-W direction. D4 folds are usually open with steep axial planes and plunge roughly towards the S-E. The massif was then uplifted inducing the development of the WSW-ENE dominated joint sets in the Ekecekdagi gabbro, diorite and granitoid and the formation of WNW-ESE faults. During or after D1 deformation, the Ortakoy metasediments underwent a single episode of regional metamorphism corresponding to the upper amphibolite facies conditions (second sillimanite grade), which is confirmed by geothermometer studies from the different metamorphic assemblages which yield between 608-761" @default.
- W3013529928 created "2020-04-03" @default.
- W3013529928 creator A5030383312 @default.
- W3013529928 date "1993-01-01" @default.
- W3013529928 modified "2023-09-26" @default.
- W3013529928 title "The Petrology and Geochemistry of the Ortakoy Area, Central Turkey" @default.
- W3013529928 hasPublicationYear "1993" @default.
- W3013529928 type Work @default.
- W3013529928 sameAs 3013529928 @default.
- W3013529928 citedByCount "3" @default.
- W3013529928 crossrefType "dissertation" @default.
- W3013529928 hasAuthorship W3013529928A5030383312 @default.
- W3013529928 hasConcept C127313418 @default.
- W3013529928 hasConcept C151730666 @default.
- W3013529928 hasConcept C160776313 @default.
- W3013529928 hasConcept C17409809 @default.
- W3013529928 hasConcept C26687426 @default.
- W3013529928 hasConcept C2777212541 @default.
- W3013529928 hasConcept C2777229588 @default.
- W3013529928 hasConcept C2778849375 @default.
- W3013529928 hasConcept C2779870107 @default.
- W3013529928 hasConcept C33757491 @default.
- W3013529928 hasConcept C34122518 @default.
- W3013529928 hasConcept C42787717 @default.
- W3013529928 hasConcept C5900021 @default.
- W3013529928 hasConcept C77928131 @default.
- W3013529928 hasConcept C79605941 @default.
- W3013529928 hasConceptScore W3013529928C127313418 @default.
- W3013529928 hasConceptScore W3013529928C151730666 @default.
- W3013529928 hasConceptScore W3013529928C160776313 @default.
- W3013529928 hasConceptScore W3013529928C17409809 @default.
- W3013529928 hasConceptScore W3013529928C26687426 @default.
- W3013529928 hasConceptScore W3013529928C2777212541 @default.
- W3013529928 hasConceptScore W3013529928C2777229588 @default.
- W3013529928 hasConceptScore W3013529928C2778849375 @default.
- W3013529928 hasConceptScore W3013529928C2779870107 @default.
- W3013529928 hasConceptScore W3013529928C33757491 @default.
- W3013529928 hasConceptScore W3013529928C34122518 @default.
- W3013529928 hasConceptScore W3013529928C42787717 @default.
- W3013529928 hasConceptScore W3013529928C5900021 @default.
- W3013529928 hasConceptScore W3013529928C77928131 @default.
- W3013529928 hasConceptScore W3013529928C79605941 @default.
- W3013529928 hasLocation W30135299281 @default.
- W3013529928 hasOpenAccess W3013529928 @default.
- W3013529928 hasPrimaryLocation W30135299281 @default.
- W3013529928 hasRelatedWork W139082560 @default.
- W3013529928 hasRelatedWork W1908040778 @default.
- W3013529928 hasRelatedWork W1971477537 @default.
- W3013529928 hasRelatedWork W1975048754 @default.
- W3013529928 hasRelatedWork W2041852442 @default.
- W3013529928 hasRelatedWork W2068742566 @default.
- W3013529928 hasRelatedWork W2086330480 @default.
- W3013529928 hasRelatedWork W2116362343 @default.
- W3013529928 hasRelatedWork W2133608321 @default.
- W3013529928 hasRelatedWork W2149203698 @default.
- W3013529928 hasRelatedWork W2154745739 @default.
- W3013529928 hasRelatedWork W2367907532 @default.
- W3013529928 hasRelatedWork W2524129053 @default.
- W3013529928 hasRelatedWork W2605187003 @default.
- W3013529928 hasRelatedWork W2901366383 @default.
- W3013529928 hasRelatedWork W2995214547 @default.
- W3013529928 hasRelatedWork W3004223848 @default.
- W3013529928 hasRelatedWork W3094123866 @default.
- W3013529928 hasRelatedWork W363267401 @default.
- W3013529928 hasRelatedWork W1879255551 @default.
- W3013529928 isParatext "false" @default.
- W3013529928 isRetracted "false" @default.
- W3013529928 magId "3013529928" @default.
- W3013529928 workType "dissertation" @default.