Highly extended terrains, lateral segmentation of the substratum, and basin development: The middle-late Miocene Radicondoli Basin (inner northern Apennines, Italy)

Tectonics ◽  
2008 ◽  
Vol 27 (5) ◽  
pp. n/a-n/a ◽  
Author(s):  
Andrea Brogi ◽  
Domenico Liotta
Keyword(s):  
Late Miocene ◽  
Northern Apennines ◽  
Basin Development

scholarly journals Geology of the late Miocene south-eastern Volterra Basin (Northern Apennines, Italy)

2014 ◽  
Vol 12 (1) ◽  
pp. 12-25 ◽  
Author(s):  
Alessandro Ielpi ◽  
Gianluca Cornamusini
Keyword(s):  
Late Miocene ◽  
Northern Apennines ◽  
South Eastern

Late Miocene shortening of the Northern Apennines back-arc

2014 ◽  
Vol 74 ◽  
pp. 1-31 ◽  
Author(s):  
Marco Bonini ◽  
Federico Sani ◽  
Eusebio M. Stucchi ◽  
Giovanna Moratti ◽  
Marco Benvenuti ◽  
...  
Keyword(s):  
Late Miocene ◽  
Northern Apennines ◽  
Back Arc

scholarly journals New Constraints on the Evolution of the Inner Northern Apennines by K‐Ar Dating of Late Miocene‐Early Pliocene Compression on the Island of Elba, Italy

Tectonics ◽  
2018 ◽  
Vol 37 (9) ◽  
pp. 3229-3243 ◽  
Author(s):  
Giulio Viola ◽  
Espen Torgersen ◽  
Francesco Mazzarini ◽  
Giovanni Musumeci ◽  
Roelant Lelij ◽  
...  
Keyword(s):  
Late Miocene ◽  
Northern Apennines ◽  
Early Pliocene

scholarly journals Late Miocene remagnetization within the internal sector of the Northern Apennines, Italy

2004 ◽  
Vol 383 (1-2) ◽  
pp. 1-14 ◽  
Author(s):  
I.W Aiello ◽  
J.T Hagstrum ◽  
G Principi
Keyword(s):  
Late Miocene ◽  
Northern Apennines

scholarly journals Pliocene–Pleistocene sedimentary–tectonic development of the Mesaoria (Mesarya) Basin in an incipient, diachronous collisional setting: facies evidence from the north of Cyprus

2016 ◽  
Vol 155 (5) ◽  
pp. 997-1022 ◽  
Author(s):  
ROMESH N. PALAMAKUMBURA ◽  
ALASTAIR H. F. ROBERTSON
Keyword(s):  
Late Miocene ◽  
Sediment Accumulation ◽  
Early Pleistocene ◽  
The South ◽  
Geological Evidence ◽  
Northern Margin ◽  
The North ◽  
Surface Uplift ◽  
Basin Development ◽  
Multi Stage

AbstractThe Mesaoria (Mesarya) Basin exemplifies multi-stage basin development within a regional setting of diachronous continental collision. The Plio-Pleistocene represented a period of major sediment accumulation between two topographic highs, the Kyrenia Range in the north and the Troodos Massif in the south. During Pliocene time, open-marine marls and chalks of the Nicosia (Lefkoşa) Formation accumulated in a shelf setting. The Early Pleistocene period was characterized by a relative fall in sea level and a change to shallower-water bioclastic deposition of the Athalassa (Gürpınar) Formation. The northern margin of the basin was approximately delineated by the E–W neotectonic Ovgos (Dar Dere) fault zone. A carbonate ramp system formed directly to the south of this structural feature. During Early Pleistocene time, the basin evolved from an open-marine shelf to semi-enclosed lagoons with deltaic deposits, and finally to a non-marine aeolian setting, flanked by the rising Kyrenia Range to the north. Synthesis of geological evidence from the Mesaoria (Mesarya) Basin as a whole, including outcrop and borehole evidence from the south, adjacent to the Troodos Massif, indicates that the Pliocene – Early Pleistocene represented a relatively quiescent period. This intervened between Late Miocene – earliest Pleistocene southward thrusting–folding of the Kyrenia Range and Pleistocene intense surface uplift of both the Kyrenia Range and the Troodos Massif. The basin development reflects flexurally controlled collapse during Late Miocene – earliest Pliocene time related to southward thrusting, followed by strike-slip during westward tectonic escape of Anatolia, and finally regional uplift controlled by under-thrusting of continental crust from the south, as collision progressed.

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