DOI: 10.1007/s00531-017-1452-2
Scopus记录号: 2-s2.0-85014085043
论文题名: Metamorphic conditions and structural evolution of the Kesebir-Kardamos dome: Rhodope metamorphic complex (Greece-Bulgaria)
作者: Moulas E. ; Schenker F.L. ; Burg J.-P. ; Kostopoulos D.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2017
卷: 106, 期: 8 起始页码: 2667
结束页码: 2685
语种: 英语
英文关键词: Migmatitic dome
; Rhodope
; Syn-metamorphic deformation
; Tectonics
; Zircon dating
Scopus关键词: brittle deformation
; dome
; exhumation
; geobarometry
; geochronology
; geodynamics
; metamorphic rock
; petrology
; shear zone
; SHRIMP dating
; subduction zone
; tectonic evolution
; zircon
; Bulgaria
; Greece
英文摘要:
The synmetamorphic nappe system of the Rhodope Metamorphic Complex has been deformed into dome-and-basin structures attributed to syn- to post-convergent exhumation. We document the deformation style and present new thermobarometric and geochronological constraints for the Kesebir–Kardamos dome in southern Bulgaria and northern Greece. The dome consists of a migmatitic core overlain by high-grade thrust sheets. Kinematic indicators indicate a continuum from ductile to brittle conditions during exhumation. Thermodynamic modeling applied to the high-grade, intermediate thrust sheets yielded peak conditions of 1.2 GPa and ca 730 °C. New U–Pb SHRIMP-II dating of zircons from rocks of the same unit revealed Late Jurassic–Early Cretaceous (145 Ma) as the time of metamorphic crystallization; some zircon rims yielded Eocene ages (53 and 44 Ma) interpreted as having been thermally reset owing to coeval granitoid magmatism. The high-grade rocks were covered by Lutetian–Priabonian marine sediments after exhumation. Slumps suggest that sedimentation took place in a tectonically active environment. Our new structural, petrological and geochronological results suggest that the major shear zone in the core of the Kesebir-Kardamos dome is equivalent to the Late Jurassic–Early Cretaceous Nestos Shear Zone. Post-Jurassic metamorphic ages recorded in the Rhodope most likely represent crustal rather than deep subduction geodynamic processes. © 2017, Springer-Verlag Berlin Heidelberg.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85014085043&doi=10.1007%2fs00531-017-1452-2&partnerID=40&md5=15ebb715211ca580af801e2fbf3a2819
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/69952
Appears in Collections: 影响、适应和脆弱性 气候减缓与适应
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作者单位: Department of Earth Sciences, ETH-Zurich, Zurich, Switzerland; Institute of Earth Science, University of Applied Sciences and Arts of Southern Switzerland (SUPSI), Campus Trevano, Manno, Switzerland; Department of Mineralogy and Petrology, National and Kapodistrian University of Athens, Athens, Greece
Recommended Citation:
Moulas E.,Schenker F.L.,Burg J.-P.,et al. Metamorphic conditions and structural evolution of the Kesebir-Kardamos dome: Rhodope metamorphic complex (Greece-Bulgaria)[J]. International Journal of Earth Sciences,2017-01-01,106(8)