کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4677240 1634791 2013 14 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Segmentation of the Hellenides recorded by Pliocene initiation of clockwise block rotation in Central Greece
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات علوم زمین و سیاره ای (عمومی)
پیش نمایش صفحه اول مقاله
Segmentation of the Hellenides recorded by Pliocene initiation of clockwise block rotation in Central Greece
چکیده انگلیسی

New paleomagnetic data from Early Miocene to Pliocene terrestrial sedimentary and volcanic rocks in Central Greece constrain the history of vertical-axis rotation along the central part of the western limb of the Aegean arc. The present-day pattern of rapid block rotation within a broad zone of distributed deformation linking the right-lateral North Anatolian and Kephalonia continental transform faults initiated after Early Pliocene time, resulting in a uniform clockwise rotation of 24.3±6.5° over a region >250 km long and >150 km wide encompassing Central Greece and the western Cycladic archipelago. Because the published paleomagnetic dataset requires clockwise rotations of >50° in Western Greece after ∼17 Ma, while our measurements resolve no vertical-axis rotation of Central Greece between ∼15 Ma and post-Early Pliocene time, a large part of the clockwise rotation of Western Greece must have occurred during the main period of contraction within the external thrust belt of the Ionian Zone between ∼17 and ∼15 Ma. Pliocene initiation of rapid clockwise rotation in Central and Western Greece reflects the development of the North Anatolia–Kephalonia Fault system within the previously extended Aegean Sea region, possibly in response to entry of dense oceanic lithosphere of the Ionian Sea into the Hellenic subduction zone and consequent accelerated slab rollback. The development of the Aegean geometric arc therefore occurred in two short-duration pulses characterized by rapid rotation and strong regional deformation.


► We present paleomagnetic remanence directions from Neogene rocks in Central Greece.
► Clockwise rotation occurred in two distinct episodes.
► Initial clockwise rotation occurred in Middle Miocene time.
► A second pulse of clockwise rotation initiated after Early Pliocene time.
► Pliocene start of clockwise rotation records growth of Central Hellenic Shear Zone and onset of differential trench retreat.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Earth and Planetary Science Letters - Volume 362, 15 January 2013, Pages 6–19
نویسندگان
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