In:
Tectonics, American Geophysical Union (AGU), Vol. 29, No. 3 ( 2010-06)
Abstract:
The Rhodope Metamorphic Province in the area around the Mesta Graben (SW Bulgaria) exposes a structurally lower complex, the Pangaion‐Pirin Complex of Variscan continental crust and its cover (mostly orthogneiss and marble), and a higher complex, the Rhodope Terrane of mixed oceanic and continental origin with metamorphosed Jurassic arc magmatites. The boundary between the two is the top‐to‐the‐southwest Nestos Shear Zone. The regional top‐to‐the‐southwest shearing of the two basement complexes is related to the emplacement of the Rhodope Terrane over the Pangaion‐Pirin Complex along this shear zone. Syntectonic and posttectonic Alpine intrusions within the basement can provide age limits for the thrusting. Zircons from the posttectonic Teshovo (south Pirin) Granitoid Pluton in the Pangaion‐Pirin Complex yielded crystallization ages of 32 ± 0.2 Ma (LA‐SF‐ICP‐MS U‐Pb method). Zircons from two syntectonic granite plutons in the Rhodope Terrane (Dolno Dryanovo and Spanchevo) have circa 143 to 145 Ma old inherited magmatic cores and circa 55 to 56 Ma old magmatic rims. These ages, especially the presence of the Upper Jurassic/Lower Cretaceous cores in the plutons from the Rhodope Terrane, and the structural relations indicate that the southwestward thrusting of the Rhodope Terrane over the Pangaion‐Pirin Complex took place in the Paleogene. A model is proposed in which the Pangaion‐Pirin Complex represents the margin of Apulia and the structure of the Rhodopes is explained by a switch of subduction polarity from SW dipping in the Jurassic and Early Cretaceous to NE dipping in the Late Cretaceous and Paleogene.
Type of Medium:
Online Resource
ISSN:
0278-7407
,
1944-9194
DOI:
10.1029/2009TC002558
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2010
detail.hit.zdb_id:
2013221-9
detail.hit.zdb_id:
780264-X
SSG:
16,13
SSG:
13
