Drip tectonics and the enigmatic uplift of the Central Anatolian Plateau.
Drip tectonics and the enigmatic uplift of the Central Anatolian Plateau.
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DOI:
10.1038/s41467-017-01611-3
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发表时间:
2017-11-16
影响因子:
16.6
通讯作者:
Gün E
中科院分区:
文献类型:
--
作者:
Göğüş OH;Pysklywec RN;Şengör AMC;Gün E
Lithospheric drips have been interpreted for various regions around the globe to account for the recycling of the continental lithosphere and rapid plateau uplift. However, the validity of such hypothesis is not well documented in the context of geological, geophysical and petrological observations that are tested against geodynamical models. Here we propose that the folding of the Central Anatolian (Kırşehir) arc led to thickening of the lithosphere and onset of “dripping” of the arc root. Our geodynamic model explains the seismic data showing missing lithosphere and a remnant structure characteristic of a dripping arc root, as well as enigmatic >1 km uplift over the entire plateau, Cappadocia and Galatia volcanism at the southern and northern plateau margins since ~10 Ma, respectively. Models show that arc root removal yields initial surface subsidence that inverts >1 km of uplift as the vertical loading and crustal deformation change during drip evolution. The recycling of continental lithosphere and rapid plateau uplift is believed to be the result of lithospheric drips, but natural examples are missing. Here, the authors use geodynamic models to suggest that the folding and thickening of the Central Anatolian arc caused lithospheric dripping of the arc root.
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影响因子:
3.9
作者:
Beaumont, C;Kamp, PJJ;Fullsack, P
通讯作者:
Fullsack, P
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