Fragmentation of Adria and active decollement tectonics within the southern peri-Tyrrhenian orogen, Italy

被引：0
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作者：
Oldow, JS [1 ]
Ferranti, L
机构：
[1] Univ Idaho, Dept Geol Sci, Moscow, ID 83844 USA
[2] Univ Naples Federico II, Dipartimento Sci Terra, I-80138 Naples, Italy
来源：
ADRIA MICROPLATE GPS GEODESY, TECTONICS AND HAZARDS | 2006年 / 61卷
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中图分类号：
P3 [地球物理学]; P59 [地球化学];
学科分类号：
0708 ; 070902 ;
摘要：
Seismicity and GPS velocities in the southern peri-Tyrrhenian orogen record complex differential motion amongst crustal blocks constituting the tectonically fragmented paleotectonic domain, Adria. Coeval transpressional and transtensional belts within the orogen are kinematically coordinated and are consistent with displacement above a through-going basal decollement system that separates the heterogeneously deforming upper and middle crust from a presumed pattern of regular displacement within the underlying lithosphere. Seismicity and GPS velocities within the orogen reflect only indirectly the relative convergence between Africa and Eurasia.
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页码：269 / +
页数：4
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